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

Volume: 23, Issue: 4, Pages: 1365 - 1377
Published: May 1, 2013
Abstract
null null 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 indicates that high-grade metamorphism occurred at ~ 500 Ma. Evidence from detrital zircons in Paleozoic sediments from the Songliao Block also...
Paper Details
Title
The crustal accretion history and tectonic evolution of the NE China segment of the Central Asian Orogenic Belt
Published Date
May 1, 2013
Volume
23
Issue
4
Pages
1365 - 1377
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