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Published in 2019 at "Marine and Petroleum Geology"
DOI: 10.1016/j.marpetgeo.2019.04.003
Abstract: Abstract Continental extension may, or may not, be coeval with significant mantle melting, leading to the formation of distinct types of passive margins (respectively magma-poor or volcanic), with distinct crustal structures. Especially in inter-cratonic mobile…
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Keywords:
magmatic ocean;
extension;
ocean continent;
continent transitions ... See more keywords