Carbon recycled into deep Earth: Evidence from dolomite dissociation in subduction-zone rocks Journal Article uri icon

DCO ID 11121/6561-6533-9175-9859-CC

in language

  • eng

year of publication

  • 2002


  • {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


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