Zobrazeno 1 - 10
of 24
pro vyhledávání: '"Dmitry Zastrozhnov"'
Autor:
Sverre Planke, Christian Berndt, Carlos A A Zarikian, Ritske S Huismans, Stefan Bünz, Jan Inge Faleide, Nina Lebedeva-Ivanova, Dmitry Zastrozhnov, Expedition Scientists
Continental breakup in the NE Atlantic was associated with mafic magmatism recorded by basalt flows, volcanogenic sediments, magmatic underplates, and intrusive sheet complexes in the nearby sedimentary basins and continental crust. The voluminous ma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ae2700176ef8de610493ff86a5033204
https://doi.org/10.5194/egusphere-egu23-13260
https://doi.org/10.5194/egusphere-egu23-13260
Autor:
Nina Lebedeva-Ivanova, Sverre Planke, John M. Millett, Stefan Bünz, Cornelia M. Binde, Ben Manton, Dmitry Zastrozhnov, Christian Berndt, David W. Jolley, Henk Brinkhuis
Extensive magmatism during the NE Atlantic break-up generated about 6-10 million cubic kilometers of magma in the Paleogene. Magmatic degassing and explosive discharge of thermogenic gases by contact metamorphism is implicated in triggering the Paleo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6a19d77ec832ee3c464884578acc69c2
https://doi.org/10.5194/egusphere-egu23-17396
https://doi.org/10.5194/egusphere-egu23-17396
Autor:
Mansour M. Abdelmalak, Sébastien Gac, Jan Inge Faleide, Grace E. Shephard, Filippos Tsikalas, Stéphane Polteau, Dmitry Zastrozhnov, Trond H. Torsvik
The formation of the NE Atlantic conjugate margins is the result of multiple rifting phases spanning from the Late Paleozoic and culminating in the early Eocene when breakup was accompanied with intense magmatic activity. The pre-breakup configuratio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cdb1c6ab68a1b4d19a4e22722db6b53d
https://doi.org/10.5194/egusphere-egu23-9908
https://doi.org/10.5194/egusphere-egu23-9908
Autor:
Andrey Zastrozhnov, Guzel Danukalova, Eugenija Osipova, Ravil Kurmanov, Sergei Lazarev, Dmitry Zastrozhnov
Publikováno v:
Quaternary International.
Autor:
Mansour M. Abdelmalak, Sébastien Gac, Jan Inge Faleide, Grace E. Shephard, Filippos Tsikalas, Stéphane Polteau, Dmitry Zastrozhnov, Trond H. Torsvik
Publikováno v:
Tectonics
e2022TC007386
e2022TC007386
The formation of the NE Atlantic conjugate margins is the result of multiple rifting phases spanning from the Late Paleozoic and culminating in the early Eocene when breakup was accompanied with intense magmatic activity. The pre-breakup configuratio
Autor:
D. O. Gimranov, Vadim V. Titov, Ravil Kurmanov, Andrey Zastrozhnov, Tatyana Yakovleva, Guzel Danukalova, Oleksandr Kovalchuk, Dmitry Zastrozhnov, Maria A. Zenina, Anatoly Yakovlev, Mikhail Golovachev, Eugenija Osipova
Publikováno v:
Quaternary International. 590:85-121
There are many Middle-Upper Pleistocene outcrop sections in the Lower Volga region (Caspian Lowland, Russia) in between cities of Volgograd and Astrakhan. The present study focuses on the Seroglazovka locality, which is among the most famous key site
Autor:
Ben Manton, Philipp Müller, Adriano Mazzini, Dmitry Zastrozhnov, Dougal A. Jerram, John M. Millett, Daniel W. Schmid, Christian Berndt, Reidun Myklebust, Sverre Planke
Publikováno v:
Marine Geology. 453:106913
Publikováno v:
Proc Natl Acad Sci U S A
Anthropogenic global warming may be accelerated by a positive feedback from the mobilization of methane from thawing Arctic permafrost. There are large uncertainties about the size of carbon stocks and the magnitude of possible methane emissions. Met
Extensional processes can lead to complex crustal configuration depending on the mechanisms of lithospheric thinning and the impact of magmatic additions during rifting and breakup. In this context, we studied the Vøring volcanic passive margin offs
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::be10ded2e286c7afcfe679beaf03187a
http://hdl.handle.net/10852/92678
http://hdl.handle.net/10852/92678
Autor:
Sverre Planke, Dmitry Zastrozhnov, Reidun Myklebust, Jan Inge Faleide, Mohamed Mansour Abdelmalak, Laurent Gernigon
The structure and tectonostratigraphic development of the mid-Norwegian volcanic passive margin have been extensively studied over last 30 years. However, an understanding of its crustal architecture and basin evolution remains incomplete and debated
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fa1d55b95d7c93f1a0fa12160af08bbd
https://doi.org/10.5194/egusphere-egu2020-10558
https://doi.org/10.5194/egusphere-egu2020-10558