2015
DOI: 10.1016/j.oregeorev.2015.01.020
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Electron microprobe analyses of ore minerals and H–O, S isotope geochemistry of the Yuerya gold deposit, eastern Hebei, China: Implications for ore genesis and mineralization

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Cited by 17 publications
(19 citation statements)
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References 119 publications
(163 reference statements)
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“…Liu et al, 2016;Liu, Shao, et al, 2018;Shi et al, 2015;Shi et al, 2019;Song et al, 2016;Xiong, 2017;Zhang et al, 2017;Zhang et al, 2020). The carbon and oxygen isotopes of the quartz inclusions and hydrothermal carbonates in the gold deposits in the study area indicated that the source of carbon in the fluids of the main metallogenic stage was mainly the deep-seated magmatic source (Kong et al, 2015;Liu et al, 2016;Liu, Deng, et al, 2018;Shi et al, 2015;Xiong, 2017).…”
Section: Tectonic Setting and Implications For Metallogenesismentioning
confidence: 89%
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“…Liu et al, 2016;Liu, Shao, et al, 2018;Shi et al, 2015;Shi et al, 2019;Song et al, 2016;Xiong, 2017;Zhang et al, 2017;Zhang et al, 2020). The carbon and oxygen isotopes of the quartz inclusions and hydrothermal carbonates in the gold deposits in the study area indicated that the source of carbon in the fluids of the main metallogenic stage was mainly the deep-seated magmatic source (Kong et al, 2015;Liu et al, 2016;Liu, Deng, et al, 2018;Shi et al, 2015;Xiong, 2017).…”
Section: Tectonic Setting and Implications For Metallogenesismentioning
confidence: 89%
“…Samples of sulphide minerals from the Matouniu gold deposit yielded δ 34 S values ranging from À0.5 to 5.6‰, with an average value of 4.4‰; the limited range of δ 34 S values suggest relatively stable physicochemical conditions in the ore-forming fluids in this stage (Ma et al, 2018), which has features similar to those of typical magmatic-hydrothermal deposits (0 ± 5‰, Ohmoto, 1972;Ohmoto & Rye, 1997). Moreover, sulphide isotope compositions of the Matouniu gold deposit are consistent with those of other Yanshanian Au deposits in the Eastern Hebei region, such as the Xiajinbao (À0.2 to 3.7‰), Huajian (1.5-5.4‰), Jinchangyu (À4.4 to 5.2‰), Tangzhangzi (2.1-5.5‰), and Yuerya (À0.3 to 5.3‰) deposits; all of which are commonly thought to be of magmatic origin (He, 2015;Kong et al, 2015;Liu et al, 2016;Liu, Shao, et al, 2018;Shi et al, 2015;Shi et al, 2019;Song et al, 2016;Zhang, Shao, Wang, Liu, & Xiong, 2017;Zhang et al, 2020), indicating that the sulphur of the Matouniu gold deposit was derived from magmatic-hydrothermal sources.…”
Section: Sources Of the Ore-forming Materials And Fluidsmentioning
confidence: 99%
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“…These gold deposits are located in brittle‐ductile shear zones and fractures (Figure 2). Gold occurs as disseminated or quartz veins within either the Precambrian metamorphic basement (e.g., Songjianghe, Jiapigou, Paishanlou, Jinchanggouliang, and Jinchangyu; L. Liu et al., 2020; S. F. Liu et al., 2021; Song et al., 2016; X. H. Zhang et al., 2005; X. T. Zhang et al., 2019) or Mesozoic granites (e.g., Yu'erya; Kong et al., 2015). The sulfides in the ore include pyrite, chalcopyrite, galena, and sphalerite.…”
Section: Geological Backgroundmentioning
confidence: 99%
“…Recently, trace element analysis of ore minerals has been widely used in the study of the metal sources of gold deposits (Zhang et al ., 2014a; 2014b; Kong et al ., 2015; Mills et al ., 2015). For example, sedimentary pyrite generally has Co/Ni ratios of <1 (Bajwah et al ., 1987), while hydrothermal pyrite generally has Co/Ni ratios of >1 (Bralia et al ., 1979).…”
Section: Introductionmentioning
confidence: 99%