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Fluid Inclusion Study on the Talate Pb‐Zn Deposit, Southern Altay, China
Author(s) -
ZHANG Hui,
XU Jiuhua,
CHENG Xihui,
BIAN Chunjing
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 - 10.1111/1755-6724.12379_66
Subject(s) - beijing , china , library science , resource (disambiguation) , chinese academy of sciences , inclusion (mineral) , science and engineering , citation , zhàng , engineering , history , sociology , computer science , social science , engineering ethics , archaeology , computer network
The Talate Pb-Zn deposit, located 20 km southeast to Altai (Fig. 1), Xinjiang, occurs in the Devonian Kelan vocanic-sedmentary basin, which strikes NW-SE along the south margin of Altay Mountains. The Talate Pb-Zn deposit was subjected to the regional metamorphism and metamorphic overprint, and the genesis of mineral deposit is in dispute as yet, such as skarn type (Li et al., 2012), VMS type (Yuan et al., 2011) and exhalation sedimentation-reformation type (Tiras., 2009). Here we present the result of fluid inclusions in the the Talate PbZn deposit and new insights of the ore genesis.