Nature and evolution of fluid inclusions in the Cenozoic Beiya gold deposit, SW China-Reference-Cited by-同舟云学术

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Nature and evolution of fluid inclusions in the Cenozoic Beiya gold deposit, SW China

Published:2018-08 Issue: Volume:161 Page:35-56
ISSN:1367-9120
Container-title:Journal of Asian Earth Sciences
language:en
Short-container-title:Journal of Asian Earth Sciences

Author:

Liu Heqing,Bi Xianwu,Lu Huanzhang,Hu Ruizhong,Lan Tingguang,Wang Xinsong,Huang Mingliang

Funder

Strategic Priority Research Program (B) of Chinese Academy of Sciences

Natural Science Foundation of China

High-level innovative talents training plan of Guizhou province

Key Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference66 articles.

1. Validation of LA-ICP-MS fluid inclusion analysis with synthetic fluid inclusions;Allan;Am. Mineral.,2005

2. The magmatic-hydrothermal evolution of two barren granites: a melt and fluid inclusion study of the Rito del Medio and Cañada Pinabete plutons in northern New Mexico (USA);Audétat;Geochim. Cosmochim. Acta,2003

3. The composition of magmatic-hydrothermal fluids in barren versus mineralized intrusions;Audétat;Econ. Geol.,2008

4. Bakker, R.J., 1997. Clathrates: Computer Programs to Calculate Fluid Inclusion V-X Properties using Clathrate Melting Temperatures. Pergamon Press, Inc.

5. Crystallization conditions (T, P, fO2) from mineral chemistry of Cu- and Au-mineralized alkaline intrusions in the Red River-Jinshajiang alkaline igneous belt, western Yunnan Province, China;Bi;Mineral. Petrol.,2009

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