The use of fluid inclusion decrepitometry to distinguish mineralized and barren quartz veins in the aberfoyle tin-tungsten mine area, Tasmania-Reference-Cited by-同舟云学术

The use of fluid inclusion decrepitometry to distinguish mineralized and barren quartz veins in the aberfoyle tin-tungsten mine area, Tasmania

Published:1983-12 Issue:1-3 Volume:19 Page:319-333
ISSN:0375-6742
Container-title:Journal of Geochemical Exploration
language:en
Short-container-title:Journal of Geochemical Exploration

Author:

Burlinson K.,Dubessy J.C.,Hladky G.,Wilkins R.W.T.

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology

Reference18 articles.

1. The geology of the Rossarden-Storeys Creek District;Blissett;Geol. Surv. Tasmania Bull.,1959

2. A decrepitation study of quartz from the Campbell and Negus-Rycon shear zone systems, Yellowknife, Northwest Territories;Boyle;Geol. Surv. Can. Bull.,1954

3. Fluid inclusion studies in relation to hydrothermal alteration and mineralization at the Koloula porphyry copper prospect Guadalcanal;Chivas;Econ. Geol.,1977

4. Analyse d'inclusions fluides à la microsonde MOLE à effet Raman;Dhamelincourt;Bull. Mineral.,1979

5. Mineralization at Aberfoyle tin mine, Rossarden, Tasmania;Edwards,1957

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