| Doyle, M. G., Fletcher, I. R., Foster, J., Large, R. R., Mathur, R., McNaughton, N. J., Meffre, S., Muhling, J. R., Phillips, D., Rasmussen, B. (2015) Geochronological Constraints on the Tropicana Gold Deposit and Albany-Fraser Orogen, Western Australia. Economic Geology, 110 (2) 355-386 doi:10.2113/econgeo.110.2.355 | Journal (article/letter/editorial) | Constraints on the Tropicana Gold Deposit and Albany-Fraser Orogen, Western Australia Mark G. Doyle,1,†...Tower, 44 St. Georges Terrace, Perth, Western Australia 6000, Australia 2 Institute for Geoscience Research...Research, Curtin University, Perth, Western Australia 6845, Australia 3 CODES, 4 Department 5 John 6 Centre...University of Tasmania, Hobart, Tasmania 7001, Australia of Geology, Juniata College, 1700 Moore Street...Research, Curtin University, Perth, Western Australia 6845, Australia for Microscopy, Characterization | | | Journal (article/letter/editorial) | Sanukitoid Gold Porphyry Deposits: A New Understanding and Genetic Model from the Lac Bachelor Gold Deposit...craton, Canada, recognition of intrusion-related gold deposits is improving, but their formation remains...quartz-syenite to alkali-granite centered deposit. Gold is associated with pyrite in localized alkaline...alkaline-oxidized magma, which favors sulfur and gold solubility and transport, migrates through the crust...volcanic host rock caused sulfide precipitation and gold deposition. This genetic model is applied to the | | Molnár, Ferenc, O’Brien, Hugh, Lahaye, Yann, Käpyaho, Asko, Sorjonen-Ward, Peter, Hyodo, Hironobu, Sakellaris, Grigorios (2016) Signatures of Multiple Mineralization Processes in the Archean Orogenic Gold Deposit of the Pampalo Mine, Hattu Schist Belt, Eastern Finland. Economic Geology, 111 (7) 1659-1703 doi:10.2113/econgeo.111.7.1659 | Journal (article/letter/editorial) | Processes in the Archean Orogenic Gold Deposit of the Pampalo Mine, Hattu Schist Belt, Eastern Finland*...Hattu schist belt is an emerging gold-producing ore district in the western part of the Archean Karelian...(550° ± 50°C; 3–5 kbar) at ca. 2.70 Ga. Orogenic gold deposits are hosted by the highly strained zones...characterize this hydrothermal activity. The major stage of gold ore deposition can be confined to the subsequent...that potassium gain correlates with increase of gold concentrations in the mafic schist and feldspar-porphyry |
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