jgs2021-095_si_001.pdf (17.57 MB)

Dynamo-thermal subsidence and sag–salt section deposition as magma-rich rifted margins move off plume centres along incipient lines of breakup

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posted on 2022-04-21, 11:42 authored by James Pindell, Teunis Heyn

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Journal of the Geological Society

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Geology not elsewhere classified

Keywords

breakup supplementary material thermal subsidence Geology

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