Zobrazeno 1 - 3
of 3
pro vyhledávání: '"Vanessa Dyja-Person"'
Autor:
Vanessa Dyja-Person, Laura Créon, Jacques Pironon, Isabella Pignatelli, Gaston Giuliani, Svetlana Pentelei, Nicolas Beaudoin, Vladimir S. Balistky, Hélène Legros, Antonin Richard, Jérôme Sterpenich, Christophe Morlot
Publikováno v:
Chemical Geology
Chemical Geology, Elsevier, 2019, 508, pp.3-14. ⟨10.1016/j.chemgeo.2018.06.012⟩
Chemical Geology, 2019, 508, pp.3-14. ⟨10.1016/j.chemgeo.2018.06.012⟩
Chemical Geology, Elsevier, 2019, 508, pp.3-14. ⟨10.1016/j.chemgeo.2018.06.012⟩
Chemical Geology, 2019, 508, pp.3-14. ⟨10.1016/j.chemgeo.2018.06.012⟩
Fluid and melt inclusions are tiny pockets of fluid and melt trapped in natural and synthetic minerals. Characterizing the 3D distribution of fluid and melt inclusions within minerals, their shape and the volume fraction of their different phases is
Publikováno v:
Marine and Petroleum Geology
Marine and Petroleum Geology, Elsevier, 2020, 114, pp.104193. ⟨10.1016/j.marpetgeo.2019.104193⟩
Marine and Petroleum Geology, Elsevier, 2020, 114, pp.104193. ⟨10.1016/j.marpetgeo.2019.104193⟩
Micron-sized fluid inclusions within quartz grains from Late Cretaceous sandstones, recovered from drill cuttings from four wells in the Great Australian Bight, contain palaeo-fluids such as brine, black oil, light oil, gas condensate, and N2 and CO2
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ac63ace7c5d9e7b3d01de7b8f8b043cc
https://hal.univ-lorraine.fr/hal-02423424
https://hal.univ-lorraine.fr/hal-02423424
Autor:
Alexandre Tarantola, Luc Siebenaller, Marie-Christine Boiron, Michel Cathelineau, Christian Hibsch, Philippe Boulvais, Antonin Richard, Vanessa Dyja-Person
Publikováno v:
Tectonophysics
Tectonophysics, Elsevier, 2018, 727, pp.56-72. ⟨10.1016/j.tecto.2018.02.001⟩
Tectonophysics, 2018, 727, pp.56-72. ⟨10.1016/j.tecto.2018.02.001⟩
Tectonophysics, Elsevier, 2018, 727, pp.56-72. ⟨10.1016/j.tecto.2018.02.001⟩
Tectonophysics, 2018, 727, pp.56-72. ⟨10.1016/j.tecto.2018.02.001⟩
International audience; The ductile-brittle transition zone in extensional regimes can play the role of a hydrogeological barrier. Quartz veins developed within an orthogneiss body located in the detachment footwall of a Metamorphic Core Complex (MCC
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::af8264af1ecca90c77c7a67403f03408
https://hal-insu.archives-ouvertes.fr/insu-01713218
https://hal-insu.archives-ouvertes.fr/insu-01713218