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Metallogenesis of the Ertix gold belt, Xinjiang and its relationship to Central Asia-type orogenesis
Authors:CHEN Huayong  CHEN Yanjing  Liu Yulin
Institution:1. Department of Geology, Peking University, Beijing 100871, China
2. The Open Laboratory of Metamorphic Geology of Changchun University of Science and Technology, Changchun 130061, China
Abstract:The Ertix gold belt is located on the boundary of the Kalatongke arc and the Kelan back-arc basin of D-C1. Most scholars used to interpret the formation and distribution of the gold deposits in the Ertix tectonic belt in terms of the petrogenic and metallogenic models for active continental margins. However, enormous data of isotopic dating and geologic research show that the mineralization was obviously later than the oceanic subduction, whereas exactly simultaneous with the collisional orogenesis during C2-P, especially at the transition stage from collisional compression to extension. Based on study of metallogenic time, tectonic background, ore geology, ore fluid nature, ore material source, etc., we reveal that all the gold deposits possess the character of orogenic deposits formed in collisional orogenic system, and that their ore-forming materials mainly have derived from the stratigraphic terranes south to individual deposits. Accordingly, the theoretical tectonic model for collisional metallogenesis and petrogenesis is employed to explain the formation of the Ertix gold belt and to determine the gold exploration directions.
Keywords:Ertix gold belt  late Carboniferous-early Permian  petrogenic and metallogenic model for collisional orogenesis
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