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Shizhuyuan Deposit

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Journal Article
Journal: Economic Geology
Published: 01 August 2003
Economic Geology (2003) 98 (5): 955–974.
...Huan-Zhang Lu; Yimao Liu; Changlie Wang; Youzhi Xu; Huaqin Li Abstract The Shizhuyuan deposit, China, is a world-class W-Sn-Bi-Mo-F skarn deposit hosted by Devonian limestone in the thermal aureole of the Qianlishan granite complex. The Qianlishan complex comprises five separate intrusions...
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First thumbnail for: Mineralization and Fluid Inclusion Study of the <s...
Second thumbnail for: Mineralization and Fluid Inclusion Study of the <s...
Third thumbnail for: Mineralization and Fluid Inclusion Study of the <s...
Journal Article
Published: 01 March 2004
Geological Magazine (2004) 141 (2): 225–231.
...XIAN-HUA LI; DUNYI LIU; MIN SUN; WU-XIAN LI; XI-RONG LIANG; YING LIU Abstract The supergiant Shizhuyuan W–Sn–Bi–Mo deposit is hosted by the Qianlishan granite, a small, highly fractionated granitic pluton (~10 km 2 ) with multiple phases of intrusions within the Early Yanshanian granitoid province...
FIGURES
First thumbnail for: Precise Sm–Nd and U–Pb isotopic dating of the supe...
Second thumbnail for: Precise Sm–Nd and U–Pb isotopic dating of the supe...
Third thumbnail for: Precise Sm–Nd and U–Pb isotopic dating of the supe...
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Fig. 2. A. Geological map of the Shizhuyuan ore region (modified after Wang et al., 1987), showing the strata, structure, granite, and mineralization. B. Drill hole profile of the Shizhuyuan deposit, showing the distribution of the four main ore types. The orientation of the first part of the profile is 98°30'; the second part is oriented 142° to show the type I ore (after Wang et al., 1987).
Published: 01 August 2003
F ig . 2. A. Geological map of the Shizhuyuan ore region (modified after Wang et al., 1987 ), showing the strata, structure, granite, and mineralization. B. Drill hole profile of the Shizhuyuan deposit, showing the distribution of the four main ore types. The orientation of the first part
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Fig. 5. Paragenetic relationships of skarn, greisen, and stockwork in the Shizhuyuan deposit. The stockwork ores overprint the skarn and partly overprint the greisen.
Published: 01 August 2003
F ig . 5. Paragenetic relationships of skarn, greisen, and stockwork in the Shizhuyuan deposit. The stockwork ores overprint the skarn and partly overprint the greisen.
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Fig. 12. Summary of published δD and δ18OH2O data of Shizhuyuan deposit. Data compiled from Huang (1988, 1989), and Ji et al. (1989). Diagram from Taylor (1997), indicating the evolution of hydrothermal fluids.
Published: 01 August 2003
F ig . 12. Summary of published δD and δ 18 O H 2 O data of Shizhuyuan deposit. Data compiled from Huang (1988 , 1989 ), and Ji et al. (1989) . Diagram from Taylor (1997) , indicating the evolution of hydrothermal fluids.
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Fig. 1. Regional geological map of southern Hunan province, China, showing the location of the Shizhuyuan deposit and important W, Sn, Pb, Zn, and F deposits in the region (after Lu, 1986). The Xihuashan W deposit is located in Jiangxi province, not too far from the Hunan-Jiangxi boundary. Most tungsten deposits are associated with small Mesozoic granites.
Published: 01 August 2003
F ig . 1. Regional geological map of southern Hunan province, China, showing the location of the Shizhuyuan deposit and important W, Sn, Pb, Zn, and F deposits in the region (after Lu, 1986 ). The Xihuashan W deposit is located in Jiangxi province, not too far from the Hunan-Jiangxi boundary. Most
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(a) Simplified map showing the main plate-scale tectonic units of China. (b) Distribution of Yanshanian grantoids in SE China, with the Early Yanshanian (mainly Jurassic) granitoid province within the interior and the Late Yanshanian (mainly Cretaceous) granitoid province along the coastal region (after Li, 2000). (c) Geological map of the study area illustrating the Qianlishan granite and the Shizhuyuan deposit (after Wang et al. 1987).
Published: 01 March 2004
the coastal region (after Li, 2000 ). (c) Geological map of the study area illustrating the Qianlishan granite and the Shizhuyuan deposit (after Wang et al . 1987 ).
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Fig. 13. Model of the Shizhuyuan W-Sn-Mo-Bi-F deposit. A. Granite 1 emplaced (182–187 Ma) into Devonian limestone, forming skarn and greisen. B. Granite 2 (158–162 Ma) intruded into Devonian limestone, cutting the granite 1, and formed massive greisen, skarn, and later stockwork deposits. C. Granite 3 intruded into granite 2, forming a small greisen body in its upper part. D. Granitic porphyry (144–146 Ma) intruded along northeast faults, associated with Cu, Pb, Zn, and Sb mineralization in surrounding sedimentary rocks.
