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

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

volume

  • 30

issue

  • 10