Metallogenesis and fluid evolution of the Devonian porphyry Cu deposits in the Central Asian Orogenic Belt: the Xiaotuergen example

Author:

Geng Xinxia1,Yang Fuquan1,Yang Chengdong1ORCID,Qin Jihua2,Wen Chaoquan2ORCID

Affiliation:

1. Key Laboratory of Metallogeny and Mineral Assessment, Ministry of Natural Resources, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, PR China

2. No. 4 Geological Team of the Xinjiang Bureau of Geology and Mineral Exploration and Development, Altay, Xinjiang, PR China

Funder

Central-level Welfare Research Institute Fundamental Research Funds for Special Projects

National Key R&D Program of China

National Natural Science Foundation of China Program

Publisher

Informa UK Limited

Subject

Geology

Reference106 articles.

1. Revised equation and table for determining the freezing point depression of H2O-Nacl solutions

2. Geochronology and geochemistry of the intrusive suite associated with the Khatsavch porphyry Cu-Au (Mo) deposit, South Mongolia

3. Burruss, R.C., 1981, Analysis of phase equilibria in C–O–H–S fluid inclusions, In: Hollister, L.S., and Crawford, M.L. (Eds.), Short course in fluid inclusions: applications to petrology. Calgary, Mineralogical Association of Canada, p. 39–74.

4. Stable isotope (S, O, H and C) studies of the phyllic and potassic–phyllic alteration zones of the porphyry copper deposit at Sungun, East Azarbaidjan, Iran

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