Published: 01 August 2003
F ig . 13. Model of the Shizhuyuan W-Sn-Mo-Bi-F deposit. A. Granite 1 emplaced (182–187 Ma) into Devonian limestone, forming skarn and greisen. B. Granite 2 (158–162 Ma) intruded into Devonian limestone, cutting the granite 1, and formed massive greisen, skarn, and later stockwork deposits. C
Journal Article
Published: 22 June 2023
Geochemistry: Exploration, Environment, Analysis (2023) 23 (2): geochem2022-062.
...Hao Zhou; Kaixuan Tan; Yongmei Li; Yanshi Xie; Shili Han; Wenzhou Xiao Abstract Shizhuyuan is a world-class W–Sn supergiant polymetallic deposit, with a large area of potential mineralization around it. Samples were taken of Dicranopteris dichotoma, which is widely distributed in the Shizhuyuan...
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First thumbnail for: Biogeochemical fractal characteristics of trace el...
Second thumbnail for: Biogeochemical fractal characteristics of trace el...
Third thumbnail for: Biogeochemical fractal characteristics of trace el...
Journal Article
Published: 14 September 2018
Geochemistry: Exploration, Environment, Analysis (2019) 19 (3): 216–231.
... geochemical anomalies. Given a study area, the MEs of ore-forming elements should be weighted by their concentration factors, in order to quantitatively assess the potential of these elements for generating economic deposits. Taking Shizhuyuan ore-field as a case study, ore-forming elements with greater MEs...
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First thumbnail for: Metallogenic efficiencies of ore-forming elements ...
Second thumbnail for: Metallogenic efficiencies of ore-forming elements ...
Third thumbnail for: Metallogenic efficiencies of ore-forming elements ...
Journal Article
Published: 03 July 2023
American Mineralogist (2023) 108 (7): 1384–1398.
...Kexin Wang; Degao Zhai; Anthony E. Williams-Jones; Dengfeng Li; Jiajun Liu Abstract Numerous skarn-type Sn deposits have been identified in the Nanling Range (South China), of which the Shizhuyuan W-Sn-Bi-Mo, Xianghualing Sn, Jinchuantang Sn-Bi, and Hehuaping Sn deposits are the largest...
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First thumbnail for: Discrete late Jurassic Sn mineralizing events in t...
Second thumbnail for: Discrete late Jurassic Sn mineralizing events in t...
Third thumbnail for: Discrete late Jurassic Sn mineralizing events in t...
Journal Article
Published: 01 March 2024
American Mineralogist (2024) 109 (3): 606–623.
... deposits [SnO 2 reserves of 140 metric kilotons [Kt], 420 Kt, and 178 Kt, respectively) ( Yao et al. 2014 ; Wang et al. 2014 ; Li et al. 2019 )]. Also located within this province are the Dengfuxian (quartz vein-type), Dayishan (greisen-type), Shizhuyuan (greisen-skarn-type), Xianghualing (granite-type...
FIGURES
First thumbnail for: Nature and timing of Sn mineralization in southern...
Second thumbnail for: Nature and timing of Sn mineralization in southern...
Third thumbnail for: Nature and timing of Sn mineralization in southern...
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Schematic geological map of the Qianlishan ore-field, showing the Qianlishan granites (after Mao et al. 1998). The yellow circle with crossing in the centre represents the Shizhuyuan W-Sn-Mo-Bi deposit. The outer black border exhibits the outline of the sediment sampling area.
Published: 14 September 2018
Fig. 1. Schematic geological map of the Qianlishan ore-field, showing the Qianlishan granites (after Mao et al. 1998 ). The yellow circle with crossing in the centre represents the Shizhuyuan W-Sn-Mo-Bi deposit. The outer black border exhibits the outline of the sediment sampling area.
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Simplified geological maps of study areas of five tin deposits: (a) Dengfuxian (after Xiong et al. 2020); (b) Xianghualing (after Wu et al. 2018); (c) Dayishan (after Sun et al. 2018 and Zeng 2013); (d) Shizhuyuan (after Liao et al. 2021); (e) Jiuyishan (after Li et al. 2019, 2021).
Published: 01 March 2024
Figure 2. Simplified geological maps of study areas of five tin deposits: ( a ) Dengfuxian (after Xiong et al. 2020 ); ( b ) Xianghualing (after Wu et al. 2018 ); ( c ) Dayishan (after Sun et al. 2018 and Zeng 2013 ); ( d ) Shizhuyuan (after Liao et al. 2021 ); ( e ) Jiuyishan (after Li et
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Plots of 40Ar*/4He versus 3He/4He of fluid inclusions trapped in stibnites from the Xikuangshan Sb deposit. The ranges of mantle and crustal fluids are defined by the data from Turner et al. (1993), Stuart et al. (1995), Burnard et al. (1999), and Hu et al. (2012). The data of the Yaogangxian W, Xihuashan W, and Shizhuyuan W-Sn-Bi-Mo deposits are, respectively, from Hu et al. (2012), Wei et al. (2019), and Wu et al. (2011).
