Pre-AGU GeoPRISMS Mini-Workshop – Save the date!


Please consider attending the following mini-workshop before the 2015 Fall AGU Meeting – Sunday December 13, 2015. Please mark your calendars today!

From rifting to drifting: evidence from rifts and margins worldwide

Further details about registration and mini-workshop programs will be coming soon on the GeoPRISMS website and will be advertised as well on the listserv.

The GeoPRISMS Office

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From rifting to drifting: evidence from rifts and margins worldwide

Sunday December 13, 2015, 9 – 5pm, Grand Hyatt, Fillmore ABC

Conveners:

Rebecca Bendick (University of Montana)

Ian Bastow (Imperial College London)

Tyrone Rooney (Michigan State University)

Harm van Avendonk (Univ. Texas Institute for Geophysics, UT-Austin)

Jolante van Wijk (New Mexico Tech)

The purpose of this workshop is to facilitate discussion on the current state of research into continental extension. Our aim is to be broadly inclusive by bringing an audience with widely varying backgrounds to a common understanding of the state of the art in this field. Our ultimate goal will then be to pursue a discussion on future research challenges for the community and how these challenges align with the existing science plans for the GeoPRISMS Eastern North America and East African Rift Focus Sites. We will organize this meeting around the following themes:

1. Melt generation in extensional environments: Mantle decompression,

thermal state and composition of the mantle.

2. Magma-lithosphere interaction: diking, metasomatism, thermal weakening,

changing the composition of the lithosphere, coupling between deformation and melt

migration.

3. Stretching of the lithosphere: Strain localization in brittle and ductile

rheology, rates of extension, punctuated events.

4. Feedback loops – rifting and surface processes: sedimentation, margin

architecture

5. Rifting and oceanic spreading – the missing link: Lithospheric breakup,

focusing of melt delivery, evolution of mantle deformation

AGU Chapman Conference on Slow Slip Phenomena Feb 21-25, 2016


This conference will bring together scientists working on slow slip in all places where they are observed. Abstracts are encouraged based on the following topics:

Observations of slow slip phenomena

Fault structure and physical conditions where slow earthquakes are observed

Slow earthquakes and their relationship to large earthquakes and seismic hazard

Models and laboratory experiments

Improving observational methods for the analysis of slow slip phenomena

The abstract submission site will open in September 2015.

Visit the conference web site (http://chapman.agu.org/slowslip/) to learn more, including how to submit an abstract, register, and reserve housing at the AGU group rate!

Conveners:
Allen Husker – Universidad Nacional Autónoma de México
Heidi Houston – University of Washington
Yoshihiro Ito – Kyoto University

Program Committee
Michel Campillo – Université Joseph Fourier
Victor Cruz-Atienza – Universidad Nacional Autónoma de México
Satoshi Ide – University of Tokyo
Matt Ikari – University of Bremen
Vladimir Kostoglodov – Universidad Nacional Autónoma de México
Susan Schwartz – University of California, Santa Cruz
David Shelly – U.S. Geological Survey
Laura Wallace – University of Texas

Job Posting: Two Assistant Professor Positions and One-Year visiting Position


1) Two Assistant Professor Positions Paleontology/Sedimentary Geology and Geophysics – OSU Boone Pickens School of Geology

2) One-Year Visiting Position in Petrology and Plate Tectonics, Calendar Year 2016 – University of North Carolina at Chapel Hill 

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1) Two Assistant Professor Positions Paleontology/Sedimentary Geology and Geophysics – OSU Boone Pickens School of Geology

The Boone Pickens School of Geology at Oklahoma State University seeks to fill two tenure track assistant professor positions: one in paleontology/sedimentary geology and another in exploration geophysics. The anticipated start date is August 16, 2016. The successful applicants should have a Ph.D. degree in geosciences or related field at the time of appointment.

For the paleontology/sedimentary geology position, we are seeking a geoscientist with research and teaching interest in paleontology as well as sedimentary geology and stratigraphy. Desired areas of specialization may include invertebrate paleontology, biostratigraphy, ichnology, micropaleontology, and paleoecology.

For the geophysics position, we are seeking a geoscientist with expertise in basic and applied energy exploration, and who is able to teach courses in seismic exploration and earthquake seismology, as well as providing other teaching activities to prepare students for the oil and gas industry. Specific areas of specialization include, but not limited to, seismic interpretation, reservoir characterization, and microseismicity-passive seismic.

The successful candidates are expected to work across disciplines within the Boone Pickens School of Geology and collaborate with faculty specializing in petroleum geology, environmental geology, hydrogeology, geochemistry, tectonics, and geophysics. We are seeking to fill the two positions with individuals who will develop vigorous and innovative externally funded research programs and who will contribute to teaching at both undergraduate and graduate levels. The successful candidates should be able to supervise MS and PhD students.

The School has state-of-the-art laboratories equipped with analytical instruments and computer hardware and software to facilitate teaching and research in the School’s areas of specialization. The School has a wealth of equipment for field acquisition of geological and geophysical data. The School also hosts the Devon Visualization Laboratory and operates a field camp facility near Cañon City, Colorado.

The application package for the positions should include a cover letter; curriculum vitae; three peer-reviewed publications; contact information for three references; and separate statements of research and teaching vision that include a brief description of how the applicant’s research will interface with that of the School’s faculty. In your cover letter, specify if you are applying for the paleontology/sedimentary geology position or the geophysics position. The application package should be submitted to: Assistant Professor Search, Boone Pickens School of Geology, 105 Noble Research Center, Oklahoma State University, Stillwater, Oklahoma 74078-3031 or electronically to: geolsearch@okstate.edu. Screening of candidates will begin on October 15, 2015 and will continue until the position is filled. Position is approved for active recruitment; however, appointment is contingent on available funding. More information about the Boone Pickens School of Geology can be found at http://geology.okstate.edu. Inquiries about the positions may be directed to Dr. Estella Atekwana (estella.atekwana@okstate.edu) or Dr. Jack Pashin (jack.pashin@okstate.edu).

Oklahoma State University is an AA/EEO/E-Verify employer committed to diversity. All qualified applicants will receive consideration for employment and will not be discriminated against based on race, color, religion, sex, sexual orientation, gender identity, national origin, disability or protected veteran status. OSU is a VEVRAA Federal Contractor and desires priority referrals of protected veterans for its openings. OSU-Stillwater is a tobacco-free campus.

