Nature and origin of the fluids responsible for forming the Hellyer Zn–Pb–Cu, volcanic-hosted massive sulphide deposit, Tasmania, using fluid inclusions, and stable and radiogenic isotopes-Reference-Cited by-同舟云学术

Nature and origin of the fluids responsible for forming the Hellyer Zn–Pb–Cu, volcanic-hosted massive sulphide deposit, Tasmania, using fluid inclusions, and stable and radiogenic isotopes

Published:2004-08 Issue:1-2 Volume:25 Page:89-124
ISSN:0169-1368
Container-title:Ore Geology Reviews
language:en
Short-container-title:Ore Geology Reviews

Author:

Solomon M,Gemmell J.B,Zaw Khin

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference96 articles.

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3. The mineralogy and chemical composition of the Woodlawn massive sulphide orebody;Ayres;Journal of the Geological Society of Australia,1979

4. Reaction pathways in the Fe–S system below 100 °C;Benning;Chemical Geology,2000

5. The tectonic significance of Cambrian allochthonous mafic–ultramafic complexes in Tasmania;Berry;Australian Journal of Earth Sciences,1988

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