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Strike-slip faults
(U.S. Geological Survey, 2016)
Strike-slip faults
(U.S. Geological Survey, 2011)
True three-dimensional trishear: A kinematic model for strike-slip and oblique-slip deformation
(Geological Society of America, 2004-07-01)
Most structural/kinematic models are inherently two-dimensional; even several recent three-dimensional models are "pseudo-three-dimensional" in that they consist of a series of parallel two-dimensional cross sections. Lack ...
Control of strike-slip fault on dyke emplacement and morphology
(Geological Society of London, 2016-07)
Strike-slip faults are commonly assumed to influence magma transport and emplacement in the Earth’s crust. However, direct observations of magma conduits within strike-slip faults are lacking. Here we provide some of the ...
Comment on “Crustal faults in the Chilean Andes: geological constraints and seismic potential” by Santibáñez et al. (2019), Andean Geology 46 (1): 32-65
(Servicio Naconal de Geología y Minería, Chile, 2021)
States of stress and slip partitioning in a continental scale strike-slip duplex: tectonic and magmatic implications by means of finite element modeling
(Elsevier, 2017)
Orogenic belts at oblique convergent subduction margins accommodate deformation in several trench parallel domains, one of which is the magmatic arc, commonly regarded as taking up the margin-parallel, strike-slip component. ...
Seismic and aseismic slip on the Central Peru megathrust
(Nature Research, 2010-05-06)
Slip on a subduction megathrust can be seismic or aseismic, with the two modes of slip complementing each other in time and space to accommodate the long-term plate motions. Although slip is almost purely aseismic at depths ...
Slow slip transients along the Oaxaca subduction segment from 1993 to 2007
(2007)
We use data from 12 continuous GPS stations in southern Mexico, including eight new stations, to better characterize transient slip episodes along the Mexican subduction zone. Continuous GPS recording in Oaxaca that began ...
Slow slip transients along the Oaxaca subduction segment from 1993 to 2007
(2007)
We use data from 12 continuous GPS stations in southern Mexico, including eight new stations, to better characterize transient slip episodes along the Mexican subduction zone. Continuous GPS recording in Oaxaca that began ...