Access the full text.
Sign up today, get DeepDyve free for 14 days.
R. Kerrich, R. Beckinsale, J. Durham (1977)
The transition between deformation regimes dominated by intercrystalline diffusion and intracrystalline creep evaluated by oxygen isotope thermometryTectonophysics, 38
A. Lachenbruch (1980)
Frictional heating, fluid pressure, and the resistance to fault motionJournal of Geophysical Research, 85
J. Blacic, J. Christie (1984)
Plasticity and hydrolytic weakening of quartz single crystalsJournal of Geophysical Research, 89
R. Maddock (1983)
Melt origin of fault-generated pseudotachylytes demonstrated by texturesGeology, 11
A. Lachenbruch, J. Sass (1980)
Heat flow and energetic of the San Andreas fault zoneJournal of Geophysical Research
Phillips Claire (1982)
Character and origin of cataclasite developed along the low-angle Whipple detachment fault, Whipple Mountains, California
C. Simpson (1983)
Displacement and strain patterns from naturally occurring shear zone terminationsJournal of Structural Geology, 5
J. Rice (1983)
Constitutive relations for fault slip and earthquake instabilitiespure and applied geophysics, 121
C. Passchier (1982)
Pseudotachylyte and the development of ultramylonite bands in the Saint-Barthelemy Massif, French PyreneesJournal of Structural Geology, 4
P. Segall, D. Pollard (1983)
Nucleation and growth of strike slip faults in graniteJournal of Geophysical Research, 88
J. Grocott (1981)
Fracture geometry of pseudotachylyte generation zones: a study of shear fractures formed during seismic eventsJournal of Structural Geology, 3
M. Watts, G. Williams (1979)
Fault rocks as indicators of progressive shear deformation in the Guingamp region, BrittanyJournal of Structural Geology, 1
J. Byerlee (1978)
Friction of rockspure and applied geophysics, 116
E. Bombolakis, J. Hepburn, D. Roy (1978)
Fault creep and stress drops in saturated silt‐clay gougeJournal of Geophysical Research, 83
W. Bakun, R. Stewart, C. Bufe, S. Marks (1980)
Implication of seismicity for failure of a section of the San Andreas FaultBulletin of the Seismological Society of America, 70
P. Jégouzo (1980)
The South Armorican Shear ZoneJournal of Structural Geology, 2
S. Hanmer (1982)
Microstructure and geochemistry of plagioclase and microcline in naturally deformed graniteJournal of Structural Geology, 4
Robert Smith, R. Bruhn (1984)
INTRAPLATE EXTENSIONAL TECTONICS OF THE EASTERN BASIN-RANGE: INFERENCES ON STRUCTURAL STYLE FROM SEISMIC REFLECTION DATA, REGIONAL TECTONICS, AND THERMAL-MECHANICAL MODELS OF BRITTLE-DUCTILE DEFORMATION.Journal of Geophysical Research, 89
G. Mitra (1979)
Ductile deformation zones in Blue Ridge basement rocks and estimation of finite strainsGeological Society of America Bulletin, 90
C. Scholz, R. Kranz (1974)
Notes on dilatancy recoveryJournal of Geophysical Research, 79
E. Rutter (1983)
Pressure solution in nature, theory and experimentJournal of the Geological Society, 140
J. Vedder, R. Wallace (1968)
Map showing recently active breaks along the San Andreas and related faults between Cholame Valley and Tejon Pass, California
W. House, D. Gray (1982)
Cataclasites along the Saltville thrust, U.S.A. and their implications for thrust-sheet emplacementJournal of Structural Geology, 4
S. Kirby (1983)
Rheology of the lithosphereReviews of Geophysics, 21
J. Engelder, J. Logan, J. Handin (1975)
The sliding characteristics of sandstone on quartz fault-gougepure and applied geophysics, 113
T. Engelder (1978)
Aspects of asperity-surface interaction and surface damage of rocks during experimental frictional slidingpure and applied geophysics, 116
M. Etheridge, J. Wilkie (1979)
Grainsize reduction, grain boundary sliding and the flow strength of mylonitesTectonophysics, 58
F. Wu (1978)
Mineralogy and physical nature of clay gougepure and applied geophysics, 116
D. McKenzie, J. Brune (1972)
Melting on Fault Planes During Large EarthquakesGeophysical Journal International, 29
G. Mitra (1984)
