Coupling crustal-scale rift architecture with rifted margin salt tectonics: a geodynamic modelling approach Many rifted passive margins are associated with widespread and thick evaporite (i.e., salt) deposits, and pronounced syn-and post-rift salt tectonics. The majority and largest salt basins known-to-date …
Large Igneous Provinces, hydrovolcanism and paleoenvironments/paleohydrology: lessons from the Paraná Basin in South Brazil In many continental flood basalt provinces (CFBPs), primary mafic volcaniclastic deposits have been shown to be significant counterparts of better-known effusive (lava flow) facies, a notion …
Quaternary basin fill and evolution of the North Sea Basin: A synthesis of sequence stratigraphy and basin modeling techniques by Baig, Irfan; Faleide, Jan Inge; Aagaard, Per; Chuahan, Teena; Hjelstuen, Berit Oline Blihovde & Sejrup, Hans Petter
Preliminary results from IODP Expedition 396 – Mid Norwegian Continental Margin Magmatism
Potential temperature and depth-dependent extension control melt volume at Atlantic volcanic margins Breakup volcanism along rifted passive margins is highly variable in time and space. The factors controlling magmatic activity during continental rifting and breakup are not resolved and controversial. …
Topography during Pangea Breakup - Case of the South Atlantic Central Segment - 2-D thermo-mechanical modelling and implications for salt basin formation In this study we use observations from the central South Atlantic conjugate margins to constrain the structural style …
Tracing tectonically active faults with the smallest earthquakes: sensitive detection of the 2021 Bitdalsvatnet earthquake swarm
Form And Fill of A Transtensional Lacustrine Rift Basin: Lower Talangakar Formation, Jatibarang Subbasin, Offshore NW Java, Indonesia
Magmatism at Atlantic volcanic rifted margins: When do we need mantle plumes? Breakup volcanism along rifted passive margins is highly variable in time and space. The factors controlling magmatic activity during continental rifting and breakup are not resolved and controversial. …
Transition from Aegean back-arc extension to Corinth rifting. Miocene to Pleistocene interacting extensional regimes of the Northern Peloponnese. Vincent Wicker1, Mary Ford1, Robert Gawthorpe2, Haralambos Kranis3, Emmanuel Skourtsos3, Pierre Bouilhol1, Martin Muravchik2, Natacha Fabregas2, Kévin Beaufumé4, Hugo Beldame5 1 - …