Ocean-continent boundary off the Iberian margin: A serpentinite diapir west of the Galicia Bank

Physics

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Scientific paper

A serpentinite diapir made of altered plagioclase-bearing lherzolites,
has been emplaced west of the Galicia Bank at the boundary between
oceanic crust and the probable thinned continental crust, that underlies
the Iberian margin.

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