Chemical controls on fault behavior: Weakening of serpentinite sheared against quartz-bearing rocks and its significance for fault creep in the San Andreas system

Weakening of the slab–mantle wedge interface induced by metasomatic growth of talc

(2012) Ken-ichi Hirauchi et al.   GEOLOGY

Lithology and internal structure of the San Andreas fault at depth based on characterization of Phase 3 whole-rock core in the San Andreas Fault Observatory at Depth (SAFOD) borehole

(2011) Kelly K. Bradbury et al.   EARTH AND PLANETARY SCIENCE LETTERS

Geologic versus geodetic deformation adjacent to the San Andreas fault, central California

(2011) S. J. Titus et al.   GEOLOGICAL SOCIETY OF AMERICA BULLETIN

Low strength of deep San Andreas fault gouge from SAFOD core

(2011) David A. Lockner et al.   NATURE

Deformation of antigorite serpentinite at high temperature and pressure

(2010) Linda J. Chernak et al.   EARTH AND PLANETARY SCIENCE LETTERS

Effect of clay content and mineralogy on frictional sliding behavior of simulated gouges: Binary and ternary mixtures of quartz, illite, and montmorillonite

(2010) Sheryl Tembe et al.   JOURNAL OF GEOPHYSICAL RESEARCH

Natural deformation related to serpentinisation of an ultramafic inclusion within a continental shear zone: The key role of fluids

(2008) Jean-Philippe Bellot   TECTONOPHYSICS

Talc friction in the temperature range 25°–400 °C: Relevance for Fault-Zone Weakening

(2007) Diane E. Moore et al.   TECTONOPHYSICS