Brittle to ductile transition due to large strains along the White Rock thrust, Wind River mountains, WyomingJournal of Structural Geology, 6
K. Ramseyer, J. Boles (1986)
Mixed-Layer Illite/Smectite Minerals in Tertiary Sandstones and Shales, San Joaquin Basin, CaliforniaClays and Clay Minerals, 34
J. Grocott (1977)
The relationship between Precambrian shear belts and modern fault systemsJournal of the Geological Society, 133
A. Nur (1975)
A note on the constitutive law for dilatancypure and applied geophysics, 113
H. Moore, R. Sibson (1978)
Experimental thermal fragmentation in relation to seismic faultingTectonophysics, 49
R. Burford, P. Harsh (1980)
Slip on the San Andreas fault in central California from alinement array surveysBulletin of the Seismological Society of America, 70
R. Sibson (1983)
Continental fault structure and the shallow earthquake sourceJournal of the Geological Society, 140
J. Ramsay, R. Graham (1970)
Strain variation in shear beltsCanadian Journal of Earth Sciences, 7
W. Thatcher, J. Hileman, T. Hanks (1975)
Seismic Slip Distribution along the San Jacinto Fault Zone, Southern California, and Its ImplicationsGeological Society of America Bulletin, 86
R. Sibson (1977)
Fault rocks and fault mechanismsJournal of the Geological Society, 133
A. Ord, J. Christie (1984)
Flow stresses from microstructures in mylonitic quartzites of the Moine Thrust zone, Assynt area, ScotlandJournal of Structural Geology, 6
G. Davis (1983)
Shear-zone model for the origin of metamorphic core complexesGeology, 11
T. Hanks (1977)
Earthquake stress drops, ambient tectonic stresses and stresses that drive plate motionspure and applied geophysics, 115
S. White (1976)
A Discussion on natural strain and geological structure - The effects of strain on the microstructures, fabrics, and deformation mechanisms in quartzitesPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 283
R. Sibson (1982)
Fault zone models, heat flow, and the depth distribution of earthquakes in the continental crust of the United StatesBulletin of the Seismological Society of America, 72
W. Ortlepp (1979)
Anatomy of a mining-induced fault zoneGeological Society of America Bulletin, 90
R. Bustin (1983)
Heating during thrust faulting in the rocky mountains: friction or fiction?Tectonophysics, 95
K. Sørensen (1983)
Growth and dynamics of the Nordre Strømfjord Shear ZoneJournal of Geophysical Research, 88
P. Reasenberg, W. Ellsworth (1982)
Aftershocks of the Coyote Lake, California, earthquake of August 6, 1979: A detailed studyJournal of Geophysical Research, 87
C. Angevine, D. Turcotte, M. Furnish (1982)
Pressure solution lithification as a mechanism for the stick‐slip behavior of faultsTectonics, 1
G. Mitra (1978)
Ductile deformation zones and mylonites; the mechanical processes involved in the deformation of crystalline basement rocksAmerican Journal of Science, 278
S. Schmid, J. Boland, M. Paterson (1977)
Superplastic flow in finegrained limestoneTectonophysics, 43
J. Brune (1976)
Chapter 5 - The Physics of Earthquake Strong MotionDevelopments in Geotechnical Engineering, 15
B. Atkinson (1984)
Subcritical crack growth in geological materialsJournal of Geophysical Research, 89
J. Brewer (1981)
Thermal effects of thrust faultingEarth and Planetary Science Letters, 56
T. Bell, R. Hammond (1984)
On the Internal Geometry of Mylonite ZonesThe Journal of Geology, 92
R. Hyndman, D. Weichert (1983)
Seismicity and rates of relative motion on the plate boundaries of Western North AmericaGeophysical Journal International, 72
S. Schmid, M. Casey, J. Starkey (1981)
The microfabric of calcite tectonites from the Helvetic Nappes (Swiss Alps)Geological Society, London, Special Publications, 9
R. Sibson (1980)
Power dissipation and stress levels on faults in the upper crustJournal of Geophysical Research, 85
P. Bird (1984)
Hydration-phase diagrams and friction of montmorillonite under laboratory and geologic conditions, with implications for shale compaction, slope stability, and strength of fault gougeTectonophysics, 107
