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Metamorphic petrology of eclogites at Luotian from the southwestern part of the North Dabie complex zone, central China, was studied. It was found that except for usual eclogitic minerals such as garnet, omphacite and rutile, the eclogites contain allanite and fluor-apatite. Allanites are rich in rare earth elements (REE) and occur as inclusion in garnet, and some of them were partly retrogreted to epidote. Whereas fluor (F)-apatite occurs as inclusion in garnet or in matrix, the former is rich in F (-3 wt%) without any exsolutions and the latter is relatively poor in F (-1 wt%) associated with the oriented pyrrhotite exsolution. In view of occurrence and assemblage of the coexisting minerals with allanite and fluor-apatite in garnet, it is suggested that they formed at peak stage of ultrahigh-pressure (UHP) metamorphism. These results provide new evidence that UHP metamorphism occurred in the eclogites at the Luotian dome.
Sprache
Chinesisch
Identifikatoren
ISSN: 0253-2778
Titel-ID: cdi_proquest_miscellaneous_30080910
Format
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