How phyllosilicate mineral structure affects fault strength in Mg-rich fault systems

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How phyllosilicate mineral structure affects fault strength in Mg-rich fault systems

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im Juni 2017 veröffentlichter wissenschaftlicher Artikel

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wetenschappelijk artikel

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наукова стаття, опублікована в червні 2017

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How phyllosilicate mineral structure affects fault strength in Mg-rich fault systems

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How phyllosilicate mineral structure affects fault strength in Mg-rich fault systems

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How phyllosilicate mineral structure affects fault strength in Mg-rich fault systems

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How phyllosilicate mineral structure affects fault strength in Mg-rich fault systems

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How phyllosilicate mineral structure affects fault strength in Mg-rich fault systems

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How phyllosilicate mineral structure affects fault strength in Mg-rich fault systems

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P1476

How phyllosilicate mineral structure affects fault strength in Mg-rich fault systems

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P2093

D. R. Faulkner

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J. Jimenez-Millan

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P2860

Low strength of deep San Andreas fault gouge from SAFOD core.

Talc-bearing serpentinite and the creeping section of the San Andreas fault.

Friction of rocks

Geochemical and microstructural evidence for interseismic changes in fault zone permeability and strength, Alpine Fault, New Zealand

Relationships between the microstructural evolution and the rheology of talc at elevated pressures and temperatures

Composition, Alteration, and Texture of Fault-Related Rocks from Safod Core and Surface Outcrop Analogs: Evidence for Deformation Processes and Fluid-Rock Interactions

Laboratory measurements of the frictional properties of the Zuccale low-angle normal fault, Elba Island, Italy

Effect of geologic structure and metamorphic fluids on seismic behavior of the San Andreas fault system in central and northern California

Earthquakes and friction laws

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5457-5467

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P31

scholarly article

P356

10.1002/2017GL073055

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P407

English

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P478

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P50

Carolyn J. Boulton

Fernando Nieto

Catalina Sánchez-Roa

P577

2017-06-12T00:00:00Z

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P921

geophysics