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GSA 2017 ANNUAL MEETING & EXPOSITION

        T225. New Perspectives on Cordilleran Tectonics,                    T229. Paleocene-Eocene Tectonic and Magmatic
        Paleogeography, and Metallogeny                                     Evolution of the Pacific Northwest

Cosponsors: GSA Sedimentary Geology Division; SEPM (Society         Cosponsors: GSA Structural Geology and Tectonics Division;
for Sedimentary Geology); Society of Economic Geologists;           GSA Sedimentary Geology Division; GSA Mineralogy,
GSA Structural Geology and Tectonics Division                       Geochemistry, Petrology, and Volcanology Division

Disciplines: Tectonics/Tectonophysics, Stratigraphy, Economic       Disciplines: Tectonics/Tectonophysics, Petrology, Igneous,
Geology                                                             Geophysics/Geodynamics

Advocates: Luke P. Beranek; Justin V. Strauss; Stephen J. Piercey   Advocates: Jeffrey H. Tepper; Eugene D. Humphreys;
                                                                    Robert B. Miller
  This session welcomes new ideas on Cordilleran evolution that
use the Neoproterozoic-Cenozoic rock record from Alaska to            Paleogene magmatism, extension, basin subsidence, and fault-
Mexico. Contributions for multidisciplinary studies in stratigra-   ing spanned the Pacific Northwest, perhaps related to ridge sub-
phy, petrology, structural geology, geochemistry, and geochronol-   duction, slab breakoff, and/or Siletzia accretion. We seek contri-
ogy are particularly welcome.                                       butions on this “Challis episode” from structure, tectonics,
                                                                    petrology, sedimentation, and geophysics.
T226. New Perspectives on Processes of Subduction Initiation
and Termination                                                     T230. Polygenetic Mélanges: A Glimpse on Tectono-
                                                                    Sedimentary Recycling in Convergent Margins
Cosponsors: GSA Structural Geology and Tectonics Division;
GSA Mineralogy, Geochemistry, Petrology, and Volcanology            Cosponsors: GSA International/International Interdisciplinary
Division; GSA Geophysics Division                                   Interest Group; IGCP 640 program S4SLIDE (Significance of
                                                                    Modern and Ancient Submarine Slope Landslides); GSA
Disciplines: Tectonics/Tectonophysics, Petrology, Igneous,          Structural Geology and Tectonics Division; GSA Sedimentary
Geophysics/Geodynamics                                              Geology Division

Advocates: Sarah Roeske; Nancy Riggs; Susanne Buiter; Douwe         Disciplines: Tectonics/Tectonophysics, Sediments, Clastic,
van Hinsenberg                                                      Structural Geology

  This session examines the formation and termination of sub-       Advocates: Andrea Festa; Kei Ogata; Gian Andrea Pini
duction zones, whether due to passage of a triple junction, change
in plate motion, or collision. Ancient and modern records and         This session addresses the definition of structures, fabric, and
modeling studies of these processes are welcome.                    texture diagnostic of sedimentary mélanges overprinted by other
                                                                    processes and the estimation of their occurrence in fossil, exhumed,
T227. Ophiolite and Ocean Plate Stratigraphy Records in             and present-day accretionary wedges and collisional chains.
Modern and Ancient Accretionary and Collisional Orogenic
Belts in the Circum-Pacific Region                                  T231. Subduction Top to Bottom 2 (ST2B-2), Cascadia
                                                                    and Beyond
Cosponsors: GSA Structural Geology and Tectonics Division;
GSA Mineralogy, Geochemistry, Petrology, and Volcanology            Cosponsors: GSA Structural Geology and Tectonics Division;
Division; GSA Geophysics Division; Geological Society of China;     Future of Tectonics Initiative
GSA Sedimentary Geology Division
                                                                    Disciplines: Tectonics/Tectonophysics, Geophysics/
Disciplines: Tectonics/Tectonophysics, Petrology, Igneous,          Geodynamics, Volcanology
Geophysics/Geodynamics
                                                                    Advocates: Gray E. Bebout; David W. Scholl; Robert Stern;
Advocates: Yildirim Dilek; Jingsui Yang                             Anne Trehu; Joan Gomberg; Thomas W. Sisson

  We encourage original contributions on the origins and              Subduction zone processes and their products, including the
emplacement mechanisms of ophiolites and remnants of ocean          associated natural hazards, are important to science and influence
plate stratigraphy in the accretionary and collisional orogenic     society. This session assesses geological, geophysical, geochemi-
belts in the Circum-Pacific region.                                 cal, and theoretical advancements and promising directions for
                                                                    future research, emphasizing Cascadia.
        T228. Origin, Accretion, and Translation of
        Mesozoic-Cenozoic Terranes along the Pacific Margin         T232. Subduction Zone Response to Ridge and Plateau
        of North America                                            Collision: Perspectives from the Archean to the Cenozoic

Cosponsor: GSA Structural Geology and Tectonics Division            Cosponsor: GSA Structural Geology and Tectonics Division

Discipline: Tectonics/Tectonophysics                                Discipline: Tectonics/Tectonophysics

Advocates: David T. Katopody; Mark T. Brandon; Bernard Housen       Advocates: Michael P. Eddy; Paul J. Umhoefer

  The Pacific margin of North America is the center of a long-        Ridge-trench interaction and oceanic plateau accretion have
standing controversy about terrane mobility along continental       profound effects on the geology of convergent margins. We wel-
margins. This session will serve as a forum to identify remaining   come submissions that document these effects throughout Earth’s
problems and opportunities in Cordilleran tectonics.                history using field, geophysical, and/or modeling data.

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