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2) One-Year Visiting Position in Petrology and Plate Tectonics, Calendar Year 2016 – University of North Carolina at Chapel Hill 

The Department of Geological Sciences at UNC Chapel Hill invites applications for a one-year sabbatical replacement/postdoctoral position beginning 1 January 2016. The successful candidate will specialize in petrology and related fields and will be expected to teach two courses, conduct their own research, be a lively part of the department environment, and assist with student research. Teaching responsibilities comprise Petrology and Plate Tectonics (core course for majors) in the Spring 2016 semester, and a course of the candidate’s choice in Fall 2016.

Relevant facilities at UNC include two thermal ionization mass spectrometers for U-Pb geochronology and Sr, Nd, and Pb isotope geochemistry; an Element2 ICPMS with laser ablation; XRF; XRD; an SEM with EDS, BSE, and CL detectors; and a 1-atmosphere experimental petrology lab.

Applicants should apply via http://unc.peopleadmin.com/postings/81384 and by emailing the following with subject Petrology Search to the department’s Administrative Manager, Dr. Elizabeth Mullane Steadman, at emullane@unc.edu:

– concise letter of interest

– concise statement of teaching interests and experience

– curriculum vitae

– summary of research plans

– contact information for two references

Specific questions about the position should be directed to Prof. Allen Glazner, afg@unc.edu; information about the department is at http://www.geosci.unc.edu/. Review of applications will begin on 15 August 2015 and will continue until the position is filled. The University of North Carolina at Chapel Hill is an equal opportunity and affirmative action employer. All qualified applicants will receive consideration for employment without regard to age, color, disability, gender, gender expression, gender identity, genetic information, race, national origin, religion, sex, sexual orientation, or status as a protected veteran.

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Please note, new job announcements (usually) will be distributed to the GeoPRISMS Listserv on the 1st and 15th of each month.
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Reminder: 2015 GeoPRISMS Theoretical and Experimental Institute on Subduction Cycles and Deformation

Apply before August 21!

The Theoretical and Experimental Institute (TEI) for the Subduction Cycles and Deformation (SCD) initiative is now open for applications. The TEI is held on the three full days of October 12-14 and is intended to provide a summary of progress made in the science objectives of the SCD initiative (as discussed in the Science and Implementation plan available through geoprisms.nineplanetsllc.com). Applicants do not have to have worked on projects funded by GeoPRISMS. We expect a broad and diverse audience drawn from domestic and international researchers, including graduate students and early career scientists, who are interested in the structure and dynamics of subduction zones.

Funding

The TEI is funded by the National Science Foundation through the GeoPRISMS Office at the University of Michigan. There is no registration fee. Due to space restrictions the meeting will be strictly limited to 150 participants. We will be able to cover on-site expenses (venue costs, hotel expenses based on double occupancy, and breakfast+lunch) for up to 120 participants. Most participants will have to cover travel to and from the meeting. Partial funding for travel is available for students and postdocs. We will not be able to provide dinner on-site but there are plenty of restaurants nearby.

Confirmed participants whose on-site expenses are covered are expected to arrive on Sunday afternoon and leave on Thursday morning.

Organizing Committee

Jeff Freymueller (University of Alaska Fairbanks), Sarah Penniston-Dorland (University of Maryland), Donna Shillington (Columbia/LDEO), Kelin Wang (Pacific Geoscience Centre), Erin Wirth (University of Washington), Gene Yogodzinski (University of South Carolina). Ex officio: Peter van Keken (GeoPRISMS Office/University of Michigan).

Important Dates

Monday July 27: Applications are invited via the meeting webpage at /tei-scd-2015/

Friday August 21: Application deadline

Friday August 28: Successful applicants are invited to confirm participation

Friday September 11: Deadline for confirmation of attendance

Late September: Final meeting agenda is released

Location

The Portofino hotel at Redondo Beach, CA. The hotel is located just 8 miles (13 km) south of the main Los Angeles airport (LAX). Shuttle service is available for transport from and to the airport in addition to cab services).

Student and postdoc symposium

On Sunday before the meeting we will hold a student and postdoc symposium which will feature short presentations by the attendees and discussion with the conveners and NSF program managers. The meeting starts at 3 pm. We encourage all students and postdocs to attend and to arrange their travel accordingly, after confirmation of attendance.

Draft agenda

The agenda will develop as the list of participants is completed. We will have five sessions focused on different components of the subduction system (each featuring a keynote speaker and invited and contributed presentations) and a summary session. There will be ample time for discussion. We will have dedicated poster sessions in the afternoons.

Sessions with confirmed keynote and invited speakers:

The Incoming Plate
          Keynote: Doug Wiens (Washington University)
          Invited: Magali Billen (UC Davis)
The shallow fore-arc
          Keynote:  Kerry Key (UCSD)
          Invited: Nathan Bangs (UTIG)
The Megathrust
          Keynote: Laura Wallace (UTIG)
          Invited: Rocco Malservisi (USF)
Slab Processes
          Keynote: Brad Hacker (UC Santa Barbara)
          Invited: Pierre Bouilhol (Durham)
Mantle wedge and arc crust
          Keynote: Peter Kelemen (Columbia)
          Invited: Ellen Syracuse (LANL)

Possible field trip to Santa Catalina Island

We may be able to organize an optional field trip (led by Sarah Penniston-Dorland) to Santa Catalina Island on Thursday October 15. This will give participants the opportunity to see amphibolite- and blueschist-facies rocks that have been exhumed from a paleosubduction zone. There is no NSF funding for this trip and participants will need to cover all expenses. We estimate that the cost (including transport from hotel to ferry terminal, ferry ride, transport on Catalina, breakfast and lunch; accommodation at the Portofino for one more night) is around $400-$500 per person. The departure time from the hotel (to catch the first ferry to the island) will be at 5:15am. Cost for participants who do not require an additional night of accommodation will be adjusted. Capacity for the field trip is limited and we will confirm participants on a first-come, first-served basis after receipt of payment.

If you are interested in participating in the field trip please send an email to Peter van Keken (keken@umich.edu) as soon as possible but certainly before the application deadline. We will follow up with details on logistics. Payment to confirm participation will be due by the end of August.

REMINDER: 2015 GeoPRISMS Theoretical and Experimental Institute on Subduction Cycles and Deformation


The Theoretical and Experimental Institute (TEI) for the Subduction Cycles and Deformation (SCD) initiative is now open for applications. The TEI is held on the three full days of October 12-14 and is intended to provide a summary of progress made in the science objectives of the SCD initiative (as discussed in the Science and Implementation plan available through geoprisms.nineplanetsllc.com). Applicants do not have to have worked on projects funded by GeoPRISMS. We expect a broad and diverse audience drawn from domestic and international researchers, including graduate students and early career scientists, who are interested in the structure and dynamics of subduction zones.

