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Building An Independent Pb‐Zn Mineralization System Related to Magmatism: A Case Study of Narusongduo Pb‐Zn Deposit in Tibet
Author(s) -
LIU Yingchao,
YANG Zhusen,
HOU Zengqian,
JI Xianhua,
MENG Xiangjin
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 - 10.1111/1755-6724.12377_10
Subject(s) - chinese academy of sciences , beijing , geological survey , geology , library science , china , geochemistry , archaeology , geography , paleontology , computer science
Five Pb-Zn mineralization types can occur in the compression environment in the world, which include porphyry Pb-Zn mineralization(Zuo et al., 2008), crytoexplosive breccia-type Pb-Zn mineralization(Zhang et al., 2012), Skarn-type Pb-Zn mineralization(Meinert et al., 2005), Manto-type Pb-Zn mineralization(Bonsall et al., 2011) and Vein-type Pb-Zn mineralization(Voudouris et al., 2008). However, nobody has done some research to judge whether these five types Pb-Zn mineralization can form in an independent Pb-Zn mineralization system. A Pb -Zn mineralization belt formed in the northern margin of the Gangdese metallogenic belt in the Tibet plateau(Tang et al., 2012). The Pb-Zn reserves are huge and there many types of Pb-Zn mineralization related to magmatism have been found, which make these Pb-Zn deposits be good examples to answer scientific question above. Narusongduo Pb-Zn deposit, located in the middle-west of the Pb-Zn mineralization belt in Gangdese, is a super large LIU Yingchao, YANG Zhusen, HOU Zengqian, JI Xianhua and MENG Xiangjin, 2014. Building an Independent Pb-Zn Mineralization System Related to Magmatism: A Case Study of Narusongduo Pb-Zn Deposit in Tibet. Acta Geologica Sinica (English Edition), 88(supp. 2): 916-918.