16 citations as recorded by crossref.

1. Potential of 3‐D vertical seismic profiles to characterize seismogenic fault zones R. von Huene et al.
2. Pressure dependence of density, porosity, compressional wave velocity of fault rocks from the ruptures of the 2008 Wenchuan earthquake, China X. Yang et al.
3. Length–displacement scaling and fault growth A. Gudmundsson et al.
4. Progress and challenges in studies of earthquake rupture initiation and arrest S. Ni et al.
5. Gutenberg-Richter relation originates from Coulomb stress fluctuations caused by elastic rock heterogeneity C. Langenbruch & S. Shapiro
6. Amorphous material in SAFOD core samples (San Andreas Fault): Evidence for crush‐origin pseudotachylytes? C. Janssen et al.
7. 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 K. Bradbury et al.
8. Faulting processes in active faults – Evidences from TCDP and SAFOD drill core samples C. Janssen et al.
9. Rock Damage Structure of the South Longmen‐Shan Fault in the 2008 M8 Wenchuan Earthquake Viewed with Fault‐Zone Trapped Waves and Scientific Drilling Y. LI et al.
10. Nanoscale porosity in SAFOD core samples (San Andreas Fault) C. Janssen et al.
11. Rock and mineral transformations in a fault zone leading to permanent creep: Interactions between brittle and viscous mechanisms in the San Andreas Fault J. Richard et al.
12. Helium measurements of pore fluids obtained from the San Andreas Fault Observatory at Depth (SAFOD, USA) drill cores S. Ali et al.
13. Transform faults and transfer faults: Plate boundary and intra-continental tectonic dynamics transition Y. Dong et al.
14. Engineering Specifications on LTBMS Telemetry System for NanTroSEIZE 3.5 km Riser Hole Y. Namba et al.
15. Fault zone structure at depth from differential dispersion of seismic guided waves: evidence for a deep waveguide on the San Andreas Fault J. Wu et al.
16. Deep rock damage in the San Andreas Fault revealed by P- and S-type fault-zone-guided waves W. Ellsworth & P. Malin