Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Sara Wassmann"'
Exhumed metamorphic rocks from fossil subduction zones represent a unique source of information on the microscale deformation mechanisms and stress history within the seismogenic domain in subduction zones. Microstructural analysis of these rocks yie
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b6243c2692061f41a850113ae82980d1
https://doi.org/10.5194/egusphere-egu23-16761
https://doi.org/10.5194/egusphere-egu23-16761
Publikováno v:
Solid Earth, Vol 5, Iss 1, Pp 141-159 (2014)
Return flow in a deep subduction channel (DSC) has been proposed to explain rapid exhumation of high pressure–low temperature metamorphic rocks, entirely based on the fossil rock record. Supported by thermo-mechanical models, the DSC is envisioned
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e94d89109a7f487777afda0610e89c4a
https://www.solid-earth.net/5/141/2014/
https://www.solid-earth.net/5/141/2014/
Rheology of the plate interface — Dissolution precipitation creep in high pressure metamorphic rocks
Autor:
Sara Wassmann, Bernhard Stöckhert
Publikováno v:
Tectonophysics. 608:1-29
Subduction zone models invoke deformation to be concentrated along the plate interface, in a region of particularly low temperature. Geophysical observations do not provide constraints on temperature, stress and deformation patterns with desired reso
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::546e0a58b54f7d5080ce00190d637f88
https://doi.org/10.1016/j.tecto.2013.09.030
https://doi.org/10.1016/j.tecto.2013.09.030
Publikováno v:
Tectonics. 32:1272-1293
[1] The structural record at the base of a basement nappe (Preveli nappe, Crete, Greece) thrust upon sedimentary rocks is investigated, aimed on understanding mechanisms which result in decoupling of the thrust sheet from its original substratum. We
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::af2499d6e3a8bbe4e10b33614535273c
https://doi.org/10.1002/tect.20079
https://doi.org/10.1002/tect.20079
Autor:
Sara Wassmann, Bernhard Stöckhert
Publikováno v:
Journal of Structural Geology. 46:200-219
Microstructures indicating incongruent dissolution precipitation creep of garnet in eclogite-facies graphitic micaschist (Tauern window, Eastern Alps) are investigated. Garnet dissolution is observed where garnet poikiloblasts grown at eclogite facie
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c6b545cda01fee39a92f1a43ec069545
https://doi.org/10.1016/j.jsg.2012.09.002
https://doi.org/10.1016/j.jsg.2012.09.002
Publikováno v:
Tectonophysics. :86-101
Many tectonic HP–LT melanges exhibit block-in-matrix structures. In contrast to the pervasively deformed matrix, the blocks of various lithologies and PT-histories usually appear undeformed. If we accept that an HP–LT melange reflects persistent
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::182960730b7eaf33e3efb01ac04ecac2
https://doi.org/10.1016/j.tecto.2011.11.004
https://doi.org/10.1016/j.tecto.2011.11.004
Autor:
Sara Wassmann, Bernhard Stöckhert
Publikováno v:
Tectonophysics. :135-153
Exhumed high pressure–low temperature metamorphic melanges of tectonic origin are believed to reflect high strain accumulated in large scale interplate shear zones during subduction. Rigid blocks of widely varying size are embedded in a weak matrix
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2b7a6f9d89d2a1fb85b805242a3cf9ee
https://doi.org/10.1016/j.tecto.2012.01.009
https://doi.org/10.1016/j.tecto.2012.01.009
Publikováno v:
Geological Society, London, Special Publications. 360:129-149
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::99e4e8efeb0dc49720c323b0ea295470
https://doi.org/10.1144/sp360.8
https://doi.org/10.1144/sp360.8