Zobrazeno 1 - 10
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pro vyhledávání: '"Dave May"'
A recently developed continuum formulation of rate and state friction (Pranger et al., 2022) treats fault friction as an internal flow process in a granular medium, instead of its conventional treatment as a sliding process on a surface between juxta
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::429b28bc4656872a898cfc4b80676608
https://doi.org/10.5194/egusphere-egu23-13815
https://doi.org/10.5194/egusphere-egu23-13815
Geological and geophysical observations have highlighted the multi-stage deformation history of the continental lithosphere. Such inherited heterogeneities, observed from microscopic to kilometre-scales, lead to important mechanical weakening for the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ae93e3dbe041a4ffa02e6a024993db2f
https://doi.org/10.5194/egusphere-egu23-13519
https://doi.org/10.5194/egusphere-egu23-13519
Basin inversion is usually associated with compressional uplift and erosion of the exhuming sedimentary succession, while the resulting uplift rates are governed by variable convergence rates and the inherited lithospheric structure. However, observa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::25c8cd23a2729c517b7d06e037583bc8
https://doi.org/10.5194/egusphere-egu23-671
https://doi.org/10.5194/egusphere-egu23-671
Two-phase flow, a system where Stokes flow and Darcy flow are coupled, is of great importance in the Earth's interior, such as in subduction zones, mid-ocean ridges, and hotspots. However, it remains challenging to solve the two-phase equations accur
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https://explore.openaire.eu/search/publication?articleId=doi_________::2097fd295314c3ef2181f85293ecb051
https://doi.org/10.5194/egusphere-egu23-6105
https://doi.org/10.5194/egusphere-egu23-6105
Dykes are tensile fractures that rapidly transport magma from the hot, ductile asthenosphere across the cold, brittle upper lithosphere. They play an important role in tectonic extension settings by drastically reducing the force needed for rifting (
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https://explore.openaire.eu/search/publication?articleId=doi_________::f8980afd0693b250d9f3c4e847640fdb
https://doi.org/10.5194/egusphere-egu23-14818
https://doi.org/10.5194/egusphere-egu23-14818
Continental rifting is often oblique to the rift axis or plate boundary, comprising many active rifts and mature rifted margins on Earth. Previous research has identified the role of vertical strike-slip and transform structures in oblique extension
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https://explore.openaire.eu/search/publication?articleId=doi_________::a858121a5eb336f39c76f75fe5bef19e
https://doi.org/10.5194/egusphere-egu23-13192
https://doi.org/10.5194/egusphere-egu23-13192
Autor:
Robert Lewis Walker, Matthew Knepley, Brad T Aagaard, Charles A. Williams, Simone Puel, Dave May, Brittany Erickson, Daniel Shapero, Colin Meyer
PyLith, a community, open-source code (\url{https://geodynamics.org/resources/pylith/}) for modeling quasi-static and dynamic crustal deformation with an emphasis on earthquake faulting, has recently been updated with a flexible multiphysics implemen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::37e4bf30cb41eb8c9c74e99b36e15cd5
https://doi.org/10.22541/essoar.167039842.28194633/v1
https://doi.org/10.22541/essoar.167039842.28194633/v1
Publikováno v:
e2022JB024687
Journal of Geophysical Research (JGR): Solid Earth
Journal of Geophysical Research (JGR): Solid Earth
Continental rifts grow by propagation, overlap and linkage of individual fault segments. These processes are influenced by erosion and sedimentation and generate complex three-dimensional fault-interaction patterns. We use a 3D thermo-mechanical mode
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::70063e185301ef6a0696fd0095a103a5
https://doi.org/10.1029/2022jb024687
https://doi.org/10.1029/2022jb024687
Under dynamic perturbations, it has been observed that materials like sedimentary rocks show complex mechanical behaviors. They include the simultaneous dependence of the elastic moduli and attenuation on strain at the same time scale of the perturba
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eaebe3ecaed7cb9b88eb436299342766
https://doi.org/10.5194/egusphere-egu22-10523
https://doi.org/10.5194/egusphere-egu22-10523
Passive and transform margins emerging during continental rifting and opening of oceanic basins are fundamental elements of plate tectonics. It has been suggested that inherited structures, variable plate divergence velocities and surface processes e
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7e86de1ea5586c6b60523a13c21a5a2b
https://doi.org/10.5194/egusphere-egu22-8005
https://doi.org/10.5194/egusphere-egu22-8005