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Stress orientations and magnitudes in the SAFOD pilot hole
Author(s) -
Hickman Stephen,
Zoback Mark
Publication year - 2004
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2004gl020043
Subject(s) - geology , borehole , seismology , differential stress , stress field , stress (linguistics) , crust , ultimate tensile strength , fault (geology) , slip (aerodynamics) , drilling , geotechnical engineering , geophysics , deformation (meteorology) , materials science , finite element method , linguistics , oceanography , physics , philosophy , metallurgy , thermodynamics
Borehole breakouts and drilling‐induced tensile fractures in the 2.2‐km‐deep SAFOD pilot hole at Parkfield, CA, indicate significant local variations in the direction of the maximum horizontal compressive stress, S Hmax , but show a generalized increase in the angle between S Hmax and the San Andreas Fault with depth. This angle ranges from a minimum of 25 ± 10° at 1000–1150 m to a maximum of 69 ± 14° at 2050–2200 m. The simultaneous occurrence of tensile fractures and borehole breakouts indicates a transitional strike‐slip to reverse faulting stress regime with high horizontal differential stress, although there is considerable uncertainty in our estimates of horizontal stress magnitudes. If stress observations near the bottom of the pilot hole are representative of stresses acting at greater depth, then they are consistent with regional stress field indicators and an anomalously weak San Andreas Fault in an otherwise strong crust.