Funding
The TEI is funded by the National Science Foundation through the GeoPRISMS Office at the University of Michigan. There is no registration fee. Due to space restrictions the meeting will be strictly limited to 150 participants. We will be able to cover on-site expenses (venue costs, hotel expenses based on double occupancy, and breakfast+lunch) for up to 120 participants. Most participants will have to cover travel to and from the meeting. Partial funding for travel is available for students and postdocs. We will not be able to provide dinner on-site but there are plenty of restaurants nearby.
Confirmed participants whose on-site expenses are covered are expected to arrive on Sunday afternoon and leave on Thursday morning.
Organizing Committee
Jeff Freymueller (University of Alaska Fairbanks), Sarah Penniston-Dorland (University of Maryland), Donna Shillington (Columbia/LDEO), Kelin Wang (Pacific Geoscience Centre), Erin Wirth (University of Washington), Gene Yogodzinski (University of South Carolina). Ex officio: Peter van Keken (GeoPRISMS Office/University of Michigan).
Important Dates
Monday July 27: Applications are invited via the meeting webpage at /tei-scd-2015/
Friday August 21: Application deadline
Friday August 28: Successful applicants are invited to confirm participation
Friday September 11: Deadline for confirmation of attendance
Late September: Final meeting agenda is released
Location
The Portofino hotel at Redondo Beach, CA. The hotel is located just 8 miles (13 km) south of the main Los Angeles airport (LAX). Shuttle service is available for transport from and to the airport in addition to cab services).
Student and postdoc symposium
On Sunday before the meeting we will hold a student and postdoc symposium which will feature short presentations by the attendees and discussion with the conveners and NSF program managers. The meeting starts at 3 pm. We encourage all students and postdocs to attend and to arrange their travel accordingly, after confirmation of attendance.
Draft agenda
The agenda will develop as the list of participants is completed. We will have five sessions focused on different components of the subduction system (each featuring a keynote speaker and invited and contributed presentations) and a summary session. There will be ample time for discussion. We will have dedicated poster sessions in the afternoons.

Sessions with confirmed keynote and invited speakers:

The Incoming Plate
          Keynote: Doug Wiens (Washington University)
          Invited: Magali Billen (UC Davis)
The shallow fore-arc
          Keynote:  Kerry Key (UCSD)
          Invited: Nathan Bangs (UTIG)
The Megathrust
          Keynote: Laura Wallace (UTIG)
          Invited: Rocco Malservisi (USF)
Slab Processes
          Keynote: Brad Hacker (UC Santa Barbara)
          Invited: Pierre Bouilhol (Durham)
Mantle wedge and arc crust
          Keynote: Peter Kelemen (Columbia)
          Invited: Ellen Syracuse (LANL)
Possible field trip to Santa Catalina Island
We may be able to organize an optional field trip (led by Sarah Penniston-Dorland) to Santa Catalina Island on Thursday October 15. This will give participants the opportunity to see amphibolite- and blueschist-facies rocks that have been exhumed from a paleosubduction zone. There is no NSF funding for this trip and participants will need to cover all expenses. We estimate that the cost (including transport from hotel to ferry terminal, ferry ride, transport on Catalina, breakfast and lunch; accommodation at the Portofino for one more night) is around $400-$500 per person. The departure time from the hotel (to catch the first ferry to the island) will be at 5:15am. Cost for participants who do not require an additional night of accommodation will be adjusted. Capacity for the field trip is limited and we will confirm participants on a first-come, first-served basis after receipt of payment.
If you are interested in participating in the field trip please send an email to Peter van Keken (keken@umich.edu) as soon as possible but certainly before the application deadline. We will follow up with details on logistics. Payment to confirm participation will be due by the end of August.

Job Postings: Faculty Positions


1) Faculty Positions – Scripps Institution of Oceanography, UCSD

2) Assistant Professor of Earth and Atmospheric Science (Exploration Geophysics) – University of Nebraska-Lincoln

3) Tenure-track Assistant Professor in Structural Geology/ Neotectonics – Department of Geography, Geology and Planning, Missouri State University

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1) Faculty Positions – Scripps Institution of Oceanography, UCSD

Scripps Institution of Oceanography at the University of California San Diego seeks up to two outstanding candidates from a broad range of disciplines within the Earth and Planetary Sciences, including geochemistry, tectonic processes, theoretical and computational geophysics, seismology, and marine and terrestrial geodesy.

For full description and to apply by September 15, 2015 deadline, go to:

Assistant Professor at: https://apol-recruit.ucsd.edu/apply/JPF00843

Associate/Full Professor at: https://apol-recruit.ucsd.edu/apply/JPF00852

UCSD is an AA/EOE/M/F/D/V.

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2) Assistant Professor of Earth and Atmospheric Science (Exploration Geophysics) – University of Nebraska-Lincoln

Applications are invited for a tenure track position as Assistant Professor in the Department of Earth and Atmospheric Sciences at the University of Nebraska-Lincoln. The successful candidate will be expected to participate in teaching and curricular development of undergraduate and graduate courses, to advise and direct graduate students, and to develop a rigorous research program that is supported by external funding. It is expected that the research program will include field and subsurface-based studies of exploration geophysics. Ability to contribute to growing petroleum geoscience-related teaching and research activities within the Department of Earth & Atmospheric Sciences will be considered as an advantage. The candidate should demonstrate strong potential for research and teaching and must hold a Ph.D. in Geology, Geophysics, or a related field at the time of appointment.

The Department of Earth and Atmospheric Sciences offers B.S. degrees in Geology and Meteorology-Climatology, as well as M.S. and Ph.D. degrees in Earth and Atmospheric Sciences. Primary research areas within the geological sciences include sedimentary geology, paleontology and paleobiology, petroleum geosciences and geobiology. Research in atmospheric sciences is focused on meterological hazards, climate change, and remote sensing. Additional active research areas include Climate System Science, Geoscience Education and Hydrological sciences. Additional information about our department can be found on our web site: http://eas.unl.edu.

To apply, go to http://employment.unl.edu, search for requisition #F_150159 and complete the “faculty/administrative form”. Applicants must attach a cover letter, curriculum vitae, statements of research and teaching interests, and names of at least three references via the above website. We will begin to review applications on October 12, but the position will remain open until it is filled.

The University of Nebraska is committed to a pluralistic campus community through affirmative action, equal opportunity, work-life balance, and dual careers.

For further information, contact Dr. Chris Fielding, Search Committee Chair by email, phone, or mail at: cfielding2@unl.edu, 1-402-472-9801; Department of Earth & Atmospheric Sciences, University of Nebraska-Lincoln, 214 Bessey Hall, Lincoln NE 68588-0340.

