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Archean crustal evolution of the northern North China CratonThe Archean granultie facies rocks of the North China (Sino-Korean) Craton mostly occur inside the northern boundary forming a unique and spectacular granulite belt trending roughly E-W from eastern Hebei, North China in the east to Mt. Daqinchan, western Inner Mongolia in the west, ranging about 1,000 km long. Over the years in the middle portion of this Archean high-grade metamorphic belt a stratigraphic unconformity between the khondalite rock assemblage and the medium in composition granulite assemblage in Datong-Xinghe area is determined. The geological structural properties of the North China Craton are discussed.
Document ID
19880020851
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Qian, Xianglin
(Peking Univ.)
Chen, Yaping
(Peking Univ.)
Liu, Jinzhong
(Peking Univ.)
Date Acquired
September 5, 2013
Publication Date
January 1, 1988
Publication Information
Publication: Lunar and Planetary Inst., Workshop on the Growth of Continental Crust
Subject Category
Geophysics
Accession Number
88N30235
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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