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Carbon recycled into deep earth: Evidence from dolomite dissociation in subduction-zone rocks: Comment and reply

Hermann, Joerg


The dolomite-dissociation textures documented here in rocks from the Kokchetav ultrahigh-pressure massif suggest that the experimentally expected dolomite dissociation happened in the subducted slabs represented by these rocks. Two reactions, magnesite =

CollectionsANU Research Publications
Date published: 2003
Type: Journal article
Source: Geology
DOI: 10.1130/0091-7613(2002)030<0947:CRIDEE>2.0.CO;2


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