Weakness of the San Andreas Fault revealed by samples from the active fault zone
暂无分享,去创建一个
[1] C. Marone,et al. Frictional behavior of materials in the 3D SAFOD volume , 2009 .
[2] T. Wong,et al. Frictional strength of cuttings and core from SAFOD drillhole phases 1 and 2 , 2006 .
[3] W. Evans,et al. Chemical and Isotopic Composition of Water and Gases From the SAFOD Wells: Implications to the Dynamics of the San Andreas Fault at Parkfield, California , 2005 .
[4] D. Faulkner,et al. Can the maintenance of overpressured fluids in large strike-slip fault zones explain their apparent weakness? , 2001 .
[5] C. Spiers,et al. Fault rocks from the SAFOD core samples : implications for weakening at shallow depths along the San Andreas Fault, California , 2011 .
[6] T. Wong,et al. Constraints on the stress state of the San Andreas Fault with analysis based on core and cuttings from San Andreas Fault Observatory at Depth (SAFOD) drilling phases 1 and 2: STRESS STATE CONSTRAINTS ON THE SAF , 2009 .
[7] C. Collettini,et al. Fault zone fabric and fault weakness , 2009, Nature.
[8] C. Morrow,et al. Fault Mechanics And Transport Properties Of Rocks , 2002 .
[9] D. Elsworth,et al. Fabric induced weakness of tectonic faults , 2010 .
[10] L. Warr,et al. Origin and significance of clay‐coated fractures in mudrock fragments of the SAFOD borehole (Parkfield, California) , 2006 .
[11] C. Marone. LABORATORY-DERIVED FRICTION LAWS AND THEIR APPLICATION TO SEISMIC FAULTING , 1998 .
[12] L. Warr,et al. Nanocoatings of clay and creep of the San Andreas fault at Parkfield, California , 2010 .
[13] P. Fulton,et al. Potential role of mantle‐derived fluids in weakening the San Andreas Fault , 2009 .
[14] Ben A. van der Pluijm,et al. Mineralogical characterization of protolith and fault rocks from the SAFOD Main Hole , 2006 .
[15] D. Lockner,et al. Using drill cutting separates to estimate the strength of narrow shear zones at SAFOD , 2006 .
[16] M. Zoback,et al. New Evidence on the State of Stress of the San Andreas Fault System , 1987, Science.
[17] James P. Evans,et al. Internal structure and weakening mechanisms of the San Andreas Fault , 1993 .
[18] Michael J. Rymer,et al. Talc-bearing serpentinite and the creeping section of the San Andreas fault , 2007, Nature.
[19] L. Warr,et al. Constraints on mineralization, fluid-rock interaction, and mass transfer during faulting at 2―3 km depth from the SAFOD drill hole , 2009 .
[20] C. Spiers,et al. Effect of phyllosilicates on fluid-assisted healing of gouge-bearing faults , 2000 .
[21] W. Ellsworth,et al. Scientific Drilling Into the San Andreas Fault Zone , 2010 .
[22] C. Marone,et al. Comparison of smectite- and illite-rich gouge frictional properties: application to the updip limit of the seismogenic zone along subduction megathrusts , 2003 .
[23] Robert M. Nadeau,et al. Nonvolcanic Tremor Evolution and the San Simeon and Parkfield, California, Earthquakes , 2009, Science.
[24] J. Brune,et al. Heat Flow, Stress, and Rate of Slip along the San Andreas Fault, , 1969 .
[25] A. Lachenbruch,et al. Corrections to ‘Heat flow and energetics of the San Andreas Fault Zone’ and some additional comments on the relation between fault friction and observed heat flow , 1981 .
[26] Christopher H. Scholz,et al. Evidence for a strong San Andreas fault , 2000 .