2017
DOI: 10.1016/j.jseaes.2016.09.004
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Mesozoic gold mineralization in Hainan Province of South China: Genetic types, geological characteristics and geodynamic settings

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Cited by 28 publications
(33 citation statements)
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“…1.8 -1.45 Ga); [16], Meso-Neoproterozoic Shilu Group (ca. 1075 -880 Ma); [19] and Neoproterozoic-Sinian Shihuiding Formation [12]. The Baoban Group predominantly distributed in the central Hainan Province, is composed of migmatitic gneisses, black shales, plagioclase-amphibole gneisses, and quartz-muscovite schists with amphibolite to granulite facies metamorphism [9,20].…”
Section: Regional Geologymentioning
confidence: 99%
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“…1.8 -1.45 Ga); [16], Meso-Neoproterozoic Shilu Group (ca. 1075 -880 Ma); [19] and Neoproterozoic-Sinian Shihuiding Formation [12]. The Baoban Group predominantly distributed in the central Hainan Province, is composed of migmatitic gneisses, black shales, plagioclase-amphibole gneisses, and quartz-muscovite schists with amphibolite to granulite facies metamorphism [9,20].…”
Section: Regional Geologymentioning
confidence: 99%
“…It is noteworthy to mention that all the Precambrian metasediments are characterized with high contents of CM, up to volumetrically >10%, and it is hosted in the black shales, slates and carbonaceous shales, carbonaceous phyllites and carbonaceous mudstones [12,16,17]. These carbonaceous rocks commonly occur over many tens of kilometers rock band in the central Hainan Province [23].Previous research indicates that CM is likely to be generated by metamorphism during Caledonian period, and soured from Precambrian [24].…”
Section: Regional Geologymentioning
confidence: 99%
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