Zobrazeno 1 - 10
of 122
pro vyhledávání: '"James D. Byerlee"'
Autor:
Murrell, S. A. F.
Publikováno v:
Geophysical Journal International; March 1980, Vol. 60 Issue: 3 p505-505, 1p
Publikováno v:
Journal of Geophysical Research: Solid Earth. 106:4327-4335
Self-potential (SP) anomalies observed above suspected magma reservoirs, dikes, etc., on various volcanoes (Kilauea, Hawaii; Mount Unzen, Japan; Piton de la Fournaise, Reunion Island, Miyake Jima, Japan) result from transient surface electric fields
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4be5057685c2307bed4831c95b1a7db4
https://doi.org/10.1029/2000jb900349
https://doi.org/10.1029/2000jb900349
Publikováno v:
Journal of Geophysical Research: Solid Earth. 103:9691-9712
We analyze friction data from two published suites of laboratory tests on granite in order to explore and quantify the effects of temperature (T) and pore water pressure (Pp) on the sliding behavior of faults. Rate-stepping sliding tests were perform
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e5fa3153b4f5a345f43011cc1219cd41
https://doi.org/10.1029/98jb00162
https://doi.org/10.1029/98jb00162
Publikováno v:
Journal of Geophysical Research: Solid Earth. 102:14787-14801
Serpentinite has been proposed as a cause of both low strength and aseismic creep of fault zones. To test these hypotheses, we have measured the strength of chrysotile-, lizardite-, and antigorite-rich serpentinite gouges under hydrothermal condition
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aacf145a496644d0e9ffb4a3a06c7b84
https://doi.org/10.1029/97jb00995
https://doi.org/10.1029/97jb00995
Publikováno v:
Journal of Geophysical Research: Solid Earth. 101:22215-22224
A model of a fault in the Earth is a sand-filled saw cut in a granite cylinder subjected to a triaxial test. The saw cut is inclined at an angle α to the cylinder axis, and the sand filling is intended to represent gouge. The triaxial test subjects
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::095ade3925659b0186ad5aa892444741
https://doi.org/10.1029/96jb02094
https://doi.org/10.1029/96jb02094
Publikováno v:
Geophysical Research Letters. 23:487-490
Mogi [1974] proposed a simple model of the incipient rupture surface to explain the Coulomb failure criterion. We show here that this model can plausibly be extended to explain the Mohr failure criterion. In Mogi's model the incipient rupture surface
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::15ea91343eeaf2cbbf504c55bb5d05f6
https://doi.org/10.1029/96gl00241
https://doi.org/10.1029/96gl00241
Publikováno v:
Journal of Geophysical Research: Solid Earth. 100:13045-13064
Sliding on faults in much of the continental crust likely occurs at hydrothermal conditions, i.e., at elevated temperature and elevated pressure of aqueous pore fluids, yet there have been few relevant laboratory studies. To measure the strength, sli
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6e0bf112f8e3172cdcbcc4947d8387b3
https://doi.org/10.1029/95jb00862
https://doi.org/10.1029/95jb00862
Autor:
James D. Byerlee, David A. Lockner
Publikováno v:
Pure and Applied Geophysics PAGEOPH. 145:717-745
It has been proposed that large strike-slip faults such as the San Andreas contain water in seal-bounded compartments. Arguments based on heat flow and stress orientation suggest that in most of the compartments, the water pressure is so high that th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::85fdd60a7d2fb45c2613cdf5bf28eec3
https://doi.org/10.1007/bf00879597
https://doi.org/10.1007/bf00879597
Autor:
James D. Byerlee, David A. Lockner
Publikováno v:
Geophysical Research Letters. 21:2353-2356
Laboratory studies have shown that consolidated fault gouge dilates in response to an increase in the rate of shearing. During the period of accelerating slip that characterizes the onset of an instability, or earthquake, on a fault containing consol
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3cd77a50c2dfc3d4a7ea86982607d277
https://doi.org/10.1029/94gl02366
https://doi.org/10.1029/94gl02366
Publikováno v:
Science. 265:1558-1561
The addition of hydrothermal fluids to heated, intact granite leads to permeability reductions in the temperature range of 300 degrees to 500 degrees C, with the rate of change generally increasing with increasing temperature. The addition of gouge e
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cdf3b9677699ad3e01f6427f7f6fde30
https://doi.org/10.1126/science.265.5178.1558
https://doi.org/10.1126/science.265.5178.1558