2007
DOI: 10.1016/j.oregeorev.2005.01.002
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Distinctive features of Late Palaeozoic massive sulphide deposits in South China

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Cited by 85 publications
(61 citation statements)
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“…The age of the Shuikoushan granodioritic intrusions is approximately 163.2 Ma . (3) SE China hosts more than half of the world's W-Sn reserves, mostly concentrated in southern Hunan and Jiangxi, northern Guangdong, and Guangxi provinces (Chen et al 1992;Shen et al 1994;Mao and Li 1995;Yin et al 2002;Lu et al 2003;Li et al 2004bLi et al , 2007dMao et al 2004Mao et al , 2007Zhao et al 2005;Peng et al 2006;Gu et al 2007;Hua et al 2007;Yuan et al 2007;Zaw et al 2007). The W-Sn deposits are represented by Shizhuyuan W-Sn and Furong Sn polymetallic deposits in south Hunan, both of which are among the largest and economically important skarn-greisen-vein tungsten-polymetallic deposits in China (Mao and Li 1995;Yin et al 2002;Lu et al 2003).…”
Section: Mesozoic Igneous Rocks In Se Chinamentioning
confidence: 99%
“…The age of the Shuikoushan granodioritic intrusions is approximately 163.2 Ma . (3) SE China hosts more than half of the world's W-Sn reserves, mostly concentrated in southern Hunan and Jiangxi, northern Guangdong, and Guangxi provinces (Chen et al 1992;Shen et al 1994;Mao and Li 1995;Yin et al 2002;Lu et al 2003;Li et al 2004bLi et al , 2007dMao et al 2004Mao et al , 2007Zhao et al 2005;Peng et al 2006;Gu et al 2007;Hua et al 2007;Yuan et al 2007;Zaw et al 2007). The W-Sn deposits are represented by Shizhuyuan W-Sn and Furong Sn polymetallic deposits in south Hunan, both of which are among the largest and economically important skarn-greisen-vein tungsten-polymetallic deposits in China (Mao and Li 1995;Yin et al 2002;Lu et al 2003).…”
Section: Mesozoic Igneous Rocks In Se Chinamentioning
confidence: 99%
“…The first group is stratiform sulfide deposits hosted by Late Carboniferous strata [5][6][7][8][9][10] (e.g. Xinqiao, Dongguashan, Tongguashan, Chengmenshan and Chengshan deposits).…”
Section: Regional Geological Settingmentioning
confidence: 99%
“…In the MLYRB, a similar discordant veinlet and stockwork mineralization below the stratiform sulfide orebody generally is observed, and is thus considered as one of the most important pieces of evidence for the exhalative sedimentary origin of ore deposits [7,10,[16][17][18][19][20]. Previously, the timing of massive sulfide deposits was estimated by dating the minerals in the stratabound sulfide orebody [21][22][23][24][25].…”
mentioning
confidence: 95%
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