Mineral equilibria and zircon, garnet and titanite U-Pb ages constraining the PTt path of granite-related hydrothermal systems at the Big Bell gold deposit, Western Australia

Author:

Mueller Andreas G.,McNaughton Neal J.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Reference83 articles.

1. Aleinikoff JN, Wintsch RP, Fanning CM, Dorais MJ (2002) U-Pb geochronology of zircon and polygenetic titanite from the Glastonbury complex, Connecticut, USA: an integrated SEM, EPMA, TIMS and SHRIMP study. Chem Geol 188:125–147

2. Barth TFW (1959) Principles of classification and norm calculations of metamorphic rocks. J Geol 67:135–152

3. Baxter JL (1978) Molybdenum, tungsten, vanadium and chromium in Western Australia. Geological Survey of Western Australia, Mineral Resour Bull 11 140 pp

4. Beck R (1900) The nature of ore deposits (in German, translated and revised by WH weed, 1905, 1909). McGraw-Hill, New York 685 pp

5. Bhattacharya A, Mazumdar AC, Sen SK (1988) Fe-Mg mixing in cordierite: constraints from natural data and implications for cordierite-garnet geothermometry in granulites. Am Mineral 73:338–344

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