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3) Tenure-track Assistant Professor in Structural Geology/ Neotectonics – Department of Geography, Geology and Planning, Missouri State University

The Department of Geography, Geology, and Planning invites applications for a tenure-track position in Geology at the rank of Assistant Professor to begin in either January 2016 or August 2016 with an emphasis in either Structural Geology or Neotectonics.

A Ph.D. (or ABD) in Geology or a closely related field is required at time of appointment. Requirements include a commitment to undergraduate- and Master’s-level teaching as well as research expertise and interest at a level appropriate to supervise Master’s-level thesis projects. The successful applicant will teach an undergraduate course in structural geology and one or more upper-level courses in his or her specialty. Additionally, the individual will also teach introductory-level geology courses, and participate in department-level field trips. Post-doctoral research experience and evidence of teaching effectiveness would be advantageous. Applicants must be able to demonstrate knowledge of and the ability to work in an environment that encourages an understanding of, respect for, and development of skills to engage with those of other cultures or diverse backgrounds.

The Department grants undergraduate degrees in Geology, Geography, Planning, Geospatial Science, and Earth Science Education and an M.S. in Geospatial Science in Geography, Geology and Planning. The successful applicant would be expected to teach and advise in the undergraduate program in Geology and in the department’s graduate program.

Qualified applicants should apply online at jobs.missouristate.edu and upload a single PDF that includes a letter of application, current curriculum vitae, detailed research plan, statement of teaching philosophy, and contact information for 3–5 professional references. The evaluation of applications will begin September 15, 2015, and will continue until a successful candidate is found. Further information can be obtained at +1-417-836-5800, or visit our web site at geosciences.missouristate.edu. The University is dedicated to the goal of building a culturally diverse and inclusive faculty and staff committed to teaching and working in a multicultural environment and strongly encourages applications from women, persons from underrepresented ethnic and racial groups, individuals with disabilities and covered veterans. Employment will require a criminal background check at University expense. Missouri State University is an Equal Opportunity/Affirmative Action/Minority/Female/Veterans/Disability employer and institution.

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Please note, new job announcements (usually) will be distributed to the GeoPRISMS Listserv on the 1st and 15th of each month.

More sessions of Interest at the 2015 AGU Fall Meeting


Please see below for more sessions of interest to the GeoPRISMS Community, taking place at the 2015 AGU Fall Meeting, December 14-18 in San Francisco. Note, AGU abstract submission deadline is August 5, 2015.

Submit your abstract: http://fallmeeting.agu.org/2015/abstract-submissions/

T031. Marine Sedimentary Records of Climate-Tectonic Interactions

T035. Oceanic and arc lithospheres: clues from modern examples and ophiolites

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T031. Marine Sedimentary Records of Climate-Tectonic Interactions

Session ID#: 8742

Theoretical considerations and field studies suggest that geodynamic and surficial processes are coupled within orogens. This session focuses on the evolution of orogens and associated diffuse plate boundary zones through the analysis of marine sedimentary strata where there is a greater potential for a well-dated, continuous record of these interactions. This session is timely given several recent scientific ocean drilling expeditions with the explicit objective to distinguish and quantify cause and effect relationships between tectonics and climate, particularly in areas of rapid sedimentation where the potential resolution of events is greatest. Presentations are encouraged that highlight the development and/or application of novel techniques, including but not limited to geophysical, geochemical, isotopic, and thermochronometric techniques as applied to marine sediments to study the temporal evolution of potentially coupled climate-geodynamic systems. We particularly welcome submissions on the Bengal, Indus and Nicobar Fans in the Indian Ocean.

Invited Presenters
Peter Clift – Louisiana State University
Ken Ridgeway – Purdue University

Volkhard Spiess –  University of Bremen

Conveners:
Jonathan M Bull, University of Southampton
John M Jaeger, Univ Florida
Sean Gulick, University of Texas at Austin

Kolluru Sree Krishna, National Institute of Oceanography, Panjim, India

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T035: Oceanic and arc lithospheres: clues from modern examples and ophiolites

Session ID#: 8985

Much of what has been learned from Alpine-Himalayan ophiolite studies in the last ~50 years, despite lingering debate as to their exact genetic setting, has been widely used to interpret the structure of the oceanic lithosphere flooring modern oceans. In contrast, most Pacific ophiolitic complexes have been interpreted as newly created supra-subduction lithosphere formed in Arc to Forearc settings.

Intriguingly, the comparatively abundant studies of crustal and lithospheric structures formed at modern Mid Ocean Ridge, Back-arc, Arc, and Forearc settings have rarely been used to elucidate the nature of ophiolites and constrain where and how most ophiolites formed.

In an attempt to reconcile these contrasting views and approaches, we incite an across-communities discussion (with contributions from marine geology and geophysics, petrology-geochemistry, tectonics, ophiolite studies) to reexamine the link between modern oceans and arcs and their past ophiolitic analogues, and better assess what ophiolites tell us.

Conveners:
Cesar R Ranero, ICM-CSIC
Philippe Agard, University Pierre and Marie Curie Paris VI
Mathilde Cannat, Institut de Physique du Globe de Paris
Robert J Stern, Univ Texas Dallas

Reminder: Apply to host a GeoPRISMS Distinguished Speaker


GeoPRISMS Distinguished Lectureship Program (DLP), 2015-2016 Season

Deadline: August 1, 2015

DLP Speakers 2015-2016

The GeoPRISMS Office is happy to announce the annual GeoPRISMS Distinguished Lectureship Program for academic year 2015-2016 with an outstanding speakers list. Distinguished scientists involved with GeoPRISMS science are available to visit US colleges and universities to present technical and public lectures on subjects related to GeoPRISMS science.

Any US college or university can apply to host a DLP speaker. Applications are due August 1, 2015 for visiting speakers in Fall 2015 and Spring 2016. Institutions that are not currently involved with GeoPRISMS research are strongly encouraged to apply, including those granting undergraduate or masters degrees, as well as those with PhD programs. Institutions may request a technical and/or public lecture. The GeoPRISMS Office will cover airfare for speakers’ travel and will coordinate travel and off-site logistics. Host institutions are responsible for local expenses for the duration of the visit.

