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

Hermann, Joerg

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

Date

2003

Authors

Hermann, Joerg

Publisher

Geological Society of America Inc

Abstract

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 =