Zobrazeno 1 - 10
of 52
pro vyhledávání: '"Laurent Gernigon"'
Autor:
Laurent Gernigon, Claudia Haase, Sofie Gradmann, Marie-Andrée Dumais, Trond Slagstad, Frode Ofstad, Aziz Nasuti, Marco Bronner
We integrated high-resolution aeromagnetic data and 2D/3D seismic data from the Norwegian Southwestern Barents Sea. The main objective is to address the long-standing question on the role of pre-existing basement structures in controlling strain acco
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::372a0cceb32eb45a8cd0080d7ba49127
https://doi.org/10.5194/egusphere-egu23-12301
https://doi.org/10.5194/egusphere-egu23-12301
The interest for the polar regions and complex continental margins and ocean has increased during the last few decades. New technologies allow to conduct research in this hostile environment, permitting to investigate the tectonic and geodynamic hist
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9666710e03b8e491ab6bc9d9360228d6
https://doi.org/10.5194/egusphere-egu23-6339
https://doi.org/10.5194/egusphere-egu23-6339
Autor:
Shihao Hao, Lianfu Mei, Xiong Pang, Laurent Gernigon, Douglas Paton, Jinyun Zheng, Qing Ye, Zhichao Zhou, Ye Zhong
Publikováno v:
GSA Bulletin.
Continental passive margins are commonly classified into volcanic (or magma-rich) and non-volcanic (or magma-poor) types based on the magmatic budget. It is difficult, however, to use either of these models to define the northern margin of the South
The true partitioning between continental and oceanic lithosphere in oceans is unclear. According to early models, oceanic-type accretion generates pairs of linear magnetic anomalies, which are indicators of oceanic lithosphere and can be used as iso
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::57a9d092d35f6fd60889f4b961e73760
https://doi.org/10.1130/2021.2553(06)
https://doi.org/10.1130/2021.2553(06)
Autor:
Gillian Foulger, Anatoly Nikishin, Elizaveta Rodina, Ksenia Startseva, Laurent Gernigon, Laurent Geoffroy, Jordan Phethean, Andrey Chernykh
The disintegration of Pangea north of the Charlie Gibbs fracture zone led to the formation of the NE Atlantic and Arctic Oceans. Both these oceans are exceptionally complex in terms of diversity of the structures they contain and the sequence of even
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ef2477e2f3a79a4461c51745c79b2848
https://doi.org/10.5194/egusphere-egu22-6253
https://doi.org/10.5194/egusphere-egu22-6253
Publikováno v:
Geophysical Journal International
SUMMARY Insights into the spreading evolution of the Knipovich Ridge and development of the Fram Strait are revealed from a recent aeromagnetic survey. As an ultraslow spreading ridge in an oblique system located between the Svalbard–Barents Sea an
Publikováno v:
Geophysical journal international, 2020, Vol.222(3), pp.1471-1479 [Peer Reviewed Journal]
SUMMARYWe propose a tectonic interpretation for the outer-SDRs (SDRs: Seaward-Dipping Reflectors) and Pannikar central ridge in the aborted Laxmi Basin west of India from wide-angle seismic reflection data. The outer-SDRs comprise syn-tectonic extrus
Autor:
John M. Millett, Ben M. Manton, Dmitrii Zastrozhnov, Sverre Planke, Dwarika Maharjan, Benjamin Bellwald, Laurent Gernigon, Jan Inge Faleide, David W. Jolley, Faye Walker, Mansour M. Abdelmalak, Dougal A. Jerram, Reidun Myklebust, Bent E. Kjølhamar, Jennifer Halliday, Alex Birch-Hawkins
Publikováno v:
Geological Society, London, Special Publications. 495:99-138
The NE Atlantic volcanic rifted margins include vast underexplored basin areas neighbouring mature petroleum-producing regions. We appraise the cross-border prospectivity of the outer and central Faroe–Shetland, Møre and southern Vøring basins an
Publikováno v:
Tectonophysics. 849:229734
Autor:
Odleiv Olesen, Mohamed Mansour Abdelmalak, Jan Inge Faleide, Dmitrii Zastrozhnov, Dwarika Maharjan, Ben Manton, Reidun Myklebust, Laurent Gernigon, Sverre Planke
Publikováno v:
Norwegian Journal of Geology.
A new generation of long-offset 2D seismic reflection lines, 2D-cubed seismic volumes, extensive 3D seismic surveys, high-resolution potential field data, and exploration wells has resulted in improved geological mapping of the Mid–Norwegian contin