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- W2316282779 abstract "Geological and geophysical evidences appear not to support the current axiom for vertical hydrocarbon migration through listric faults and salt windows in the Brazilian Salt Basins. Restrictions imposed on the theory in which such features would act as principal routes for petroleum relies on: 1) dry wells drilled in the specifications of such model; 2) listric faults are closely associated to salt movement, therefore its activity takes place only during a limited period of time, not always coincident with the petroleum expulsion time; 3) the non plasticity of other salt species, but halite, harming the sealing character of the “salt window”. The Transtensional Faulting Incidence Zone (in Portuguese, ZIFTT) is proposed as the right model to explain most of the vertical hydrocarbon migration pathways that are present in the Brazilian Salt Basins. The model is associated to localized stress in the continental margin due to the South Atlantic opening which is still active as can be verified by low magnitude earthquakes. Its role encompasses not only hydrocarbon pathways but distribution of dykes and sills in volcanic basins, incised valleys (plataformal environments) and salt diapirism." @default.
- W2316282779 created "2016-06-24" @default.
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- W2316282779 date "2009-01-01" @default.
- W2316282779 modified "2023-09-25" @default.
- W2316282779 title "The Death Of Listric Faults And Salt Windows As Hydrocarbon Migration Pathways: A Modern Insight About The Ziftt Role In The Petroleum System Dynamics" @default.
- W2316282779 doi "https://doi.org/10.3997/2214-4609-pdb.195.1845_evt_6year_2009" @default.
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