The crustal accretion history and tectonic evolution of the NE China segment of the Central Asian Orogenic Belt

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The crustal accretion history and tectonic evolution of the NE China segment of the Central Asian Orogenic Belt

The basement rocks in parts of NE China constitute a khondalitic sequence of sillimanite- and garnet-bearing gneisses, hornblende–plagioclase gneiss and various felsic paragneisses. Zircon U–Pb dating of garnet–sillimanite gneiss samples from the Erguna, Xing'an, Jiamusi and Khanka blocks indic...

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Bibliographic Details
Main Authors:	Zhou, J., Wilde, Simon
Format:	Journal Article
Published:	Elsevier Science BV 2013
Subjects:	Combined NE China plates NE China Khondalitic Belt Solonker–Xar Moron–Changchun suture zone Pacific plate subduction Central Asian Orogenic Belt
Online Access:	http://hdl.handle.net/20.500.11937/24070

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