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Numerical simulations on megathrust rupture stabilized under strong dilatancy strengthening in slow slip region

نوع: Journal Paper

ناشر: Wiley

سال: 2013

The Coulomb critical taper theory applied to gravitational instabilities

نوع: Journal Paper

نویسنده : Mourgues, R. - Lacoste, A. - Garibaldi, C.

ناشر: � American Geophysical Union

سال: 2014

Displacement and dynamic weakening processes in smectite rich gouge from the Central Deforming Zone of the San Andreas Fault

نوع: Journal Paper

ناشر: � American Geophysical Union

سال: 2014

Shallow, old, and hydrologically insignificant fault zones in the Appalachian orogen

نوع: Journal Paper

نویسنده : Malgrange, Juliette - Gleeson, Tom

ناشر: � American Geophysical Union

سال: 2014

Deep fluids can facilitate rupture of slow moving giant landslides as a result of stress transfer and frictional weakening

نوع: Journal Paper

ناشر: American Geophysical Union

سال: 2014

Deep long period earthquakes west of the volcanic arc in Oregon: Evidence of serpentine dehydration in the fore arc mantle wedge

نوع: Journal Paper

ناشر: American Geophysical Union

سال: 2014

Evidence for fluid triggered slip in the 2009 Mount Rainier, Washington earthquake swarm

نوع: Journal Paper

ناشر: Wiley

سال: 2013

Imaging the source regions of normal faulting sequences induced by the 2011â€‰M9.0 Tohoku Oki earthquake

نوع: Journal Paper

ناشر: Wiley

سال: 2013

Source duration of stress and water pressure induced seismicity derived from experimental analysis of P wave pulse widt

نوع: Journal Paper

نویسنده : h in granite

ناشر: Wiley

سال: 2013

Conditions and threshold for magma transfer in the layered upper crust: Insights from experimental models

نوع: Journal Paper

ناشر: Wiley

سال: 2013

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Numerical simulations on megathrust rupture stabilized under strong dilatancy strengthening in slow slip region

The Coulomb critical taper theory applied to gravitational instabilities

Displacement and dynamic weakening processes in smectite rich gouge from the Central Deforming Zone of the San Andreas Fault

Shallow, old, and hydrologically insignificant fault zones in the Appalachian orogen

Deep fluids can facilitate rupture of slow moving giant landslides as a result of stress transfer and frictional weakening

Deep long period earthquakes west of the volcanic arc in Oregon: Evidence of serpentine dehydration in the fore arc mantle wedge

Evidence for fluid triggered slip in the 2009 Mount Rainier, Washington earthquake swarm

Imaging the source regions of normal faulting sequences induced by the 2011â€‰M9.0 Tohoku Oki earthquake

Source duration of stress and water pressure induced seismicity derived from experimental analysis of P wave pulse widt

Conditions and threshold for magma transfer in the layered upper crust: Insights from experimental models

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Numerical simulations on megathrust rupture stabilized under strong dilatancy strengthening in slow slip region

The Coulomb critical taper theory applied to gravitational instabilities

Displacement and dynamic weakening processes in smectite rich gouge from the Central Deforming Zone of the San Andreas Fault

Shallow, old, and hydrologically insignificant fault zones in the Appalachian orogen

Deep fluids can facilitate rupture of slow moving giant landslides as a result of stress transfer and frictional weakening

Deep long period earthquakes west of the volcanic arc in Oregon: Evidence of serpentine dehydration in the fore arc mantle wedge

Evidence for fluid triggered slip in the 2009 Mount Rainier, Washington earthquake swarm

Imaging the source regions of normal faulting sequences induced by the 2011â€‰M9.0 Tohoku Oki earthquake

Source duration of stress and water pressure induced seismicity derived from experimental analysis of P wave pulse widt

Conditions and threshold for magma transfer in the layered upper crust: Insights from experimental models