Zobrazeno 1 - 10
of 44
pro vyhledávání: '"Uwe Kroner"'
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-21 (2023)
Abstract The spatial analysis of horizontal stress orientation is important to study stress sources and understand tectonics and the deformation of the lithosphere. Additional to the stress sources, the geometry of stress fields depends on the underl
Externí odkaz:
https://doaj.org/article/161ddcf442f8482b8d88c5e87e33b5d9
To be a quantitative and testable tectonic model, plate tectonics requires spherical geometry and spherical kinematics in terms of finite rotations conveniently parametrized by their angle and axis and described by unit quaternions. In treatises on
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7520b7c67eccc87a7dc726a12d91a689
https://doi.org/10.22541/au.168137161.12641139/v1
https://doi.org/10.22541/au.168137161.12641139/v1
Publikováno v:
Zeitschrift der Deutschen Gesellschaft für Geowissenschaften.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4db1bee3ebf8ff00b99341a956db3acc
https://doi.org/10.1127/zdgg/2023/0365
https://doi.org/10.1127/zdgg/2023/0365
Publikováno v:
Geochimica et Cosmochimica Acta. 314:178-208
Felsic rocks of the Erzgebirge in the Central European Variscides experienced ultra-high pressure metamorphism at ∼340 Ma, followed by nearly isothermal decompression during channel like rapid exhumation within ∼10 Ma. Despite the general time fr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8e8ccb67133f16afcf733a078cc7d1fa
https://doi.org/10.1016/j.gca.2021.08.043
https://doi.org/10.1016/j.gca.2021.08.043
Autor:
Franz Müller, Uwe Kroner
Publikováno v:
Zeitschrift der Deutschen Gesellschaft für Geowissenschaften.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cdb597f9f725867071200e30fecda456
https://doi.org/10.1127/zdgg/2022/0331
https://doi.org/10.1127/zdgg/2022/0331
Publikováno v:
New Developments in the Appalachian-Caledonian-Variscan Orogen
GSA Special Papers ; 554
GSA Special Papers ; 554
Early Ordovician to late Permian orogenies at different plate-boundary zones of western Pangea affected continental crust derived from the plates of North America (Laurentia), Europe (East European Craton including Baltica plus Arctida), and Gondwana
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5aa9d51f3be49568f17a49b20d281691
https://doi.org/10.1130/2021.2554(001)
https://doi.org/10.1130/2021.2554(001)
Publikováno v:
Geological Society, London, Special Publications. 503:83-104
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a5edc1afe3b436b6fe6ddf718677c7b9
https://doi.org/10.1144/sp503-2020-15
https://doi.org/10.1144/sp503-2020-15
Autor:
Rolf L. Romer, Uwe Kroner
Publikováno v:
New Developments in the Appalachian-Caledonian-Variscan Orogen
GSA Special Papers ; 554
GSA Special Papers ; 554
The Paleozoic plate boundary zone between Laurussia and Gondwana in western Pangea hosts major magmatic and hydrothermal Sn-W-Ta, Au, and U mineralization. Individual mineral deposits represent the results of the superposition of a series of exogenic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::10d1b0a8e26deb5c447f90210f341692
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011663
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011663
Publikováno v:
Geology
Major tin (Sn) deposits within the Variscan orogen are closely related to 325–270 Ma postkinematic granites that intruded the metamorphic rocks of the former precollisional accretionary wedge of the Gondwana margin. In the Erzgebirge (Germany), som
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e226f85ed1bf072f46e88fccc2d7c938
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5013632
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5013632
For permanent nuclear waste disposal sites, crystalline rocks, especially granitic/granodioritic batholiths, are considered an appropriate host rock. Principally, three types of granitic plutons occur in the extra-alpine crystalline basement of Germa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9d7dfc4ef4cdf537bed56aaf3102da62
https://sand.copernicus.org/articles/1/67/2021/
https://sand.copernicus.org/articles/1/67/2021/