P. Gretener (1977)
On the Character of Thrust Faults With Particular Reference to the Basal TonguesBulletin of Canadian Petroleum Geology, 25
R. Bucknam, G. Plafker, R. Sharp (1978)
Fault movement (afterslip) following the Guatemala earthquake of February 4, 1976Geology, 6
T. Hanks, C. Raleigh (1980)
The conference on magnitude of deviatoric stresses in the Earth's crust and uppermost mantleJournal of Geophysical Research, 85
R. Cardwell, D. Chinn, G. Moore, D. Turcotte (1978)
Authors' reply to ‘A comment on ‘Frictional heating on a fault zone with finite thickness’’Geophysical Journal International, 56
S. White, S. Burrows, J. Carreras, N. Shaw, F. Humphreys (1980)
On mylonites in ductile shear zonesJournal of Structural Geology, 2
R. Sibson (1985)
Stopping of earthquake ruptures at dilational fault jogsNature, 316
R. Sibson (1975)
Generation of Pseudotachylyte by Ancient Seismic FaultingGeophysical Journal International, 43
K. McClay (1977)
Pressure solution and Coble creep in rocks and minerals: a reviewJournal of the Geological Society, 134
H. Melosh (1979)
Acoustic fluidization: A new geologic process?Journal of Geophysical Research, 84
D. Kohlstedt, M. Weathers (1980)
Deformation‐induced microstructures, paleopiezometers, and differential stresses in deeply eroded fault zonesJournal of Geophysical Research, 85
A. Beach (1980)
Retrogressive metamorphic processes in shear zones with special reference to the Lewisian complexJournal of Structural Geology, 2
P. Okubo, J. Dieterich (1984)
Effects of physical fault properties on frictional instabilities produced on simulated faultsJournal of Geophysical Research, 89
C. Simpson (1985)
Deformation of granitic rocks across the brittle-ductile transitionJournal of Structural Geology, 7
A. Boullier, Y. Guéguen (1975)
SP-Mylonites: Origin of some mylonites by superplastic flowContributions to Mineralogy and Petrology, 50
The physical origin of earthquakes lies ultimately in the geological structure of fault zones and the deformation processes that occur therein in response to tectonic stress. Although the possibility now exists that the nucleation regions for large earthquakes at depths of,..., 10 km may shortly become directly accessible by deep drilling, our present knowledge of fault structure and the shallow earthquake source is derived largely from a variety of indirect sources. These include seismological studies, surface studies of fault zones and earthquake ruptures, geodetic information on modes of fault slip, ·geophysical constraints on fault zone structure and rheology, and information garnered from materials science and experi mental rock deformation. Studies of fault zone structure and the rock products of faulting provide complementary information on deformation processes at depth in fault zones. Although descriptions of fault rocks are widespread in the geological literature (e.g. Spry 1969, Higgins 1971), it is only in the past decade that they have begun to be interpreted in the context of the physical conditions and processes prevalent in seismically active fault zones at different crustal depths (Sibson 1977, Watts & Williams 1979, Anderson et a11983, Wise et aI 1984). Such interpretations are still at
Annual Review of Earth and Planetary Sciences – Annual Reviews
Published: May 1, 1986
Read and print from thousands of top scholarly journals.
Already have an account? Log in
Bookmark this article. You can see your Bookmarks on your DeepDyve Library.
To save an article, log in first, or sign up for a DeepDyve account if you don’t already have one.
Copy and paste the desired citation format or use the link below to download a file formatted for EndNote
Access the full text.
Sign up today, get DeepDyve free for 14 days.
All DeepDyve websites use cookies to improve your online experience. They were placed on your computer when you launched this website. You can change your cookie settings through your browser.