2015
DOI: 10.1002/gj.2644
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Geochemistry, zircon U–Pb analysis, and fluid inclusion 40Ar/39Ar geochronology of the Yingchengzi gold deposit, southern Heilongjiang Province, NE China

Abstract: The Yingchengzi gold deposit, located 10 km west of Shalan at the eastern margin of the Zhangguangcai Range, is the only high commercially valuable gold deposit in southern Heilongjiang Province, NE China. This study investigates the chronology and geodynamic mechanisms of igneous activity and metallogenesis within the Yingchengzi gold deposit. New zircon U-Pb data, fluid inclusion 40 Ar/ 39 Ar dating, whole-rock geochemistry and Sr-Nd isotopic analysis is presented for the Yingchengzi deposit to constrain its… Show more

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Cited by 18 publications
(11 citation statements)
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“…For the major orogenic gold deposits in the world that was listed by Goldfarb, Groves, and Gardoll () and Groves, Goldfarb, Gebre‐Mariam, Hagemann, and Robert (), gold mineralization was originally thought to occur in an accretionary orogenic tectonic setting (e.g., Barley & Groves, ; Kerrich, Goldfarb, Groves, Garwin, & Jia, ), especially in the outer converge supercontinent cycle or the edge of the inner converge supercontinent cycle. In recent years, several medium to large orogenic gold deposits have been discovered in collisional orogenic belt (e.g., Chai, Sun, Xing, Chen, & Han, ; Kong et al, ), especially in the Tibetan Plateau in China. At least two important Himalayan period orogenic gold deposit belts have been identified, which are the Ailaoshan orogenic gold belt controlled by lateral shear strike‐slip (~30 Ma; e.g., Deng & Wang, ; Deng, Wang, Li, Li, & Wang, ) and the Yarlung Tsangpo orogenic gold belt controlled by forward collision extrusion (~50 Ma; e.g., Hou & Cook, ; Jiang, Nie, Hu, Lai, & Liu, ; Sun et al, , ; Zhang et al, ).…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…For the major orogenic gold deposits in the world that was listed by Goldfarb, Groves, and Gardoll () and Groves, Goldfarb, Gebre‐Mariam, Hagemann, and Robert (), gold mineralization was originally thought to occur in an accretionary orogenic tectonic setting (e.g., Barley & Groves, ; Kerrich, Goldfarb, Groves, Garwin, & Jia, ), especially in the outer converge supercontinent cycle or the edge of the inner converge supercontinent cycle. In recent years, several medium to large orogenic gold deposits have been discovered in collisional orogenic belt (e.g., Chai, Sun, Xing, Chen, & Han, ; Kong et al, ), especially in the Tibetan Plateau in China. At least two important Himalayan period orogenic gold deposit belts have been identified, which are the Ailaoshan orogenic gold belt controlled by lateral shear strike‐slip (~30 Ma; e.g., Deng & Wang, ; Deng, Wang, Li, Li, & Wang, ) and the Yarlung Tsangpo orogenic gold belt controlled by forward collision extrusion (~50 Ma; e.g., Hou & Cook, ; Jiang, Nie, Hu, Lai, & Liu, ; Sun et al, , ; Zhang et al, ).…”
Section: Introductionmentioning
confidence: 99%
“…In recent years, several medium to large orogenic gold deposits have been discovered in collisional orogenic belt (e.g., Chai, Sun, Xing, Chen, & Han, 2016;Kong et al, 2017), especially in the Tibetan Plateau in China. At least two important Himalayan period orogenic gold deposit belts have been identified, which are the Ailaoshan orogenic gold belt controlled by lateral shear strike-slip (~30 Ma; e.g., Deng & Wang, 2016;Deng, Wang, Li, Li, & Wang, 2014) and the Yarlung Tsangpo orogenic gold belt controlled by forward collision extrusion (~50 Ma; e.g., Hou & Cook, 2009;Jiang, Nie, Hu, Lai, & Liu, 2009;Sun et al, 2015Sun et al, , 2016Zhang et al, 2017).…”
Section: Introductionmentioning
confidence: 99%
“…The majority of orogenic or lode gold deposits are structurally controlled by brittle–ductile shear zones and faults, and are characterized by fault‐valve behavior (Sibson, , ; Sibson et al, ; Cox et al, ; Chai et al, , b, c). The fault‐valve model for these gold deposits describes a cyclical fluctuation in fluid pressures, from lithostatic to hydrostatic, on account of episodic shearing (Sibson et al, ).…”
Section: Discussionmentioning
confidence: 99%
“…Mesozoic continental facies volcanic–sedimentary rocks, Cenozoic continental basalts and fluvial clastic sediments are also present within sedimentary basins in the area (Sun et al ., 2000). The formation of base metal and precious metal mineral deposits, including numerous porphyry and epithermal gold, copper and molybdenum deposits, occurred during multiphase tectonic activity and magmatism (Sun et al, ); consequently, the geology of the study area has been investigated in detail (Wu et al, ; Meng et al, ; Mao et al, ; Qi et al, ; Sun et al, ; Chai et al, , b).…”
Section: Regional Geologymentioning
confidence: 99%