Geological and C–O–S–Pb–Sr isotopic constraints on the origin of the Qingshan carbonate-hosted Pb–Zn deposit, Southwest China-Reference-Cited by-同舟云学术

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Geological and C–O–S–Pb–Sr isotopic constraints on the origin of the Qingshan carbonate-hosted Pb–Zn deposit, Southwest China

Published:2013-02-05 Issue:7 Volume:55 Page:904-916
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Zhou Jia-Xi¹,Huang Zhi-Long¹,Gao Jian-Guo²,Yan Zai-Fei¹

Affiliation:

1. a State Key Laboratory of Ore Deposit Geochemistry , Institute of Geochemistry, Chinese Academy of Sciences , Guiyang , 550002 , China

2. b Faculty of Land Resource Engineering, Kunming University of Science and Technology , Kunming , 650093 , China

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2013.767496

Reference65 articles.

1. Sulfur Isotope Evidence for Thermochemical Reduction of Dissolved Sulfate in Mississippi Valley-Type Zinc-Lead Mineralization, Bongara Area, Northern Peru

2. A new variable dispersion double-focusing plasma mass spectrometer with performance illustrated for Pb isotopes

3. Precise lead isotope fingerprinting of hydrothermal activity associated with Ordovician to Carboniferous metallogenic events in the Lachlan fold belt of New South Wales

4. Sulphur isotope variations in the mantle from ion microprobe analyses of micro-sulphide inclusions

5. Chen, H.S. and Ran, C.Y. 1992.Isotope geochemistry of copper deposit in Kangdian area, 1–25. Beijing: Geological Publishing House, p. Chinese

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