Low-frequency earthquakes reveal punctuated slow slip on the deep extent of the Alpine Fault, New Zealand
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Large-displacement, hydrothermal frictional properties of DFDP-1 fault rocks, Alpine Fault, New Zealand: Implications for deep rupture propagation.Shear behavior of DFDP-1 borehole samples from the Alpine Fault, New Zealand, under a wide range of experimental conditionsLithospheric shear velocity structure of South Island, New Zealand, from amphibious Rayleigh wave tomographyA 15 year catalog of more than 1 million low-frequency earthquakes: Tracking tremor and slip along the deep San Andreas FaultConstraints on the source parameters of low-frequency earthquakes on the San Andreas FaultPetrophysical, Geochemical, and Hydrological Evidence for Extensive Fracture-Mediated Fluid and Heat Transport in the Alpine Fault's Hanging-Wall Damage ZoneMicroseismicity and P–wave tomography of the central Alpine Fault, New ZealandFault Zone Guided Wave generation on the locked, late interseismic Alpine Fault, New ZealandStructural heterogeneity of the midcrust adjacent to the central Alpine Fault, New Zealand: Inferences from seismic tomography and seismicity between Harihari and Ross
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Low-frequency earthquakes reveal punctuated slow slip on the deep extent of the Alpine Fault, New Zealand
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article
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wetenschappelijk artikel
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наукова стаття, опублікована в липні 2014
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name
Low-frequency earthquakes reve ...... the Alpine Fault, New Zealand
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Low-frequency earthquakes reve ...... the Alpine Fault, New Zealand
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Low-frequency earthquakes reve ...... the Alpine Fault, New Zealand
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Low-frequency earthquakes reve ...... the Alpine Fault, New Zealand
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Low-frequency earthquakes reve ...... the Alpine Fault, New Zealand
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Low-frequency earthquakes reve ...... the Alpine Fault, New Zealand
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Low-frequency earthquakes reve ...... the Alpine Fault, New Zealand
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Tim A. Stern
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10.1002/2014GC005436
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2014-07-01T00:00:00Z