15 citations as recorded by crossref.

1. Potential of 3‐D vertical seismic profiles to characterize seismogenic fault zones R. von Huene et al. 10.1029/2008GC002013
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. 10.1016/j.tecto.2013.09.012
3. Length–displacement scaling and fault growth A. Gudmundsson et al. 10.1016/j.tecto.2013.06.012
4. Gutenberg-Richter relation originates from Coulomb stress fluctuations caused by elastic rock heterogeneity C. Langenbruch & S. Shapiro 10.1002/2013JB010282
5. Amorphous material in SAFOD core samples (San Andreas Fault): Evidence for crush‐origin pseudotachylytes? C. Janssen et al. 10.1029/2009GL040993
6. 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. 10.1016/j.epsl.2011.07.020
7. Faulting processes in active faults – Evidences from TCDP and SAFOD drill core samples C. Janssen et al. 10.1016/j.jsg.2014.04.004
8. 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. 10.1111/1755-6724.12207
9. Nanoscale porosity in SAFOD core samples (San Andreas Fault) C. Janssen et al. 10.1016/j.epsl.2010.10.040
10. 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. 10.1002/2014JB011489
11. Helium measurements of pore fluids obtained from the San Andreas Fault Observatory at Depth (SAFOD, USA) drill cores S. Ali et al. 10.1007/s10040-010-0645-6
12. Transform faults and transfer faults: Plate boundary and intra-continental tectonic dynamics transition Y. Dong et al. 10.1007/s11430-024-1536-7
13. Engineering Specifications on LTBMS Telemetry System for NanTroSEIZE 3.5 km Riser Hole Y. Namba et al. 10.5918/jamstecr.7.43
14. 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. 10.1111/j.1365-246X.2010.04612.x
15. Deep rock damage in the San Andreas Fault revealed by P- and S-type fault-zone-guided waves W. Ellsworth & P. Malin 10.1144/SP359.3