Steady-State Failure Equilibrium and Deformation of Intraplate Lithosphere
about
Geologic carbon storage is unlikely to trigger large earthquakes and reactivate faults through which CO2 could leakEarthquake triggering and large-scale geologic storage of carbon dioxide.Induced earthquakes. Sharp increase in central Oklahoma seismicity since 2008 induced by massive wastewater injection.Porphyry-copper ore shells form at stable pressure-temperature fronts within dynamic fluid plumesHeating, weakening and shear localization in earthquake rupture.Structural heterogeneity of the midcrust adjacent to the central Alpine Fault, New Zealand: Inferences from seismic tomography and seismicity between Harihari and RossWhat do faults feel? Observational constraints on the stresses acting on seismogenic faults
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Steady-State Failure Equilibrium and Deformation of Intraplate Lithosphere
description
wetenschappelijk artikel
@nl
наукова стаття, опублікована в травні 2002
@uk
name
Steady-State Failure Equilibrium and Deformation of Intraplate Lithosphere
@en
Steady-State Failure Equilibrium and Deformation of Intraplate Lithosphere
@nl
type
label
Steady-State Failure Equilibrium and Deformation of Intraplate Lithosphere
@en
Steady-State Failure Equilibrium and Deformation of Intraplate Lithosphere
@nl
prefLabel
Steady-State Failure Equilibrium and Deformation of Intraplate Lithosphere
@en
Steady-State Failure Equilibrium and Deformation of Intraplate Lithosphere
@nl
P2860
P1476
Steady-State Failure Equilibrium and Deformation of Intraplate Lithosphere
@en
P2093
Balz Grollimund
P2860
P304
P356
10.2747/0020-6814.44.5.383
P577
2002-05-01T00:00:00Z