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Complete transition from mantle plume to mantle exhumation on the Central Atlantic Guyana/Suriname margin - Communications Earth & Environment
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Modern data are clarifying tectonic transitions from continents to oceans. The importance of magmatic additions relative to mechanical extension varies between cases and through time based on observations of isolated margins and ridges. Magma poor spreading centers and magma rich continental margins are both well known. Here we present data to document the complete and continuous evolution from a magma rich Central Atlantic margin to a magma-starved ocean floor.
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