Visit the GeoPRISMS website to apply and learn more about the speakers and talks available:

/education/distinguished-lectureship-program/

Also, please review the DLP Best Practices for making the most of your visiting speaker:

/education/distinguished-lectureship-program/geoprisms-dlp-best-practices/

Please direct any questions to the GeoPRISMS Office at info@geoprisms.nineplanetsllc.com

The GeoPRISMS Office

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2015-2016 Speakers:

Elizabeth Cottrell (Smithsonian Institution)
     Public Lecture: Volcanoes: Windows to the Deep
     Technical Lecture: Oxygen Cycling Through Subduction Zones and the Generation of Continents
Bradley Hacker (UC, Santa Barbara)
     Public Lecture: Earth’s Tempo: The Bleeding Edge of Geochronology
     Technical Lecture: Differentiation of the Continental Crust by Relamination
Beatrice Magnani (Southern Methodist University)
     Public Lecture: The legacy of ancient plate boundaries in continental intraplate deformation
     Technical Lecture: From plate boundary to intraplate: understanding the role of paleotectonic structures in continental intraplate deformation
Andy Nyblade (Penn State University)
     Public Lecture: The formation of the Great Rift Valley in East Africa:  Is there a Connection with Human Origins?
     Technical Lecture: Cenozoic Rifting, Plateau Uplift, and Volcanism in Eastern Africa and the African Superplume
Robert J. Stern (University of Texas at Dallas)
     Public Lecture: Geoscientific Investigations of the Southern Mariana Trench and the Challenger Deep
     Technical Lecture: Convergent Plate Margins, Subduction Zones, and Island Arcs
Laura Wallace (University of Texas at Austin)
     Public Lecture: The slow slip revolution: Leading to a better understanding of earthquakes
     Technical Lecture: Sticky or Slippery? Controls on subduction megathrust behavior at the Hikurangi subduction margin, New Zealand

More Sessions of Interest at the 2015 AGU Fall Meeting

Please see below for more sessions of interest to the GeoPRISMS Community, taking place at the 2015 AGU Fall Meeting, December 14-18 in San Francisco. Note, AGU abstract submission deadline is August 5, 2015.

See http://fallmeeting.agu.org/2015/

Submit your abstract: http://fallmeeting.agu.org/2015/abstract-submissions/

T015. Cumulative deformation in the overlying plate due to subduction and related feedbacks
T021. From the seismic cycle to geological time scales, how do subduction processes that can possibly modify the megathrust geometry and mechanical properties control the tectonic evolution and deformation of active margins, and the subduction seismic behavior?
T037. Revisiting the Tectonics, Regional Structure, and Geodynamics of Alaska and the North Pacific
T038. Rifts and Passive Margins: Tectonics, Dynamics, Processes
T039. Scientific advances from subduction zone observatories
T043. Subduction across scales
V002. 4D Variations in Cascade Arc Magmatic Systems: Linking Tectonics, Geochemistry, and Geodynamics
V011. Geochemistry of sediments and sediment recycling and implications for crust and mantle evolution over Earth history”
V018. How and when do volcanic eruptions start and stop, and what controls the tempo of everything in between?
V027. Quantifying Storage, Transport, and Volumes of Magmas in the Earth’s Crust
V032. The Earth’s geodynamic carbon cycle: subduction, storage, migration, and outgassing
V034. The ophiolite-subduction connection: Using peridotites as analogs for subduction zone mantle
V045. Where Arc Magmas Reside: Comparing the Volcanic and Plutonic Records
MR020. The spectrum of slip behaviors of continental and subduction fault zones
DI007. Geochemical and geophysical links between subduction zone dynamics and arc systems
S027. Unraveling the complexities of mantle flow, crustal rotation and crustal faulting in the Cascade subduction zone system
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T015. Cumulative deformation in the overlying plate due to subduction and related feedbacks

Session ID#: 8167

Subduction over time modifies the overriding plate by fractionation, accretion, and tectonic deformation. This can lead to processes such as tectonic shortening (orogeny), regional uplift, weakening by back-arc spreading and volcanism, basin formation, and/or destabilization of the lithosphere. In turn, the composition, strength, and morphology of the overlying plate, which may be the product of a long geological history and have significant along-strike variations, can affect current large-scale subduction dynamics such as slab dip, and ultimately broad-scale plate kinematics in two and three dimensions. Examples of geological settings that bear witness to these processes are found along the Pacific Rim, the Tethys margin, including the Mediterranean mobile belt, and northwestern North America. We seek contributions from all disciplines, including geodesy, geology, geochemistry, seismology, and geodynamics, that document the tectonic evolution of overlying plate deformation and their link to subduction processes.

Invited speakers:
Fabio Capitanio, Monash Univ.
Huw Davies, Cardiff Univ.
Tatsuya Ishiyama, U. Tokyo/ERI

Onno Oncken, GFZ-Potsdam U.

Conveners:
Hiroshi Sato (University of Tokyo)
David A Okaya (University of Southern California)
Susan M Ellis (GNS Science)

Thorsten W Becker (University of Southern California)

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T021. From the seismic cycle to geological time scales, how do subduction processes that can possibly modify the megathrust geometry and mechanical properties control the tectonic evolution and deformation of active margins, and the subduction seismic behavior?

Session ID#: 7866

A fundamental feature of overriding plates is that on 100  to 107yr time-scales, they deform both abruptly and dramatically or slowly and subtly in response to an array of distinct subduction processes, among which are earthquake cycles, subducting ridges, and erosion/accretion. Over short time-scales, the pattern of upper-plate vertical deformation is dominated by subduction seismic cycles controlled by the megathrust structure and mechanical properties. Over longer time-scales, upper-plates present various vertical deformation patterns, which can be transient, vary along-strike, reflect long lasting elastic behavior (no permanent deformation) or not (building of permanent topography). Consequently, observations of long-term vertical deformation offer clues to investigate the structure, properties and processes enveloping the interplate thrust zone and their significance regarding subduction seismic behavior. This session welcomes insights focusing on active deformation at convergent margins through observations and modeling that seek to integrate the different time-scales to comprehend the factors controlling subduction zone behavior.

Conveners:
Frédérique Leclerc, Earth Observatory of Singapore
Frederick W Taylor, Institute for Geophysics, Austin
Nathalie Feuillet, Institut de Physique du Globe de Paris

Luc L Lavier, Jackson School of Geosciences, Austin

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T037. Revisiting the Tectonics, Regional Structure, and Geodynamics of Alaska and the North Pacific

Session ID#: 9027

The Pacific-North American plate boundary in Alaska is in the scientific spotlight now because of the spectacular geology and tectonic processes preserved and ongoing in the region, and the major financial investment by the National Science Foundation through EarthScope and GeoPRISMS. It is timely to review the available data and tectonic-geodynamic models, as several major new scientific efforts are now in their infancy. Certain tectonic components have a first order effect, including the impact of the subduction of the Yakutat terrane, and the role of lithospheric heterogeneity from broad scales to more localized zones of weakness, such as the Denali fault. In this diffuse plate boundary, active deformation is partitioned across a large area, including related tectonic systems in Canada and Russia. We welcome submissions using observational and modeling studies relevant to the Alaska-Aleutian subduction zone and the North Pacific region, including new work and review or integrative submissions.

