MR33C
The Spectrum of Slip Behaviors of Continental and Subduction Fault Zones II Posters

Wednesday, 16 December 2015: 13:40-18:00
Poster Hall (Moscone South)
Primary Conveners:  Nicola De Paola, University of Durham, Durham, United Kingdom
Conveners:  Cristiano Collettini, Sapienza University of Rome, Rome, Italy, Andre R Niemeijer, Utrecht University, Utrecht, Netherlands and Wenlu Zhu, University of Maryland College Park, College Park, MD, United States
Chairs:  Nicola De Paola, University of Durham, Durham, United Kingdom, Cristiano Collettini, Sapienza University of Rome, Rome, Italy and Andre R Niemeijer, Utrecht University, Department of Earth Sciences, Utrecht, Netherlands
OSPA Liaisons:  Andre R Niemeijer, Utrecht University, Department of Earth Sciences, Utrecht, Netherlands
 
Shear heating and solid state diffusion: Constraints from clumped isotope thermometry in carbonate faults (63160)
Shalev Siman-Tov1,2, Hagit P Affek3, Alan Matthews1, Einat Aharonov1 and Zeev Reches4, (1)Hebrew University of Jerusalem, Jerusalem, Israel, (2)University of California Santa Cruz, Earth and Planetary Sciences, Santa Cruz, CA, United States, (3)Yale University, New Haven, CT, United States, (4)University of Oklahoma Norman Campus, Norman, OK, United States
 
Amorphization and Frictional Processes in Smectite-Quartz Gouge Mixtures Sheared from Sub-seismic to Seismic Slip Rates (63740)
Stefano Aretusini1, Silvia Mittempergher2, Elena Spagnuolo3, Giulio Di Toro4 and Alessandro Gualtieri2, (1)University of Padova, Padova, Italy, (2)University of Modena and Reggio Emilia, Modena, Italy, (3)National Institute of Geophysics and Volcanology, Roma 1, Rome, Italy, (4)University of Padua, Padua, Italy
 
Deformation and chemical reaction in an ultramafic terrane boundary: the Livingstone Fault, New Zealand (64152)
Jordan Alexander Crase and Steven A.F. Smith, University of Otago, Dunedin, New Zealand
 
The implication of gouge mineralogy evolution on fault creep: an example from The North Anatolian Fault, Turkey (64606)
Maor Kaduri1, Jean-Pierre Gratier2, Francois Renard3, Ziyadin Cakir4 and Cecile Lasserre1, (1)Université Grenoble Alpes, ISTerre, Grenoble, France, (2)ISTerre Institute of Earth Sciences, Saint Martin d'Hères, France, (3)University Joseph Fourier Grenoble, Grenboble, France, (4)Istanbul Technical Univ, Geology, Istanbul, Turkey
 
Frictional controls on high-angle reverse faulting during compressional basin inversion (65577)
Simon Alder1, Steven A.F. Smith1, Telemaco Tesei2 and Cristiano Collettini3, (1)University of Otago, Dunedin, New Zealand, (2)University of Perugia, Perugia, Italy, (3)Sapienza University of Rome, Rome, Italy
 
Laboratory Evidence of Strength Recovery of Healed Faults (65622)
Koji Masuda, Geological Survey of Japan, Tsukuba, Japan
 
Dynamically triggered slip and sustained fault gouge instability associated with unique slip behavior under laboratory shear conditions (67341)
Paul A Johnson, Los Alamos National Laboratory, Earth and Environmental Sciences, Los Alamos, NM, United States
 
The Effect of Micrite and Micro-porous Skeletal Grains on the NMR Response of Carbonate Rocks (62122)
Ammar El Husseiny, Stanford University, Stanford, CA, United States
 
In-situ stress and strength in the Nankai inner accretionary prism at Site C0002, IODP NanTroSEIZE (68821)
Hiroko Kitajima, Texas A & M University College Station, College Station, TX, United States
 
The Role of Fluid Pressure in Earthquake Triggering: Insights from an Experimental Study of Frictional Stability of Carbonates (69021)
Cristiano Collettini and Marco Scuderi, Sapienza University of Rome, Rome, Italy
 
Preferential earthquake-nucleating locations on faults determined by heterogeneous direct- and evolution-effect parameters of rate- and state-dependent friction (69944)
Sohom Ray and Robert C Viesca, Tufts University, Civil and Environmental Engineering, Medford, MA, United States
 
Loading Rate-Dependent Elastoviscoplasticity in San Andreas Fault Observatory at Depth (SAFOD) Fault Gouge: Implications for Repeating Earthquakes and Fault Zone-Guided Waves (70340)
Arjun H Kohli, Stanford University, Stanford, CA, United States and David A Lockner, USGS, Menlo Park, CA, United States
 
Micromechanical processes of frictional aging and the affect of shear stress on fault healing: insights from material characterization and ultrasonic velocity measurements (70538)
Kerry L Ryan, Pennsylvania State University Main Campus, University Park, PA, United States
 
Flow properties through a single fracture in Neogene-Quaternary siltstone on effective pressure increasing and decreasing processes (71826)
Shin-ichi Uehara, Toho University, Chiba, Japan and Mami Noguchi, The University of Tokyo, Graduate School of Frontier Sciences, Kashiwa, Chiba, Japan
 
Frictional Properties of Phyllosilicate-rich Mylonite and Conditions for the Brittle-Ductile Transition (72448)
Lei Zhang, Institute of Geology, China Earthquake Administration, Beijing, China
 
