Current Conference:
Eclogites in Space and Time – Bridging the Micro to Planetary Scales
Rohnert Park, California, USA | 19–23 June 2025
Know Before
You Go
Program and
Abstract Volume
Field Guide
(Non-Peer Reviewed)
Welcome
Welcome to Rohnert Park, California, for the 2025 GSA Penrose Conference, which will also represent
the 15th International Eclogite Conference (IEC-15). We are excited to bring together the
international community of scientists working on eclogites and subduction-zone processes to discuss
recent advances in diverse fields, catalyze breakthroughs in our understanding of subduction-zone
processes, and chart future research on eclogites in space and time. Our location near the Franciscan
subduction complex, which is among the first natural laboratories for the study of subduction
processes, provides a fitting location for the conference and field trips.
We are thrilled to have over 98 participants from 16 countries attend the Penrose 2025/IEC-15. Fifty-
six are Early Career scientists, including undergraduate and graduate students, postdoctoral fellows,
research scientists, and junior faculty. Since 1982, the eclogite community has organized a series of
international meetings and field trips focusing on high-pressure and ultrahigh-pressure processes
under the auspices of the International Eclogite Conference, and we look forward to continuing this
tradition of exchanging ideas and promoting collaboration.
We would also like to express our gratitude to our sponsors and supporting institutions for making
this conference possible.
On behalf of the convenors and field trip leaders, we hope you enjoy the Penrose 2025/IEC-15.
Chris Mattinson,
Central Washington University
Kennet Flores,
University of North Carolina at Chapel Hill
David Hernandez-Uribe,
University of Illinois Chicago
Suzanne Baldwin,
Syracuse University
International Eclogite Conference
Eclogites in Space and Time — Bridging the Micro to Planetary Scales
will represent the 15th meeting of the International Eclogite Conference
(IEC-15). The IEC was established in 1982 to promote worldwide
communication and cooperation among scientists who study high-pressure
and ultrahigh-pressure rocks and processes.
Find out more about the IEC
Description
The multidisciplinary study of eclogites from micro to planetary scales over the past 50 years has
significantly advanced our understanding of plate tectonics. Eclogites are both the recorders and drivers of
planetary-scale tectonics, and their formation is involved in such diverse processes as the geochemical exchange
between Earth’s surface and deep interior, intermediate-depth seismicity, and continental growth, collision, and
evolution.
Objectives
The objective of this Penrose Conference is to bring together the international eclogite community and
scientists working on subduction-zone processes to discuss recent advances in diverse fields (e.g., geodynamics,
geochemistry, experimental petrology, and geochronology); catalyze breakthroughs in our understanding of
subduction-zone processes; and chart future research on eclogites in space and time.
This Penrose Conference will represent the 15th International Eclogite Conference (IEC15) and will be the first
time U.S.-based scientists host the international eclogite community at a dedicated conference.
Conference Format
The conference format will include oral presentations, poster presentations, breakout discussions, and
mentoring opportunities for early career scientists. Attendees will be expected to observe the GSA Code of
Ethics & Professional Conduct throughout the meeting.
The venue is close to some of the classic localities of the Franciscan Complex, which we will visit during two
syn-conference field excursions. Learn more about the venue online.
Thematic Sessions
Eclogites, Micro to Macro Scales
What processes do eclogites and eclogite-facies rock reveal at different scales? How do new insights from
micro-scale observations on high-pressure and ultrahigh-pressure (HP–UHP) metamorphic rocks better constrain and
inform subduction-zone processes? This thematic session will explore the state of knowledge regarding bridging
the scales in eclogite research.
Advances in Methods: Thermobarometry and Geo/ Thermochronology
Mineral assemblages preserved in HP–UHP metamorphic rocks challenge the assumption that equilibrium was
attained during prograde, peak, and retrograde conditions. This thematic session will explore advances in
thermo-barometry and geo/thermochronologic techniques used to determine the
pressure-temperature-time-deformation (P-T-t-D) histories of eclogite and related rocks.
The Role of Eclogite in Geodynamics
This thematic session will explore how P-T-t paths and deformation histories of eclogites (and related
rocks) can be used to improve our understanding of paleogeothermal gradients, and thus the thermal evolution of
our planet. It will include how seismic tomography can be integrated with observations from exhumed rocks to
constrain the role of eclogites in Earth’s geodynamic evolution.
