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نمایش تعداد 1-10 از 22

Laboratory constraints on models of earthquake recurrence

نوع: Journal Paper

ناشر: American Geophysical Union

سال: 2014

Importance of mechanochemical effects on fault slip behavior during earthquakes

نوع: Journal Paper

ناشر: Wiley

سال: 2013

Mineral assemblage anomalies in the slip zone of the 1999 Taiwan Chi Chi earthquake: Ultrafine particles preserved only in the latest slip zone

نوع: Journal Paper

ناشر: American Geophysical Union

سال: 2014

Dynamic weakening of serpentinite gouges and bare surfaces at seismic slip rates

نوع: Journal Paper

ناشر: American Geophysical Union

سال: 2014

Fault frictional parameters and material properties revealed by slow slip events at Kilauea volcano, Hawaiâ€˜i

نوع: Journal Paper

ناشر: Wiley

سال: 2013

A slower fault may produce a smaller preseismic moment rate: Non 1/tf acceleration of moment rate during nucleation and

نوع: Journal Paper

نویسنده : dependency on the background slip rate

ناشر: Wiley

سال: 2013

Are scale invariant stress orientations related to seismicity rates near the San Andreas fault?

نوع: Journal Paper

نویسنده : Davidsen, Jörn - Schumann, Aicko Y. - Naylor, Mark

ناشر: Wiley

سال: 2013

Predicting fault damage zones by modeling dynamic rupture propagation and comparison with field observations

نوع: Journal Paper

ناشر: � American Geophysical Union

سال: 2014

Under what circumstances does a seismogenic patch produce aseismic transients in the later interseismic period?

نوع: Journal Paper

نویسنده : Noda, H. - Hori, T.

ناشر: American Geophysical Union

سال: 2014

Rock and mineral transformations in a fault zone leading to permanent creep: Interactions between brittle and viscous mechanisms in the San Andreas Fault

نوع: Journal Paper

ناشر: American Geophysical Union

سال: 2014

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Laboratory constraints on models of earthquake recurrence

Importance of mechanochemical effects on fault slip behavior during earthquakes

Mineral assemblage anomalies in the slip zone of the 1999 Taiwan Chi Chi earthquake: Ultrafine particles preserved only in the latest slip zone

Dynamic weakening of serpentinite gouges and bare surfaces at seismic slip rates

Fault frictional parameters and material properties revealed by slow slip events at Kilauea volcano, Hawaiâ€˜i

A slower fault may produce a smaller preseismic moment rate: Non 1/tf acceleration of moment rate during nucleation and

Are scale invariant stress orientations related to seismicity rates near the San Andreas fault?

Predicting fault damage zones by modeling dynamic rupture propagation and comparison with field observations

Under what circumstances does a seismogenic patch produce aseismic transients in the later interseismic period?

Rock and mineral transformations in a fault zone leading to permanent creep: Interactions between brittle and viscous mechanisms in the San Andreas Fault

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Laboratory constraints on models of earthquake recurrence

Importance of mechanochemical effects on fault slip behavior during earthquakes

Mineral assemblage anomalies in the slip zone of the 1999 Taiwan Chi Chi earthquake: Ultrafine particles preserved only in the latest slip zone

Dynamic weakening of serpentinite gouges and bare surfaces at seismic slip rates

Fault frictional parameters and material properties revealed by slow slip events at Kilauea volcano, Hawaiâ€˜i

A slower fault may produce a smaller preseismic moment rate: Non 1/tf acceleration of moment rate during nucleation and

Are scale invariant stress orientations related to seismicity rates near the San Andreas fault?

Predicting fault damage zones by modeling dynamic rupture propagation and comparison with field observations

Under what circumstances does a seismogenic patch produce aseismic transients in the later interseismic period?

Rock and mineral transformations in a fault zone leading to permanent creep: Interactions between brittle and viscous mechanisms in the San Andreas Fault