How Orogen-scale Exhumed Strike-slip Faults Initiate (72917)
Shuyun Cao, China University of Geosciences Wuhan, State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences, Wuhan, China; University of Salzburg, Dept. Geography and Geology, Salzburg, Austria
 
Fault rupture as a series of nano-seismic events during high-velocity shear experiments (73085)
Ximeng Zu1, Zeev Reches1, Xiaowei Chen2 and Jefferson C Chang3, (1)University of Oklahoma Norman Campus, Norman, OK, United States, (2)University of Oklahoma Norman Campus, School of Geology and Geophysics, Norman, OK, United States, (3)Oklahoma Geological Survey, Leonard, OK, United States
 
Frictional melting experiments investigate coseismic behaviour of pseudotachylyte-bearing faults in the Outer Hebrides Fault Zone, UK. (73337)
Lucy Campbell1, Nicola De Paola2, Stefan Bjorklund Nielsen2, Robert Holdsworth2, Geoffrey E Lloyd1, Richard J Phillips1 and Rachel Walcott3, (1)University of Leeds, Institute of Geophysics and Tectonics, Leeds, United Kingdom, (2)University of Durham, Durham, United Kingdom, (3)National Museums Scotland, Edinburgh, United Kingdom
 
Dilatancy and pore pressure effects during fracture and shear of antigorite-rich serpentinite (75383)
Melodie E French and Wenlu Zhu, University of Maryland College Park, College Park, MD, United States
 
Is frictional healing slip-dependent? (77181)
Pathikrit Bhattacharya1, Allan M Rubin1, Kerry L Ryan2, Jacques Vincent Riviere3 and Chris Marone2, (1)Princeton University, Princeton, NJ, United States, (2)Pennsylvania State University Main Campus, University Park, PA, United States, (3)Los Alamos National Laboratory, Earth and Environmental Sciences, Los Alamos, NM, United States
 
Experimental study on propagation of fault slip along a simulated rock fault (78262)
Kazuo Mizoguchi, Central Research Institute of Electic Power Industry, Tokyo, Japan
 
The Energetic Assessment of Frictional Instability Based on Rowe’s Theory (79119)
Momoko Hirata, Jun Muto and Hiroyuki Nagahama, Tohoku University, Sendai, Japan
 
The frictional properties and deformation mechanisms of faults in near-surface, poorly lithified sediments: implications for rupture propagation in the shallow crust (79480)
Rachael J Bullock1, Nicola De Paola2, Robert Holdsworth2 and Shmuel Marco3, (1)University of Durham, Durham, DH1, United Kingdom, (2)University of Durham, Durham, United Kingdom, (3)Tel Aviv University, Tel Aviv, Israel
 
Multi-surface Earthquake Rupture Recorded in Pseudotachylyte Vein Geometries, Norumbega Shear Zone, southern Maine (81089)
Catherine Ross1, Christie D Rowe2, Stephen G Pollock3, Mark Swanson3, Matthew Tarling1, Nils Rainer Backeberg1, Sophie Coulson4, Naomi Barshi2, Charlotte Bate5, Kelian Dascher-Cousineau1, Jacek Scibek5, Nicolas Harrichhausen1, Alexander Timofeev6, Paul Rakoczy1, Haylea Nisbet1, Andres Castro1 and Hendrik Smith1, (1)McGill University, Department of Earth and Planetary Sciences, Montreal, QC, Canada, (2)McGill University, Dept of Earth and Planetary Sciences, Montreal, QC, Canada, (3)University of Southern Maine, Gorham, ME, United States, (4)University of Liverpool, Liverpool, United Kingdom, (5)McGill University, Montreal, QC, Canada, (6)McGill University, Earth and Planetary Sciences, Montreal, QC, Canada
 
Static versus dynamic fracturing in shallow carbonate fault zones (81186)
Michele Fondriest1, Mai-Linh Doan2, Frans M. Aben2, Florian Fusseis3, Tom M Mitchell4 and Giulio Di Toro5, (1)University of Padova, Padova, Italy, (2)University Joseph Fourier Grenoble, ISTerre, Grenboble, France, (3)University of Edinburgh, Edinburgh, United Kingdom, (4)University College London, Rock and Ice Physics and Seismological Laboratory, London, United Kingdom, (5)University of Padua, Padua, Italy
 
Earthquake lubrication and healing explained by amorphous nanosilica (81226)
Christie D Rowe1, Kelsey Gail Lamothe2, Marieke Rempe3, Mark Andrews2, Thomas M Mitchell4, Giulio Di Toro5 and Joseph Clancy White6, (1)McGill University, Dept of Earth and Planetary Sciences, Montreal, QC, Canada, (2)McGill University, Montreal, QC, Canada, (3)Ruhr-Universität Bochum, Bochum, Germany, (4)University College London, London, United Kingdom, (5)University of Padua, Padua, Italy, (6)University of New Brunswick, Fredericton, NB, Canada
 
Relationship between amorphous silica and precious metal in quartz veins (86182)
Nicolas Harrichhausen1, Christie D Rowe2, Warwick S Board3 and Charles James Greig3, (1)McGill University, Earth and Planetary Sciences, Montreal, QC, Canada, (2)McGill University, Dept of Earth and Planetary Sciences, Montreal, QC, Canada, (3)Pretivm Resources Inc, Geology, Vancouver, BC, Canada
 
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