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• W3088789299 endingPage "104712" @default.
• W3088789299 startingPage "104712" @default.
• W3088789299 abstract "The thermal evolution and crustal nature along the Mozambique rifted margin is investigated using a forward kinematic modelling approach. The numerous plate reconstructions for the breakup of East Gondwana question the crustal nature of the Mozambique margin, especially in the vicinity of the Beira High and the Zambezi depression. Given the few geological and geophysical data available, it is necessary to propose simple but relevant hypotheses to calibrate the margin structure and evolution. Different scenarios were tested to examine the nature of the crust in the Beira High and the Zambezi depression (i.e. continental, oceanic, and mixed). As the margin thermal evolution is related to the crustal architecture and nature, we compared thermal modeling results to well data. Based on these observations, we favour a continental nature for the Beira High and the Zambezi depression. Given the widespread magmatism in the area and the possible variation of volcanic addition along-strike, we consider the presence of underplating in the Zambezi depression." @default.
• W3088789299 created "2020-10-01" @default.
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• W3088789299 date "2021-01-01" @default.
• W3088789299 modified "2023-10-13" @default.
• W3088789299 title "Kinematic modelling of the Mozambique rifted margin and associated thermal histories" @default.
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• W3088789299 doi "https://doi.org/10.1016/j.marpetgeo.2020.104712" @default.
• W3088789299 hasPublicationYear "2021" @default.
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