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Published in 2020 at "American Mineralogist"
DOI: 10.2138/am-2020-7403
Abstract: Abstract Sedimentary diapirs can be relaminated to the base of the lithosphere during slab subduction, where they can interact with the ambient lithospheric mantle to form variably metasomatized zones. Here, high-pressure experiments in sediment-harzburgite systems…
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Keywords:
lithospheric mantle;
subduction zones;
sediment;
k2o na2o ... See more keywords