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Geological Tectonic Evolution and Mineralization of Langshan Orogenic Belt in the Western Part of the Northern Margin of North China Craton
Author(s) -
CHEN Xifeng,
PENG Runmin,
YE Jinhua,
XIANG Yunchuan,
CAI Gang
Publication year - 2014
Publication title -
acta geologica sinica ‐ english edition
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 61
eISSN - 1755-6724
pISSN - 1000-9515
DOI - 10.1111/1755-6724.12376_2
Subject(s) - beijing , china , geological survey , craton , geology , chinese academy of sciences , tectonics , library science , mining engineering , archaeology , geography , seismology , paleontology , computer science
Langshan orogenic belt, located in the western part of the northern margin of the North China Craton(Fig.1), is a well-known Cu-Pb-Zn polymetallic ore belt and hosts Dongshenmiao, Tanyaokou, Huogeqi and Jiashengpan large-super large Zn-Pb-Cu-Fe sulfide deposits. Studies from the regional geological and mineral resources characteristics, the geological features and genesis of ore deposits (Zhai et al.,2004;Peng et al.,2007), the orecontrolling synchronous faults(Peng et al.,2004), synsedimentary volcanic activities(Peng et al.,2007a), the regional geological tectonic evolution(Peng et al.,2007b), the diagenesis(Peng et al.,2010) and the mineralization and its genesis(Peng et al.,2007c;Zhong et al.,2012,2013 ) have enhanced our present understanding of the geological tectonic evolution and mineralization of Langshan orogenic belt in recent years. But, the geological tectonic evolution and mineralization of Langshan orogenic belt is still an important problem which should be deeply studied.