T54B:
Models and Experiments that Couple Flow and Deformation in the Shallow Crust II

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Session ID#: 16008

Session Description:
Coupled deformation and fluid flow underlie a wide range of fundamental behaviors and processes in the shallow crust, including rock and sediment strength; mass, heat and volatile fluxes; and the links between these fluxes and subsurface biological communities. Recent advances have the potential to illuminate these fundamental processes through the application and development of coupled models that describe deformation and fluid flow in response to the evolution of the full stress field, in combination with experimental studies that extend established soil mechanics concepts to geologically relevant higher stresses and longer time scales. Examples include pore pressure in subduction zones and sedimentary basins, slope failures, subglacial till deformation and hydrology, pressure and stress interaction around deep-well injection, stress and strain surrounding complex structures, and dynamic fault zone slip processes. We welcome experimental, theoretical, and field-based contributions describing deformation behavior and rheology, and theoretical approaches to illuminating earth behavior.
Primary Convener:  Peter B Flemings, The University of Texas at Austin, Institute for Geophysics and Department of Geological Sciences, Jackson School of Geosciences, Austin, United States
Conveners:  Susan M Ellis, GNS Science, Lower Hutt, New Zealand, Demian M Saffer, Penn State University, Department of Geosciences, University Park, PA, United States and Shemin Ge, University of Colorado, Boulder, United States
Chairs:  Susan M Ellis, GNS Science, Lower Hutt, New Zealand and Shemin Ge, University of Colorado, Boulder, United States
OSPA Liaison:  Demian M Saffer, Penn State University, Department of Geosciences, University Park, PA, United States

Cross-Listed:
  • C - Cryosphere
  • MR - Mineral and Rock Physics
  • NH - Natural Hazards
  • OS - Ocean Sciences
Index Terms:

3060 Subduction zone processes [MARINE GEOLOGY AND GEOPHYSICS]
5114 Permeability and porosity [PHYSICAL PROPERTIES OF ROCKS]
8159 Rheology: crust and lithosphere [TECTONOPHYSICS]
8164 Stresses: crust and lithosphere [TECTONOPHYSICS]

Abstracts Submitted to this Session:

Matthew Weingarten, Stanford Earth Sciences, Department of Geophysics, Stanford, CA, United States, Thomas Goebel, University of California Santa Cruz, Earth and Planetary Science Department, Santa Cruz, CA, United States, Xiaowei Chen, University of Oklahoma Norman Campus, School of Geosciences, Norman, OK, United States, Jackson Haffener, University of Oklahoma Norman Campus, School of Geology and Geophysics, Norman, OK, United States and Emily E Brodsky, University of California Santa Cruz, Department of Earth and Planetary Sciences, Santa Cruz, CA, United States
David Castineira, Massachusetts Institute of Technology, Civil and Environmental Engineering, Cambridge, MA, United States, Birendra Jha, University of Southern California, Mork Family Department of Chemical Engineering and Materials Science, Los Angeles, CA, United States and Ruben Juanes, Massachusetts Institute of Technology, Earth, Atmospheric and Planetary Sciences, Cambridge, MA, United States
Rachel M Lauer, University of Calgary, Calgary, AB, Canada, Demian M Saffer, Penn State University, Department of Geosciences, University Park, PA, United States and Robert N Harris, Oregon State University, College of Earth, Ocean, and Atmospheric Sciences, Corvallis, OR, United States
Pierre Henry1, Yves Guglielmi2, Amandine Morereau1, Simon Seguy1, Raymi Castilla3, Christophe Nussbaum4, Pierre Dick5, Jérémie Durand6, David Jaeggi4, Frederic Victor Donze7 and Alexandra Tsopela7, (1)Aix-Marseille Université, CNRS, IRD,, CEREGE UM34, Aix en Provence, France, (2)University of California Berkeley, Berkeley, United States, (3)TOTAL - Centre Scientifique et Technique Jean Feger, Pau, France, (4)Swisstopo, Wabern, Switzerland, (5)IRSN Institut de Radioprotection et de Sûreté Nucléaire, Fontenay-aux-Roses cedex, France, (6)SITES, Rueil-Malmaison, France, (7)Université Grenoble Alpes, 3SR Laboratory, Grenoble, France
Maria A Nikolinakou, The University of Texas at Austin; Bureau of Economic Geology, Jackson School of Geosciences, Austin, TX, United States, Mahdi Heidari, University of Texas at Austin, Austin, TX, United States, Peter B Flemings, The University of Texas at Austin, Institute for Geophysics and Department of Geological Sciences, Jackson School of Geosciences, Austin, United States and Michael R Hudec, Bureau of Economic Geology, Jackson School of Geosciences, The University of Texas at Austin, Austin, TX, United States
Sheng-Yuan Hsu1, Suvrat P Lele2, Nora Dedontney1, Jorge Garzon1, Kevin Searles1, Pablo F Sanz1 and Grant Gist1, (1)ExxonMobil Upstream Research Company, Houston, TX, United States, (2)ExxonMobil Upstream Research Company, Spring, TX, United States
Renuhaa Asaithambi, University of Southern California, Los Angeles, CA, United States, Birendra Jha, University of Southern California, Mork Family Department of Chemical Engineering and Materials Science, Los Angeles, CA, United States and Eunseo Choi, PhD, University of Memphis, Center for Earthquake Research and Information (CERI), Memphis, TN, United States
Baiyuan Gao1, Peter B Flemings1, Demian M Saffer2, Maria A Nikolinakou3 and Mahdi Heidari3, (1)The University of Texas at Austin, The Department of Geological Sciences, Austin, TX, United States, (2)Penn State University, Department of Geosciences, University Park, PA, United States, (3)The University of Texas at Austin, Bureau of Economic Geology, Austin, TX, United States

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