Conveners:
Jeffrey Todd Freymueller, University of Alaska Fairbanks
Margarete Ann Jadamec, University of Houston

Douglas H Christensen, University of Alaska Fairbanks

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T038. Rifts and Passive Margins: Tectonics, Dynamics, Processes

Session ID#: 7198

This session presents recent advances on rifts and passive margins from geological and geophysical studies that are based on seismic interpretation, field geological data, plate reconstructions, sedimentology, and modeling.

We aim to assemble presentations on basin, regional and global scale that provide new insight on rift evolution in terms of inheritance and strain localization, fault interaction and stratigraphy, partial melting and volcanism, surface stress evolution, tectonics-climate interaction, small-scale convection, driving forces, and rift-to-drift transition. Most rifts feature significant along-strike structural variations. We therefore particularly encourage abstract submission on 2D investigations with regional perspective, 3D seismic arrays, as well as 3D analogue and numerical experiments.

Special emphasis will be put on contributions that develop an integrated picture by bridging multiple spatial or temporal scales or by combining results from active rifts, failed rift arms, passive margins or obducted rifted margins.

Conveners:
Sascha Brune, University of Sydney
Peter Dominic Clift, Louisiana State University
Gwenn Péron-Pinvidic, Geological Survey of Norway

Giacomo Corti, Instituto di Geoscienze e Georisorse

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T039. Scientific advances from subduction zone observatories

Session ID#: 7617

Subduction zones contain the Earth’s richest diversity of tectonic processes, from plate-scale over millennia to grain-scale over micro-seconds. Most span continental to oceanic environments, and interact with climatological and biological processes, which multiplies the diversity and observational challenges, but also opportunities to leverage and learn.  Finally, subduction zones host many of Earth’s most extreme natural events, which coupled with increasing human populations, leads to an urgent need to understand how they work. The scientific community is exploring the potential to develop a new Subduction Zone Observatory (SZO) as a multidisciplinary facility, stretching along several circum-Pacific’s subduction zones.  A SZO would provide a comprehensive suite of multidisciplinary onshore and offshore observations to understand the entire subduction zone system.  We welcome contributions that show scientific advances resulting from coordinated instrumentation, sampling, and analog experimentation/modeling of a subduction zone, or present scientific ideas and findings relevant to future development of a SZO.

Conveners:
Joan S Gomberg, USGS Western Regional Offices Seattle
Douglas A Wiens, Washington University in St Louis
Katherine A Kelley, University of Rhode Island

Anne Meltzer, Lehigh University

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T043. Subduction across scales

Session ID#: 8926

Both risk assessment and lithosphere dynamics call for a better understanding of subduction zones, particularly along and across the  subduction interface.

How can we bridge the gap between observations made at rock and plate scale, or between signals lasting from seconds to million years? Are we able to image and understand physical conditions and processes at work along the subduction interface at relevant scales, such as years and meters?

Time has come to further our understanding of the nature and structure of the subduction interface and elucidate which lithologies are incorporated and how, which rheological behaviours prevail, which fluids are there and where, or what is their exact bearing on earthquake ruptures.

Building on the recent wealth of geophysical and petrological data and models gathered on the plate-slab interface, we welcome stimulating contributions from all disciplines, seeking to foster joint collaboration and bridge the gap between the various communities.

Conveners:
Philippe Agard, University Pierre and Marie Curie Paris VI
Kelin Wang, Geological Survey of Canada Sidney
Luce Fleitout, Ecole Normale Supérieure Paris

Bradley R Hacker, University of California Santa Barbara

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V002. 4D Variations in Cascade Arc Magmatic Systems: Linking Tectonics, Geochemistry, and Geodynamics

Session ID#: 9089

This session draws together researchers in tectonics, geophysics, geochronology, geochemistry, and dynamic modeling to improve our spatial and temporal understanding of the Cascades magmatic arc. Since its enigmatic inception about 40 Ma, the arc has undergone significant changes in magmatic productivity and composition. In addition, the Cascades are volcanically and tectonically segmented into regions that differ in volcanic style, flux, and composition, as well as in faulting style, degree of crustal rotation, and relative uplift. These spatio-temporal variations may reflect differences in subduction rate or angle, the nature of the lower and upper plate, and regional tectonics. Can we determine which of these relationships are causative, and can we derive a geodynamic model for the variability of volcanism and plutonism through space and time? We seek contributions from researchers with geochemical or geophysical data sets, conceptual or numerical models, and other approaches that illuminate and help address these fundamental questions.

Conveners:
Bradley W Pitcher, Oregon State University
Thomas W Sisson, USGS, Menlo Park
Patricia A McCrory, USGS California Water Science Center Menlo Park

Haiying Gao, University of Massachusetts Amherst

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V011. Geochemistry of sediments and sediment recycling and implications for crust and mantle evolution over Earth history

Session ID#: 8150

Sedimentary rocks record information on diverse topics such as environmental conditions from the distant past, the average composition of the continents, and the redox state of the oceans and atmosphere.  Although much of the Earth’s sedimentary record has been removed from our view by subduction processes, a long term consequence may be that the mantle “sees” and is influenced by Earth surface conditions.  We seek a broad range of contributions that deal with the record of continental evolution and the rise of oxygen, seen both in the sedimentary record and also potentially in igneous systems as a result of sediment recycling over Earth history.

Conveners:
Richard M Gaschnig, University of Maryland College Park
Xiao-Ming Liu, Carnegie Institution of Washington

Elizabeth A Bell, University of California Los Angeles

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V018. How and when do volcanic eruptions start and stop, and what controls the tempo of everything in between?

Session ID#: 8269

There is much information now accumulating about the timing of volcanic eruptions, from the millennia (or longer) for the accumulation of magma into its eruptible state through to real-time observations of contemporary eruptive activity. A key aim of volcanology is to forecast the course of future events and provide advice on the timing and processes at ongoing eruptions on timescales that are relevant to humanity and with a degree of confidence about the processes involved. We invite contributions that address all the facets of this topic. These might include (1) magmatic forensics of past eruption products that contribute to accurate assessment of timescales and processes in past events; (2) studies of modern eruptions and the controls on their durations, including prolonged, multi-episode events; and (3) how temporal information about magmatic and volcanic processes can be translated into sound and useful advice to civil authorities for managing ongoing and future events.

