Using elemental and boron isotopic compositions of tourmaline to trace fluid evolutions of IOCG systems: The worldclass Dahongshan Fe Cu deposit in SW China-Reference-Cited by-同舟云学术

Using elemental and boron isotopic compositions of tourmaline to trace fluid evolutions of IOCG systems: The worldclass Dahongshan Fe Cu deposit in SW China

Published:2016-11 Issue: Volume:441 Page:265-279
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Su Zhi-Kun,Zhao Xin-Fu,Li Xiao-Chun,Zhou Mei-Fu

Funder

NSFC

973 program

Fundamental Research Funds

MOST

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference89 articles.

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4. Geochemical and boron, oxygen and hydrogen isotopic constraints on the origin of salinity in groundwaters from the crystalline basement of the Alpine Foreland;Barth;Appl. Geochem.,2000

5. Iron-oxide (CuAuREEPAgUCo) systems;Barton,2014

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