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

Publication
Journal of the Geological Society
Published
5 September 2022
Authors
James Pindell | Teunis Heyn
DOI
https://doi.org/10.1144/jgs2021-095
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lyellcollection.org
geoscienceworld.org
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https://doi.org/10.1144/jgs2021-095
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