CO2-rich fluid inclusions with chalcopyrite daughter mineral from the Fenghuangshan Cu–Fe–Au deposit, China: implications for metal transport in vapor-Reference-Cited by-同舟云学术

CO2-rich fluid inclusions with chalcopyrite daughter mineral from the Fenghuangshan Cu–Fe–Au deposit, China: implications for metal transport in vapor

Published:2007-01-04 Issue:3 Volume:42 Page:293-299
ISSN:0026-4598
Container-title:Mineralium Deposita
language:en
Short-container-title:Miner Deposita

Author:

Lai Jianqing,Chi Guoxiang

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Link

http://link.springer.com/content/pdf/10.1007/s00126-006-0109-z.pdf

Reference16 articles.

1. Baker T (2002) Emplacement depth and carbon dioxide-rich fluid inclusions in intrusion-related gold deposits. Econ Geol 97:1111–1118

2. Barnes HL (1979) Solubility of ore minerals. In: Barnes HL (ed) Geochemistry of hydrothermal ore deposits. Wiley, pp 404–460

3. Brown PE (1989) FLINCOR: a microcomputer program for the reduction and investigation of fluid inclusion data. Am Mineral 74:1390–1393

4. Chang Y, Liu X, Wu Y (1991) The copper–iron belt of the lower and middle reaches of the Changjiang river. Geological Publishing House, Beijing, p 379 (in Chinese with English abstract)

5. Chi G, Williams-Jones AE, Dube B, Williamson K (2005) Carbonic vapor-dominated fluid systems in orogenic-type Au deposits. Geochim Cosmochim Acta 69:A738

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