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Compositional Characteristics and Sulfur Isotope of Pyrites in the Zhibo Iron Deposit, Western Tianshan Mountain, NW China
Author(s) -
WANG Zhihua,
ZHANG Zhenliang,
DONG Fuchen,
GAO Yongwei,
TAN Wenjuan
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 - 10.1111/1755-6724.12384_15
Subject(s) - magmatism , geology , geochemistry , geological survey , china , archaeology , geography , paleontology , tectonics
Western Tianshan orogenic belt is a late Paleozoic composite orogenic belt and an important part of the Central Asian metallogenic domain, which experienced a complicated deformation, and several period of subduction, collision and continental superimposed orogeny (Windley et al., 1990; Allen et al., 1992; Xiao et al., 2009). Zhibo iron ore deposit is located in the eastern section of the Awulale metallogenic belt, and tectonic location belongs to the Yili Carboniferous-Permian rift. The region exposes Proterozoic, Silurian, Devonian, Carboniferous, Permian, Triassic, Jurassic and Quaternary in ascending order. Among them the Carboniferous Dahalajunshan Formation is dominant.

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