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Jun 16, 2021

Gold-only porphyries, such as at Fort Knox, Alaska appear to occur at higher levels than Cu-Au porphyry deposits, which are themselves at higher levels than Cu-Mo porphyritic intrusives as, described schematically in Fig. 2.24.The fluids are thought to be initially hot (500–600 C) but zoned alteration assemblages are formed at lower temperatures as the metal-bearing fluid

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    sedimentary rock-hosted gold deposits in P.R. China. These breccia bodies are conformable with stratigraphic units in the host rock. An example of this is the Shuangwang gold deposit (Fan, S.C. and Jin, Q.H., 1994), which is a large Carlin-type gold deposit in the Qinling area, hosted by stratabound breccia bodies (fig. 29)

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    Jan 11, 2022 Cal Everett, President and CEO of Liberty Gold stated, “The +1 million ounce Goldstrike Deposit presents robust economics at today’s gold prices as illustrated in the 2018 PEA and is advancing

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    An orogenic gold deposit is a type of hydrothermal mineral deposit.More than 75% of the gold recovered by humans through history belongs to the class of orogenic gold deposits. Rock structure is the primary control of orogenic gold mineralization at all scales, as it controls both the transport and deposition processes of the mineralized fluids, creating structural pathways of

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    Nov 10, 2020 This report summarizes the primary characteristics of alkalic-type epithermal gold (Au) deposits and provides an updated descriptive model. These deposits, primarily of Mesozoic to Neogene age, are among the largest epithermal gold deposits in the world. Considered a subset of low-sulfidation epithermal deposits, they are spatially and genetically

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    Jul 01, 2018 1. Introduction. The genesis of vein-type to disseminated gold deposits, broadly classified as orogenic gold deposits (Groves et al., 1998, Goldfarb et al., 2005) has remained controversial.The genetic models for these deposits were evaluated in a recent review by Goldfarb and Groves (2015).Much attention has been focused on the source of auriferous fluids

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