GEOCHEMISTRY OF ULTRAMAFIC ROCKS FROM THE ULTRAHIGH-PRESSURE METAMORPHIC KIMI COMPLEX IN EAST RHODOPE (NE. GREECE)
Keyword(s):
In the ultrahigh-pressure metamorphic Kimi Complex garnet-spinel metaperidotites with layers of clinopyroxenites occur. A detailed geochemical investigation using major-trace element relations and major-element modelling indicates that the peridotites represent mantle residues originated after variable melt extraction, along an adiabatic path starting from high- to ultrahigh-pressures. The clinopyroxenites represent HP clinopyroxene-rich cumulates probably formed within the garnet and/or Cr-spinel peridotite stability field.
1987 ◽
Vol 51
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pp. 183-202
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2005 ◽
Vol 42
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pp. 1815-1828
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pp. 1818-1834
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1967 ◽
Vol 66
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pp. 419-444
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1997 ◽
Vol 61
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pp. 257-269
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2013 ◽
Vol 2
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pp. 102-115
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