Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Markus E. Schumacher"'
Publikováno v:
International Journal of Earth Sciences. 94:640-656
A large-scale transfer zone subdivides the northern parts of the Upper Rhine Graben into a northern and a southern sub-basin. These sub-basins display the geometry of asymmetric half-grabens with opposing tilt directions. The transfer zone connects t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c5c132fe43befcda3c4efdf6befda2bd
https://doi.org/10.1007/s00531-005-0515-y
https://doi.org/10.1007/s00531-005-0515-y
Publikováno v:
Quaternary Science Reviews. 24:363-380
Analogue experiments on oblique rifting and subsequent transpressional reactivation were performed with two-layer slabs of sand and silicone. In this brittle–viscous system, transtensional and transpressional wrench faulting was induced by movement
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::420ae3cb1f96284ab184fcb421c4775c
https://doi.org/10.1016/j.quascirev.2004.03.015
https://doi.org/10.1016/j.quascirev.2004.03.015
Publikováno v:
International Journal of Earth Sciences. 94:680-696
The southern end of the Upper Rhine Graben (URG) is formed by a major continental transfer zone, which was localised by the reactivation of ENE-oriented basement faults of Late Palaeozoic origin. A combination of subcrop data (derived from exploratio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ad32a8265a772f26c13c04be57bd13cc
https://doi.org/10.1007/s00531-004-0454-z
https://doi.org/10.1007/s00531-004-0454-z
Publikováno v:
Eclogae Geologicae Helvetiae. 97:17-31
The southern Rhinegraben represents a key area to unravel the Neogene paleohydrographic history of the northern Alpine foreland. At least, three successive main drainage systems are documented by the youngest sediments of the graben fill. They are re
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::499347bd749627f70d4b9fa8d645849d
https://doi.org/10.1007/s00015-004-1112-4
https://doi.org/10.1007/s00015-004-1112-4
Publikováno v:
Marine and Petroleum Geology. 14:3-25
In order to evaluate the petroleum potential of southern Switzerland (south-Alpine fold-and-thrust belt), gas geochemical investigations including free and adsorbed gases were combined with a basin modelling analysis. The palaeotectonic setting and A
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b1bce2a7e90bbf35306194ca39a0162d
https://doi.org/10.1016/s0264-8172(96)00037-2
https://doi.org/10.1016/s0264-8172(96)00037-2
Publikováno v:
Giamboni, M.; Ustaszewski, K.; Schmid, S. M.; Schumacher, M. E.; Wetzel, Alexander (2004). Plio-Pleistocene transpressional reactivation of Paleozoic and Paleogene structures in the Rhine-Bresse transform zone (northern Switzerland and eastern France). International journal of earth sciences, 93(2), pp. 207-223. Springer-Verlag 10.1007/s00531-003-0375-2
Pliocene to recent uplift and shortening in the southern Rhinegraben is documented by deformation of Pliocene fluvial gravels, deposited on a nearly planar surface, as well as by progressive deflection and capture of rivers. This deformation is sugge
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0f82c73b2b1c1894eef38c99b36fb102
https://boris.unibe.ch/117510/1/531_2003_Article_375.pdf
https://boris.unibe.ch/117510/1/531_2003_Article_375.pdf
Publikováno v:
Quaternary Science Reviews. 24:2303
Erratum to ‘‘Fault reactivation in brittle-viscous wrench systems—Dynamically scaled analogue models and application to the Rhine–Bresse transfer zone’’ [Quaternary Science Reviews 24 (2005) 365–382] Kamil Ustaszewski , Markus E. Schuma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::52cad9fd6656c38c2067b4516a6dcb6b
https://doi.org/10.1016/j.quascirev.2005.08.001
https://doi.org/10.1016/j.quascirev.2005.08.001
Autor:
Markus E. Schumacher
Publikováno v:
Tectonics. 21:6-1
[1] The evolution of the Cenozoic Upper Rhine Graben was controlled by a repeatedly changing stress field and the reactivation of a complex set of crustal discontinuities that had come into evidence during Permo-Carboniferous times. A comparison of t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::18c0545a1575d465a32b9dcc77a4791d
https://doi.org/10.1029/2001tc900022
https://doi.org/10.1029/2001tc900022