Published: 25 July 2022
) . The data of the Yaogangxian W, Xihuashan W, and Shizhuyuan W-Sn-Bi-Mo deposits are, respectively, from Hu et al. (2012) , Wei et al. (2019) , and Wu et al. (2011) .
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Sm–Nd isochron diagram for garnet, fluorite and wolframite mineral separates from skarn and greisen at the Shizhuyuan polymetallic deposit. Sm–Nd isochron age and εNd(T) values were calculated using Isoplot/Ex 2.49 after Ludwig (2001), where 0.5 % was chosen as the error of 147Sm/144Nd ratios. Errors are quoted at the 95 % confidence level. G – garnet; F – fluorite; W – wolframite.
Published: 01 March 2004
Figure 3. Sm–Nd isochron diagram for garnet, fluorite and wolframite mineral separates from skarn and greisen at the Shizhuyuan polymetallic deposit. Sm–Nd isochron age and εNd(T) values were calculated using Isoplot/Ex 2.49 after Ludwig (2001) , where 0.5 % was chosen as the error of 147 Sm
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The superimposed geochemical anomalies of W-Sn-Mo-Bi-Au-Cu-Pb-Zn and the locations of the predominant deposits in the Shizhuyuan ore-field, southern Hunan Province, China (modified after Mao et al. 1998). Herein the area delineated by the irregular closed curve at the central part represents the causative Qianlishan granites; and the red lines represent the regional lineaments: the three thicker ones denoted by F1, F2 and F3 (F4 is the inferred fracture) stand for major fractures and the other thinner ones for the secondary fractures attaching to the main rupture system. The sizes of marks of the predominant deposits correspond to the tonnages of ore reserves.
Published: 14 September 2018
Fig. 7. The superimposed geochemical anomalies of W-Sn-Mo-Bi-Au-Cu-Pb-Zn and the locations of the predominant deposits in the Shizhuyuan ore-field, southern Hunan Province, China (modified after Mao et al. 1998 ). Herein the area delineated by the irregular closed curve at the central part
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Plots of (A) Q/3He versus 4He/3He and (B) 4He/36Ar versus 3He/Q of the inclusion fluids trapped by stibnites from the Xikuangshan Sb deposit (modified after Burnard and Polya, 2004). The ranges of Lucky Strike vent fluids and East Pacific Rise (EPR) vent fluids are defined by the data from Jean-Baptiste et al. (1998), Lupton et al. (1989), and Lupton et al. (1995). The plots of the Yaogangxian W, Xihuashan W, and Shizhuyuan W-Sn-Bi-Mo deposits are calculated, respectively, from the raw data of Hu et al. (2012), Wei et al. (2019), and Wu et al. (2011). MORB—mid-oceanic ridge basalt; STP—standard temperature and pressure.
Published: 25 July 2022
are defined by the data from Jean-Baptiste et al. (1998) , Lupton et al. (1989) , and Lupton et al. (1995) . The plots of the Yaogangxian W, Xihuashan W, and Shizhuyuan W-Sn-Bi-Mo deposits are calculated, respectively, from the raw data of Hu et al. (2012) , Wei et al. (2019) , and Wu et al. (2011
Journal Article
Journal: SEG Discovery
Published: 01 July 2007
SEG Discovery (2007) (70): 1–15.
..., South China : Ore Geology Reviews , v. 31 , p. 304 – 318 . Mao , J. , and Li , H. , 1995 , Evolution of the Qianlishan granite stock and its relation to the Shizhuyuan polymetallic tungsten deposit : International Geology Review , v. 37 , p. 63 – 80 . Mao , J. , Li , H...
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First thumbnail for: Exploring in China: The Challenges and Rewards
Journal Article
Journal: Economic Geology
Published: 01 August 2019
Economic Geology (2019) 114 (5): 1005–1012.
... 0.59 Mt Sn 151.8 ± 1.4 150.3 ± 0.5 (molybdenite Re-Os) Mao et al., 2013 ; Liang et al., 2016 Sn-W deposit Shizhuyuan Skarn and greisen 0.80 Mt WO 3 ; 0.49 Mt Sn 155 151.0 ± 3.5 (molybdenite Re-Os) Zhao et al., 2018 Xiangyuan Greisen 0.08 Mt Sn; 0.10 Mt WO 3 158 157.5 ±1.0...
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First thumbnail for: Protolith-Related Thermal Controls on the Decoupli...
Second thumbnail for: Protolith-Related Thermal Controls on the Decoupli...
Third thumbnail for: Protolith-Related Thermal Controls on the Decoupli...