The Permian Watershed tungsten deposit (northeast Queensland, Australia): fluid inclusion and stable isotope constraints

Author:

Poblete J. A.12ORCID,Huizenga J-M.134ORCID,Chang Z.15,Dirks P.1ORCID

Affiliation:

1. Economic Geology Research Centre, College of Science and Engineering, James Cook University, Townsville, QLD, Australia

2. W.H. Bryan Geology and Mining Centre, Sustainable Minerals Institute, Indooroopilly, QLD, Australia

3. Faculty of Environmental Sciences and Natural Resource Management, Norwegian University of Life Sciences, Ås, Norway

4. Department of Geology, University of Johannesburg, Johannesburg, South Africa

5. Department of Geology and Geological Engineering, Colorado School of Mines, Golden, CO, USA

Funder

Geological Survey of Queensland, Department of Natural Resources, Mines and Energy, Queensland, under the Future Resources Program

Publisher

Informa UK Limited

Reference72 articles.

1. Adams, C. J., Wormald, R., & Henderson, R. A. (2013). Detrital zircons from the Hodgkinson Formation: Constraints on its maximum depositional age and provenance. In P. A. Jell (Ed.), Geology of Queensland (pp. 239–241). Geological Survey of Queensland.

2. The structure of the Palaeozoic sediments of the Mossman and Cooktown areas, North Queensland

3. Ault, W. V. (1963). Summary of sulfur isotope standards. In M. L. Jensen (Ed.), Biogeochemistry of sulfur isotopes, National Science Foundation Symposium Proceedings (pp. 509–567). Yale University.

4. Fluid Inclusions in Hydrothermal Ore Deposits

5. Bodnar, R. J., & Vityk, M. O. (1994). Interpretation of microthermometric data for H2O–NaCl fluid inclusions. In B. De Vivo & M. L. Frezzotti (Eds.), Minerals, methods and applications (pp. 117–130). Virginia Tech.

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