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Analysis of Gold Mineralization in Tectonic‐Magmatic Environment: A Case Study of Ertix Gold Metallogenic Zone
Author(s) -
Xiaoqiang LÜ,
GUO Naxin,
LI Chunxia
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 - 10.1111/1755-6724.12385_27
Subject(s) - beijing , chinese academy of sciences , geological survey , china , geology , mineralization (soil science) , tectonics , geochemistry , library science , citation , mining engineering , political science , geography , archaeology , computer science , seismology , paleontology , soil science , soil water
Ertix gold metallogenic belt is located in transitional zone of Siberia and Kazakhstan-Junggar plates with advantageous geological setting for mineralization. A number of middle-large scale gold deposits are distributed in this area. Gold deposits occurring in the Paleozoic volcanic-clastic rocks, mostly were formed during the Late Carboniferous-Permian period, namely strike-slip stage after collision orogeny and transformation period from strike-slip mechanism to extensional one(Shen et al., 2007; Yan et al., 2006).