Mineralogical compositions of fault rocks from surface ruptures of Wenchuan earthquake and implication of mineral transformation during the seismic cycle along Yingxiu-Beichuan fault, Sichuan Province, China

[1]  Jianye Chen,et al.  Fluid-rock interactions in seismic faults : implications from the structures and mineralogical and geochemical compositions of drilling cores from the rupture of the 2008 Wenchuan earthquake, China , 2016 .

[2]  E. Torgersen,et al.  Structural and temporal evolution of a reactivated brittle–ductile fault – Part I: Fault architecture, strain localization mechanisms and deformation history , 2014 .

[3]  D. Moore.  Comparative mineral chemistry and textures of SAFOD fault gouge and damage-zone rocks , 2014 .

[4]  Sheng‐Rong Song,et al.  Clay mineral anomalies in the Yingxiu–Beichuan fault zone from the WFSD-1 drilling core and its implication for the faulting mechanism during the 2008 Wenchuan earthquake (Mw 7.9) , 2014 .

[5]  Zhiqing Xu,et al.  Structural and physical property characterization in the Wenchuan earthquake Fault Scientific Drilling project — hole 1 (WFSD-1) , 2014 .

[6]  Jianye Chen,et al.  Frictional and transport properties of the 2008 Wenchuan Earthquake fault zone: Implications for coseismic slip-weakening mechanisms , 2013 .

[7]  T. Shimamoto,et al.  Rapid postseismic strength recovery of Pingxi fault gouge from the Longmenshan fault system: Experiments and implications for the mechanisms of high‐velocity weakening of faults , 2013 .

[8]  Xiaosong Yang,et al.  Importance of thermochemical pressurization in the dynamic weakening of the Longmenshan Fault during the 2008 Wenchuan earthquake: Inferences from experiments and modeling , 2013 .

[9]  T. Shimamoto,et al.  Structures and high-velocity frictional properties of the Pingxi fault zone in the Longmenshan fault system, Sichuan, China, activated during the 2008 Wenchuan earthquake , 2013 .

[10]  Lei Zhang,et al.  Frictional properties of natural gouges from Longmenshan fault zone ruptured during the Wenchuan Mw7.9 earthquake , 2013 .

[11]  Jianye Chen,et al.  Mass removal and clay mineral dehydration/rehydration in carbonate‐rich surface exposures of the 2008 Wenchuan Earthquake fault: Geochemical evidence and implications for fault zone evolution and coseismic slip , 2013 .

[12]  Zhiqing Xu,et al.  Characteristics of the fault-related rocks, fault zones and the principal slip zone in the Wenchuan Earthquake Fault Scientific Drilling Project Hole-1 (WFSD-1) , 2013 .

[13]  Jianye Chen,et al.  Internal structures and high-velocity frictional properties of a bedding-parallel carbonate fault at Xiaojiaqiao outcrop activated by the 2008 Wenchuan earthquake , 2012 .

[14]  Jianye Chen,et al.  Magnetic properties of fault rocks from the Yingxiu–Beichuan fault: Constraints on temperature rise within the shallow slip zone during the 2008 Wenchuan earthquake and their implications , 2012 .

[15]  F. Chester,et al.  Progressive illitization in fault gouge caused by seismic slip propagation along a megasplay fault in the Nankai Trough , 2011 .

[16]  T. Shimamoto,et al.  High-velocity frictional behavior of Longmenshan fault gouge from Hongkou outcrop and its implications for dynamic weakening of fault during the 2008 Wenchuan earthquake , 2011 .

[17]  Honglin He,et al.  Internal structure of Longmenshan fault zone at Hongkou outcrop, Sichuan, China, that caused the 2008 Wenchuan earthquake , 2011 .

[18]  S. Hickman,et al.  Low strength of deep San Andreas fault gouge from SAFOD core , 2011, Nature.

[19]  Xi-wei Xu,et al.  Paleoseismic evidence and repeat time of large earthquakes at three sites along the Longmenshan fault zone , 2010 .

[20]  C. Spiers,et al.  Frictional Properties of Sedimentary Rocks and Natural Fault Gouge from the Longmen Shan Fault Zone, Sichuan, China , 2010 .

[21]  Peizhen Zhang,et al.  Oblique, High-Angle, Listric-Reverse Faulting and Associated Development of Strain: The Wenchuan Earthquake of May 12, 2008, Sichuan, China , 2010 .

[22]  T. Wong,et al.  Effect of clay content and mineralogy on frictional sliding behavior of simulated gouges: Binary and ternary mixtures of quartz, illite, and montmorillonite , 2010 .

[23]  K. Hudnut,et al.  Co-seismic ruptures of the 12 May 2008, Ms 8.0 Wenchuan earthquake, Sichuan: East–west crustal shortening on oblique, parallel thrusts along the eastern edge of Tibet , 2009 .

[24]  H. Chen,et al.  Clay mineral anomalies in the fault zone of the Chelungpu Fault, Taiwan, and their implications , 2009 .

