Zobrazeno 1 - 10
of 62
pro vyhledávání: '"H.J. Neugebauer"'
Autor:
H.J. Neugebauer, T. Spohn
Publikováno v:
Tectonophysics. 50:275-305
Elongated sedimentary basins are found along continental margins of the Atlantictype. The evolution of these basins is seen to be related to continental break-up and the associated fault system, cooling of the spreading lithosphere, sedimentary loadi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::31352f0bad29fc59336324ff68a3b3d8
https://doi.org/10.1016/0040-1951(78)90139-7
https://doi.org/10.1016/0040-1951(78)90139-7
Autor:
B. Braner, H.J. Neugebauer
Publikováno v:
Tectonophysics. 46:1-20
Rift development which is recorded in apparent structural features and the derived rift kinematics indicate that the graben proper of the Upper Rhine rift region is evidently confined to the upper part of the crust. The graben proper follows the cres
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a6fb135795a0e3fff186118d639235c6
https://doi.org/10.1016/0040-1951(78)90102-6
https://doi.org/10.1016/0040-1951(78)90102-6
Publikováno v:
Physics of the Earth and Planetary Interiors. 36:260-275
Large dip slip earthquakes contribute to the large amount of the relative motion between lithospheric plates. Immediately after an earthquake, displacements correspond to those of a purely elastic Earth while subsequent deviatoric stresses are relaxe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5bfd23fc95f6efc939d39efa9cc4a1e8
https://doi.org/10.1016/0031-9201(84)90050-5
https://doi.org/10.1016/0031-9201(84)90050-5
Autor:
T. Spohn, H.J. Neugebauer
Publikováno v:
Tectonophysics. 50:387-412
The transformation of metastable basalt to stable garnet granulite or eclogite is assumed to be a possible mechanism involved in the development of sedimentary basins adjacent to passive continental margins. It might play a significant role for both
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e2cb26b4fb399ac323ae44dd6ba2bef5
https://doi.org/10.1016/0040-1951(78)90144-0
https://doi.org/10.1016/0040-1951(78)90144-0
Autor:
W.-D. Woidt, H.J. Neugebauer
Publikováno v:
Physics of the Earth and Planetary Interiors. 21:176-180
Density instabilities are often associated with large deformations in rocks, and result in diapiric structures of different shape and dimension. The Finite Element model presented here is able to follow the large deformations in a simple two-layer mo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::85740d7a075d454b276f755aea9edb1b
https://doi.org/10.1016/0031-9201(80)90068-0
https://doi.org/10.1016/0031-9201(80)90068-0
Autor:
H.J. Neugebauer
Publikováno v:
Tectonophysics. 45:159-186
Continental rifts are observed to be associated with crustal doming. This is well-established by both the elevation of structural boundary layers as well as that of the crustmantle boundary. Rift regions show typical fault systems corresponding to th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c09e9791c99e31a8215d490aebdbb24d
https://doi.org/10.1016/0040-1951(78)90005-7
https://doi.org/10.1016/0040-1951(78)90005-7
Autor:
Rudolf Hüttel, H.J. Neugebauer
Publikováno v:
Tetrahedron Letters. 5:3541-3544
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::37a106902083990e386f5f15c6df43e6
https://doi.org/10.1016/0040-4039(64)83153-1
https://doi.org/10.1016/0040-4039(64)83153-1
Autor:
H.J. Neugebauer, P. Olson
Publikováno v:
Physics of the Earth and Planetary Interiors. 36:iii
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::66b907212bceffedd583d77534063aa2
https://doi.org/10.1016/0031-9201(84)90045-1
https://doi.org/10.1016/0031-9201(84)90045-1
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