Petrological evidence for isobaric cooling of ultrahigh-temperature pelitic granulites from the Khondalite Belt, North China Craton

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Petrological evidence for isobaric cooling of ultrahigh-temperature pelitic granulites from the Khondalite Belt, North China Craton

© 2015, Science China Press and Springer-Verlag Berlin Heidelberg. The ultrahigh-temperature (UHT) pelitic granulites from the Khondalite Belt, North China Craton (NCC), contain ilmenite in the matrix, which has been partially replaced by rutile. Based on this observation and the growth of biotite b...

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Bibliographic Details
Main Authors:	Gou, Long-Long, Zhang, C., Wang, Q.
Format:	Journal Article
Published:	2015
Online Access:	http://hdl.handle.net/20.500.11937/38641

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