[25]  Dong Jia,et al.  Co-seismic thrusting rupture and slip distribution produced by the 2008 Mw 7.9 Wenchuan earthquake, China , 2009 .

[26]  Yann Klinger,et al.  Coseismic reverse- and oblique-slip surface faulting generated by the 2008 Mw 7.9 Wenchuan earthquake, China , 2009 .

[27]  S. Ji,et al.  Uplift of the Longmen Shan Range and the Wenchuan Earthquake , 2008 .

[28]  W. Burnett,et al.  Radon and radium isotope assessment of submarine groundwater discharge in the Yellow River delta, China , 2008 .

[29]  D. Faulkner,et al.  Strength, porosity, and permeability development during hydrostatic and shear loading of synthetic quartz-clay fault gouge , 2008 .

[30]  K. Ujiie,et al.  Characteristics and implication of clay minerals in the northern and southern parts of the Chelung-pu fault, Taiwan , 2007 .

[31]  C. Wang,et al.  Fluid infiltration associated with seismic faulting: Examining chemical and mineralogical compositions of fault rocks from the active Chelungpu fault , 2007 .

[32]  K. Masuda,et al.  Effects of clay content on the frictional strength and fluid transport property of faults , 2007 .

[33]  C. Marone,et al.  Effect of hydration state on the frictional properties of montmorillonite-based fault gouge , 2007 .

[34]  James P. Evans,et al.  Structural, Mineralogical, and Geochemical Characterization of the Chelungpu Thrust Fault, Taiwan , 2007 .

[35]  L. Warr,et al.  Influence of phyllosilicate mineral assemblages, fabrics, and fluids on the behavior of the Punchbowl fault, southern California , 2003 .

[36]  D. Humphrey.  Strength and Deformation , 2002 .

[37]  D. Faulkner,et al.  Can the maintenance of overpressured fluids in large strike-slip fault zones explain their apparent weakness? , 2001 .

[38]  C. Choo,et al.  Characteristics of Clay Minerals in Gouges of the Dongrae Fault, Southeastern Korea, and Implications for Fault Activity , 2000 .

[39]  A. Mullis.  DETERMINATION OF THE RATE-LIMITING MECHANISM FOR QUARTZ PRESSURE DISSOLUTION , 1993 .

[40]  J. Longo,et al.  An Experimentally Derived Kinetic Model for Smectite-to-Illite Conversion and Its Use as a Geothermometer , 1993 .

[41]  James P. Evans,et al.  Internal structure and weakening mechanisms of the San Andreas Fault , 1993 .

[42]  F. Elsass,et al.  Chemistry of illite-smectite inferred from TEM measurements of fundamental particles , 1992, Clay Minerals.

[43]  J. Banfield,et al.  Analytical Transmission Electron Microscope Studies of Plagioclase, Muscovite, and K-Feldspar Weathering , 1990 .

[44]  G. Riedmüller,et al.  Statistical Analysis of Clay Mineral Assemblages in Fault Gouges , 1988 .

[45]  N. Kohyama,et al.  Chemical and Morphological Evidence for the Conversion of Smectite to Illite , 1987 .

[46]  J. M. Tait,et al.  The conversion of smectite to illite during diagenesis: evidence from some illitic clays from bentonites and sandstones , 1985, Mineralogical Magazine.

[47]  R. M. Pollastro.  Mineralogical and Morphological Evidence for the Formation of Illite at the Expense of Illite/Smectite , 1985 .

[48]  L. Hossner,et al.  Transformation of Chlorite to Smectite Through Regularly Interstratified Intermediates 1 , 1981 .

[49]  G. Riedmüller.  Neoformations and transformations of clay minerals in tectonic shear zones , 1978 .

[50]  Camden R. Hubbard,et al.  The reference intensity ratio, I/Ic, for computer simulated powder patterns , 1976 .

[51]  A. Niemeijer,et al.  The crucial role of temperature in high-velocity weakening of faults : Experiments on gouge using host blocks with different thermal conductivities , 2016 .

[52]  Zhou Yongsheng.  THE STRENGTH AND DEFORMATION MECHANISMS OF BRITTLE-PLASTIC TRANSITION ZONE,AND THE EFFECTS OF STRAIN RATE AND FLUIDS , 2012 .

[53]  Chen Jianye,et al.  Internal structure and permeability of Wenchuan earthquake fault , 2011 .

[54]  Donna L. Whitney,et al.  Abbreviations for names of rock-forming minerals , 2010 .

[55]  G. Wang,et al.  Preliminary study of coseismic fault gouge occurred in the slip zone of the Wenchuan Ms 8.0 earthquake and its tectonic implications , 2008 .

[56]  R. Pusch,et al.  Physico/chemical stability of smectite clays , 1996 .

[57]  J. Hower,et al.  Clay Mineral Assemblages as Low Grade Metamorphic Geothermometers: Application to the Thrust Faulted Disturbed Belt Of Montana, U.S.A , 1979 .