Ore-forming Fluid Characteristics of the Saishitang Cu-polymetallic Deposit in Qinghai Province, China
Author:
Affiliation:
1. Key Laboratory of Metallogenic Prediction of Nonferrous Metals; Ministry of Education, Central South University; Changsha 410083 China
2. School of Geosciences and Info-Physics; Central South University; Changsha 410083 China
Publisher
Wiley
Subject
Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/1755-6724.12442/fullpdf
Reference64 articles.
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2. Mixed CH4-CO2 fluid inclusions in quartz from the South Wales Coalfield as suiTable natural calibration standards for microthermometry and Raman spectroscopy;Beeskow;Chemical Geology,2005
3. Bodnar , R.J. 1995 Fluid inclusion evidence for a magmatic source for metals in porphyry copper deposits. THOMPSON J FH. Magmas, Fluids, and Ore Deposits Mineralogical Association of Canada Short Course Series, 23. Mineralogical Association of Canada 139 152
4. Synthetic fluid inclusions: XII. The system H2O-NaCl. Experimental determination of the halite liquidus and isochores for a 40 wt% NaCl solution;Bodnar;Geochimica et Cosmochimica Acta,1994
5. FLINCOR: A microcomputer program for the reduction and investigation of fluid inclusion data;Brown;American Mineralogist,1989
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1. Geosciences in Central South University: A state-of-the-art review;Journal of Central South University;2020-04
2. A New Zincian Greenockite Occurrence in the Saishitang Cu Skarn Deposit, Qinghai Province, Northwest China;Minerals;2017-07-28
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