The Franciscan and HP–UHP Rocks of the Circum-Pacific Realm
The Franciscan Complex of California is among the first natural laboratories for the study of subduction zones
and subduction processes. This session will focus on how the Franciscan Complex and other HP–UHP terranes in the
circum-Pacific realm formed and survived exhumation
to Earth’s surface. This thematic session will also explore how HP–UHP exhumation mechanisms differ between
long-lived and transient subduction zones.
Rheology of the Subduction Interface: Deformation and Earthquake Processes
Can exhumed analogs in the subduction-related metamorphic rock record be used to constrain the rheology of the
slab–mantle interface? How does the process of serpentinization affect fore-arc deformation and fluid transport
in the mantle wedge? This thematic session will explore the rheology of the subduction interface as preserved in
both the seismicity of active subduction zones and the geologic evolution of exhumed HP-UHP terranes.
Fluids, Melts, and Geochemical (Re)cycling in Subduction Zones
What are the roles of fluids and melts in the geochemical cycling in subduction zones? This thematic session
will explore how observations on HP–UHP metamorphic rocks can constrain the sources, pressures, and volumes of
fluids in subduction zones.
Summary of Key Dates
15 February 2025 |
Registration and payment deadline.
Deadline for submission of final abstracts. |
Mid-March 2025 |
Conference program finalized. Presenters will be provided information on their
presentation mode (oral vs. poster) at this time. |
18 June 2025 |
Arrival in Rohnert Park, California, USA; Airport shuttle available from San Francisco
International Airport (SFO)
|
19-23 June 2025 |
Conference and Fieldtrips |
24 June 2025 |
Participants depart from Rohnert, CA; Airport shuttle to SFO available from hotel |
Lodging
Room costs are based on double occupancy rates. If you have a roommate preference, please indicate on your
registration form. We will attempt to accommodate attendees who request their own room, subject to room
availability and at an additional cost; please select this option at registration.
Meals
On conference days all meals will be provided at the hotel. On fieldtrip days, breakfast will be at the hotel,
a boxed lunch will be provided, and participants will be free to choose where to have dinner (i.e., dinners on
field trip days will be paid for by each participant; restaurant options will be provided). If you have
any dietary restrictions (vegan, vegetarian, food allergies, etc.), please indicate these on your registration
form so we can be sure your meal needs are accommodated.
Transportation
All attendees will be expected to make their own travel arrangements to arrive at the conference venue no later
than the evening of 18 June 2025. All participants are expected to attend the full duration of the conference,
and the registration fee covers dinner and accommodations for the night of 23 June. Airport shuttle
transportation is available to/from San Francisco International airport (SFO), which will be the most convenient
airport for most participants. The shuttle also serves Oakland International Airport. For details see: https://groometransportation.com/sonoma-county/
Map of SFO Airport Shuttles
Attendees may alternatively choose to provide their own transportation to Rohnert Park, CA (e.g., rental
vehicle or personal vehicle for local attendees), but will be expected to use conference-provided bus
transportation during the meeting (i.e., for field trips). Those who plan to provide their own
transportation to the Doubletree by Hilton Hotel Sonoma-Wine Country must indicate during registration that
they require parking at the venue.
In making travel plans, some participants may wish to consider spending an additional 1-2 days visiting
additional high-pressure localities of the Bay Area on their own. AGU's Streetcar 2 Subduction guide describes stops accessible by public transit (note that we
will be visiting Ring Mountain and Marin Headlands as part of our syn-conference field trips).
Presenter Information
Presentation format will be either oral or poster. Attendees will receive more details of their presentation
format, including information on preparing an oral or poster presentation, upon abstract acceptance in
mid-March.
International Attendees
Fill out and print out your
personalized Letter of Invitation. If you require additional information on your
invitation letter in order to obtain approval to travel or for your visa, please email us at penrose2025@geosociety.org.
Get your Letter of Invitation
Sponsors
Venue
Doubletree by Hilton Sonoma–Wine Country
One Doubletree Drive
Rohnert Park, CA 94928