Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Gwenn Péron-Pinvidic"'
Autor:
John B. Naliboff, Susanne J. H. Buiter, Gwenn Péron-Pinvidic, Per Terje Osmundsen, Joya Tetreault
Publikováno v:
Nature Communications, Vol 8, Iss 1, Pp 1-9 (2017)
Continental rifting and break up processes are poorly constrained in the early stages. Here, the authors using high-resolution numerical simulations to show how early formed faults in continental extension can then control subsequent structure evolut
Externí odkaz:
https://doaj.org/article/539c8738d76d4011a63746499b2548c6
Publikováno v:
Basin Research.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::14ff4740a02b57ff42653d4c8069f05f
https://doi.org/10.1111/bre.12775
https://doi.org/10.1111/bre.12775
Within rifted margins, the necking domain corresponds to the area where drastic reduction in basement thickness leads the crust to attain a wedge-shape. The crustal thinning occurs along detachment fault systems typically recording displacements in t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ea65970aa8982c63c26fd7adb96053b9
https://doi.org/10.5194/egusphere-egu22-8003
https://doi.org/10.5194/egusphere-egu22-8003
Extensional detachment faults, core complexes and supradetachment basins play major roles in the evolution of 3D rifted margin architecture. The successive incision of basement from early to late stages in the margin evolution is rarely explained in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0b25066d8b194a56615d18b92b37e73f
https://doi.org/10.5194/egusphere-egu22-7480
https://doi.org/10.5194/egusphere-egu22-7480
Detachment fault systems recording displacements in the order of 10s to 100s of km remain poorly understood compared to smaller scale normal faults. The evolutionary models developed for the growth and interaction of Andersonian-type faults are not f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::795565ec7f6a990d4e7fc4bef162bc21
https://doi.org/10.5194/egusphere-egu21-9481
https://doi.org/10.5194/egusphere-egu21-9481
Autor:
Gwenn Peron-Pinvidic
Rifted margins mark the transition between continents and oceans, which are the two first-order types of land masses on Earth. Rifted margins contribute to our understanding of lithospheric extensional processes and are studied by various disciplines
Autor:
Gwenn Peron-Pinvidic
Rifted margins mark the transition between continents and oceans, which are the two first-order types of land masses on Earth. Rifted margins contribute to our understanding of lithospheric extensional processes and are studied by various disciplines
Publikováno v:
Petroleum Geoscience
Petroleum Geoscience, Geological Society, 2010, 16, pp.189-197
Petroleum Geoscience, Geological Society, 2010, 16, pp.189-197
The conjunction of high-quality seismic surveys, deep sea drilling, and progress in numerical modelling has changed the way of thinking about how continents rift and oceans form. In particular the discovery of exhumed continental mantle and hyper-ext
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::000dae4c367bf4af4d99fc19c67fc141
https://doi.org/10.1144/1354-079309-903
https://doi.org/10.1144/1354-079309-903
Publikováno v:
Geological Society, London, Special Publications. 306:169-183
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4f1ca427e088f0d65f7a56abceb61970
https://doi.org/10.1144/sp306.8
https://doi.org/10.1144/sp306.8
Autor:
Gianreto Manatschal, Timothy A. Minshull, Othmar Müntener, Gwenn Péron-Pinvidic, Luc L. Lavier
Publikováno v:
Geological Society, London, Special Publications. 282:291-324
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2213c3d4cb854dd1496ff9de4f9dd703
https://doi.org/10.1144/sp282.14
https://doi.org/10.1144/sp282.14