Conveners:
Colin J N Wilson, Victoria University of Wellington
Michelle L Coombs, Alaska Volcano Observatory Anchorage, USGS
Bruce F Houghton, University of Otago

Paul J Wallace, University of Oregon

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V027. Quantifying Storage, Transport, and Volumes of Magmas in the Earth’s Crust

Session ID#: 9804

When, where and for how long magmas are stored within the Earth and how they contribute to the crustal chemical, physical and thermal architecture remain important challenges in geosciences. Magmatic bodies have been detected with a wide range of geophysical approaches; however, the volumes, mechanics, chemical signatures and evolution of these bodies remain poorly constrained. We seek contributions that utilise field, numerical and experimental methods to address the following key themes: (i) how do we detect magmas bodies and do we determine their states and volumes in the Earth’s crust, (ii) how can we quantify chemical, mechanical and thermal processes that operate within those volumes, (iii) what can minerals, glass/melt and volatile emissions tell us about timescale of magmatic processes constructing the architecture of the continental crust, volcanoes and atmosphere. This session aims to foster cross-disciplinary interactions and collaborations between field geologists, geochemists, petrologists, volcanologists, geophysicists, and numerical modelers.

Conveners:
Mattia Pistone, Smithsonian Institution – National Museum of Natural History
Benoit Taisne, Earth Observatory of Singapore
Olivier Bachmann, ETH Swiss Federal Institute of Technology Zurich

Kate J Dobson, Ludwig Maximilian University of Munich

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V032. The Earth’s geodynamic carbon cycle: subduction, storage, migration, and outgassing

Session ID#: 8341

The carbon cycle is of fundamental importance to Earth processes over geologic time. However, the physics of deep carbonaceous reservoirs and the fluxe(s) between Earth’s interior (mantle) and exterior (crust, hydrosphere & atmosphere) remain enigmatic.

This session aims to promote the latest multidisciplinary research involving the behaviour of carbon within the subducted slab, crust, and mantle. We welcome contributions related to: (1) solubility and storage of carbon within Earth’s interior; (2) origin and migration of C-rich fluids and melts and their impact on redox processes, diamond formation, mantle metasomatism and associated (alkaline) magmatism; (3) the petrology of carbonaceous phases at extreme P-T conditions; (4) stable isotope fractionation; and (5) carbon release to the exosphere through volcanic, tectonic and other styles of degassing.

We invite contributions from volcanology, natural/experimental geochemistry/petrology, and mineral physics, as well as theoretical and computational studies. Submissions by early career scientists and graduate students are particularly encouraged.

Conveners:
Sami Mikhail, The University of St. Andrews
Anja Rosenthal, Bayerisches Geoinstitut
Vincenzo Stagno, Geodynamics Research Center, Matsuyama

Taryn Michelle Lopez, University of Alaska Fairbanks

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V034. The ophiolite-subduction connection: Using peridotites as analogs for subduction zone mantle

Session ID#: 8521

Supra-subduction zone ophiolites, which form in the mantle wedge of nascent subduction zones, preserve mantle lithologies that formed in response to hydrous melting. The refractory residuum of this process enhances our understanding of the geochemical flux in the mantle wedge and is critical to our understanding of the ‘subduction factory’ and resulting arc volcanism. The resulting architecture of these ophiolites demonstrates that they are petrologically and chemically distinct from igneous rocks formed at modern spreading centers in the major ocean basins. Abstracts addressing ophiolite petrogenesis with respect to subduction initiation, peridotite geochemistry, extent and nature of melt extraction, extent of fluid flux through the mantle wedge, and subsequent mantle-melt interactions are welcomed. This session aims to integrate the chemical and physical structure of the mantle wedge, address controversial origins of well-known ophiolites, and discuss the diversity in the architecture and geochemical fingerprints observed in ophiolites.

Conveners:
Marlon M Jean, Luh Institut Fuer Geologie, Hannover
John W Shervais, Utah State University

Véronique Le Roux, Woods Hole Oceanographic Inst

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V045. Where Arc Magmas Reside: Comparing the Volcanic and Plutonic Records

Session ID#: 9834

Magmatic processes are powerful agents for creating and reworking the Earth’s crust. Passage and stalling of magmas in arcs brings new material into the crust and drives interactions with wall rock, magma mixing and fractionation, leaving complex crystal histories in both volcanic and plutonic rocks. In intrusive terrains, field relationships, aureole or igneous thermobarometry, and physical modeling inform where magmas reside and get modified. Erupted magmas carry quenched time series of mineralogical and compositional imprints of their crustal traverse.  We invite contributions that use continental arc igneous assemblages to understand magma accumulation and residence in the crust, investigate magma-crust interactions and crustal assimilation, and the processes of magma mobility and eruptibility. We welcome discussions on the nature of plutonic versus volcanic rocks (cumulates/fractionates versus compositional equivalents) and volcanic-plutonic volume ratios. Contributions are welcome from petrology, geochemistry, geophysics, modelling and related fields.

Conveners:
Valbone Memeti, California State University Fullerton
Gary Michelfelder, Missouri State University
Anita Grunder, Oregon State University

Emily E. Salings, Missouri State University

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MR020. The spectrum of slip behaviors of continental and subduction fault zones

Session ID#: 8995

Recent global deployment of geophysical instrumentation produced a vast quantity of data, allowing major advances in the characterization of the slip behavior of continental/subduction fault zones. Complex modes of fault slip – including tectonic  tremor, tsunami earthquakes and slow earthquakes – have been observed in the transition zone at the up-dip and down-dip limits of the seismogenic zone. These behaviours complement classic views of fault slip behaviours, where fast, frictional sliding during earthquakes and slow, aseismic sliding during creep events occur along faults.

Although recent studies have proposed heterogeneities in fault structure, frictional properties and deformation mechanisms, to explain the broad spectrum of fault slip behavior, our understanding of these processes is still limited. We welcome multidisciplinary, innovative contributions addressing the mechanical/physical properties and sliding behaviours of fault zones during the seismic cycle through the integration of field, laboratory and seismological data.

