Zobrazeno 1 - 4
of 4
pro vyhledávání: '"J. F. A. Diener"'
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 25, Iss 3, Pp n/a-n/a (2024)
Abstract The Malawi Rift is localized within Precambrian amphibolite‐granulite facies metamorphic belts, bounded by up to 150 km long border faults, and generates earthquakes throughout ∼40 km thick crust. Rift‐related faults are inferred to ex
Externí odkaz:
https://doaj.org/article/254c3dbf444c4212b241e10e60b966a7
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 23, Iss 9, Pp n/a-n/a (2022)
Abstract Geophysical observations indicate that patches of localized fracturing occur within otherwise viscous regions of subduction plate boundaries. These observations place uncertainty on the possible down‐dip extent of the seismogenic zone, and
Externí odkaz:
https://doaj.org/article/b038da036eeb49d8aaf34a7efe33ae5a
Publikováno v:
Geofluids, Vol 2020 (2020)
Midcrustal rocks in retrograde metamorphic settings are typically H2O-undersaturated and fluid-absent and have low permeability. Exhumed continental retrograde faults, nonetheless, show evidence for the operation of fluid-mediated weakening mechanism
Externí odkaz:
https://doaj.org/article/737d90395e0a48db950e0ce58026c47d
Publikováno v:
Solid Earth, Vol 7, Iss 5, Pp 1331-1347 (2016)
The Kuckaus Mylonite Zone (KMZ) forms part of the larger Marshall Rocks–Pofadder shear zone system, a 550 km-long, crustal-scale strike-slip shear zone system that is localized in high-grade granitoid gneisses and migmatites of the Namaqua Metamorp
Externí odkaz:
https://doaj.org/article/eee576715e474ce8bba45bfab461253e