Conveners:
Nicola De Paola, University of Durham
Cristiano Collettini, Sapienza University of Rome
Andre R Niemeijer, Utrecht University

Wenlu Zhu, University of Maryland College Park

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DI007. Geochemical and geophysical links between subduction zone dynamics and arc systems

Session ID#: 9788

This session aims to explore the complex processes linking subduction dynamics and arc volcanism. We focus particularly on reconciling geochemical and geophysical observables with dynamic processes.  Subduction zones exhibit heterogeneity in composition and thickness of subducting sediments, slab age and morphology, faulting characteristics, and thermal structure.  This heterogeneity leads to temporal and spatial variability in mantle flow, seismicity, magma composition and productivity, and rates of subduction and back-arc spreading. The physical-chemical conditions and processes in arc systems have been inferred from geophysical and geochemical observations, experimental rheologic data, and geodynamic modeling. We invite contributions from these disciplines and others that link the physical-chemical conditions at volcanic arcs and the underlying mantle wedge with the dynamic processes in subduction zones.

Invited presenters include:
Geoff Abers; Cornell University
Esteban Gazel; Virginia Tech
Chris Kincaid; University of Rhode Island

Cian Wilson; Lamont-Doherty Earth Observatory

Conveners:
Aubreya Nicole Adams, Colgate University
Erin A Wirth, Yale University
Ikuko Wada, International Research Institute of Disaster Science, Sendai, Japan

Maryjo N Brounce, University of Rhode Island Narragansett Bay

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S027. Unraveling the complexities of mantle flow, crustal rotation and crustal faulting in the Cascade subduction zone system

Session ID#: 8194

Recognition of the clockwise rotation of the Cascadia forearc, arc, and backarc from paleomagnetic and GPS observations represents one of the most exciting discoveries in subduction zone dynamics.  This discovery requires a new paradigm to understand how crustal faults accommodate this rotation in a framework that includes Basin and Range extension, the active magmatic arc, north-directed compression against stable Canada, and plate subduction along the megathrust.  The existing USGS Quaternary Fault database is woefully incomplete and does not explain the clockwise rotation of the crust.  A variety of recent studies have addressed this shortfall, including new geologic mapping, high-resolution airborne LiDAR, new potential field geophysical surveys, paleoseismic studies of identified scarps, and seismic imaging of known faults. This session seeks contributions that present recent findings and new kinematic and dynamic models to explain the role of mantle flow and crustal faulting in accommodating Cascadia rotation.

Conveners:
Thomas M Brocher, USGS, Menlo Park
Richard J Blakely USGS, Menlo Park
Brian L Sherrod USGS, Seattle
Andrew Patrick Lamb USGS, Menlo Park

2015 GeoPRISMS Theoretical and Experimental Institute on Subduction Cycles and Deformation


Apply now to attend the Theoretical and Experimental Institute for the SCD Initiative

The Theoretical and Experimental Institute (TEI) for the Subduction Cycles and Deformation (SCD) initiative is now open for applications. The TEI is held on the three full days of October 12-14 and is intended to provide a summary of progress made in the science objectives of the SCD initiative (as discussed in the Science and Implementation plan available through geoprisms.nineplanetsllc.com). Applicants do not have to have worked on projects funded by GeoPRISMS. We expect a broad and diverse audience drawn from domestic and international researchers, including graduate students and early career scientists, who are interested in the structure and dynamics of subduction zones.

Funding

The TEI is funded by the National Science Foundation through the GeoPRISMS Office at the University of Michigan. There is no registration fee. Due to space restrictions the meeting will be strictly limited to 150 participants. We will be able to cover on-site expenses (venue costs, hotel expenses based on double occupancy, and breakfast+lunch) for up to 120 participants. Most participants will have to cover travel to and from the meeting. Partial funding for travel is available for students and postdocs. We will not be able to provide dinner on-site but there are plenty of restaurants nearby.

Confirmed participants whose on-site expenses are covered are expected to arrive on Sunday afternoon and leave on Thursday morning.

Organizing Committee

Jeff Freymueller (University of Alaska Fairbanks), Sarah Penniston-Dorland (University of Maryland), Donna Shillington (Columbia/LDEO), Kelin Wang (Pacific Geoscience Centre), Erin Wirth (University of Washington), Gene Yogodzinski (University of South Carolina). Ex officio: Peter van Keken (GeoPRISMS Office/University of Michigan).

Important Dates

Monday July 27: Applications are invited via the meeting webpage at /tei-scd-2015/

Friday August 21: Application deadline

Friday August 28: Successful applicants are invited to confirm participation

Friday September 11: Deadline for confirmation of attendance

Late September: Final meeting agenda is released

Location

The Portofino hotel at Redondo Beach, CA. The hotel is located just 8 miles (13 km) south of the main Los Angeles airport (LAX). Shuttle service is available for transport from and to the airport in addition to cab services).

Student and postdoc symposium

On Sunday before the meeting we will hold a student and postdoc symposium which will feature short presentations by the attendees and discussion with the conveners and NSF program managers. The meeting starts at 3 pm. We encourage all students and postdocs to attend and to arrange their travel accordingly, after confirmation of attendance.

Draft agenda

The agenda will develop as the list of participants is completed. We will have five sessions focused on different components of the subduction system (each featuring a keynote speaker and invited and contributed presentations) and a summary session. There will be ample time for discussion. We will have dedicated poster sessions in the afternoons.

Sessions with confirmed keynote and invited speakers:

The Incoming Plate
          Keynote: Doug Wiens (Washington University)
          Invited: Magali Billen (UC Davis)
The shallow fore-arc
          Keynote:  Kerry Key (UCSD)
          Invited: Nathan Bangs (UTIG)
The Megathrust
          Keynote: TBD
          Invited: Rocco Malservisi (USF)
Slab Processes
          Keynote: Brad Hacker (UC Santa Barbara)
          Invited: Pierre Bouilhol (Durham)
Mantle wedge and arc crust
          Keynote: Peter Kelemen (Columbia)
          Invited: Ellen Syracuse (LANL)

Possible field trip to Santa Catalina Island

We may be able to organize an optional field trip (led by Sarah Penniston-Dorland) to Santa Catalina Island on Thursday October 15. This will give participants the opportunity to see amphibolite- and blueschist-facies rocks that have been exhumed from a paleosubduction zone. There is no NSF funding for this trip and participants will need to cover all expenses. We estimate that the cost (including transport from hotel to ferry terminal, ferry ride, transport on Catalina, breakfast and lunch; accommodation at the Portofino for one more night) is around $400-$500 per person. The departure time from the hotel (to catch the first ferry to the island) will be at 5:15am. Cost for participants who do not require an additional night of accommodation will be adjusted. Capacity for the field trip is limited and we will confirm participants on a first-come, first-served basis after receipt of payment.

If you are interested in participating in the field trip please send an email to Peter van Keken (keken@umich.edu) as soon as possible but certainly before the application deadline. We will follow up with details on logistics. Payment to confirm participation will be due by the end of August.