Tungsten and tin mineralization in the northern Jiangxi–southern Anhui metallogenic belt, eastern Jiangnan Orogen, China
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摘要: 江南造山带东段赣北—皖南成矿带是近些年新厘定的世界级钨（W）富集区。为突破传统S型花岗岩单一控矿的认识，厘清区内S型、I型、A型花岗岩对应的钨−锡（W-Sn）成矿差异，揭示成矿动力学机制，建立区域成矿模式并服务深部勘查，文章综合运用野外地质调查、岩矿相学观察、锆石/热液矿物U-Pb测年、辉钼矿Re-Os年代学、Sr-Nd-Hf同位素分析、矿物原位微区微量元素测定以及流体包裹体分析等，系统对比朱溪、大湖塘、香炉山、阳储岭、东源、西坞口等典型矿床的地质−岩浆−热液特征，按照S型、I型、A型花岗岩分类剖析成矿作用，归纳成矿物质迁移富集过程。研究结果表明：该成矿带W资源总量已超南岭成矿带，主成矿时代集中于燕山期150～130 Ma；S型花岗岩控制朱溪和大湖塘超大型钨−铜（W-Cu）多金属矿床，为强过铝、还原岩浆体系，以矽卡岩及复合叠加矿化为特征；I型花岗岩产出香炉山、阳储岭、东源等大—中型钨−钼（W-Mo）多金属矿床，属于中—高温弱过铝质岩浆，发育斑岩−矽卡岩矿化，白钨矿钙质既可来自碳酸盐围岩，也可来自岩体中斜长石等硅酸盐矿物蚀变；A型花岗岩以西坞口锡−钨−铷（Sn-W-Rb）矿床为代表，高分异富氟，富集锡、铷等稀有金属；该成矿带遵循“基底预富集—中生代壳幔作用—岩浆流体卸载”成矿三阶段富集模式，深部动力源自古太平洋板块俯冲后撤与岩石圈伸展；该成矿带可划定出断裂交汇、隐伏岩体穹窿等4类深部找矿靶区。江南造山带钨−锡成矿并不局限于S型花岗岩，S-I-A型花岗岩可形成差异化成矿体系；双桥山群富钨、锡变质基底提供物质基础，壳幔相互作用提供热源与部分物质贡献，岩浆分异−流体演化控制金属沉淀。此研究成果完善了区域钨−锡成矿理论，可为赣北—皖南地区及其他相似地区关键矿产深部勘查提供理论依据。Abstract:
Objective Tungsten and tin are strategic critical metals in China. The Northern Jiangxi–Southern Anhui metallogenic belt in the eastern Jiangnan Orogen is a newly recognized world-class tungsten-rich province. This study aims to supplement the traditional understanding that tungsten mineralization is solely controlled by S-type granites, clarify the differences in W-Sn mineralization related to S-, I-, and A-type granites, reveal geodynamic metallogenic mechanisms, establish regional metallogenic models, and support deep mineral exploration. Methods Based on field geological investigations, petrographic observations, U–Pb dating of zircon and other hydrothermal minerals, molybdenite Re–Os geochronology, Sr–Nd–Hf isotopes, in-situ trace-element analysis of minerals, and fluid-inclusion data, typical deposits including Zhuxi, Dahutang, Xianglushan, Yangchuling, Dongyuan and Xiwukou were systematically compared. Metallogenic processes were analyzed under the classification of S-, I- and A-type granites, and the migration-enrichment of ore-forming materials was summarized. Results (1) The total W resources in this belt exceed those in the Nanling metallogenic belt, with major Yanshanian metallogenic ages of 150–130 Ma. (2) S-type granites host the giant Zhuxi and Dahutang W-Cu polymetal deposits, characterized by strongly peraluminous, reduced magmas and skarn-superimposed mineralization. (3) I-type granites host medium-to-large W-Mo polymetal deposits, such as Xianglushan, Yangchuling, and Dongyuan, which formed under medium-to-high temperature conditions in weakly-peraluminous systems with porphyry-skarn mineralization; calcium for scheelite formation derives either from carbonate wall rocks or silicate-mineral (e.g, plagioclase) alteration within plutons. (4) The A-type-granite-related Xiwukou Sn-W-Rb deposit records highly fractionated, F-rich magmatism with the enrichment of Sn, Rb, and other rare metals. (5) A three-stage enrichment model is established: basement pre-enrichment, Mesozoic crust-mantle interaction, and magmatic fluid exsolution and unloading. Regional mineralization is likely driven by Paleo-Pacific slab rollback and lithospheric extension. (6) Four categories of deep prospecting targets, e.g. fault intersections and concealed pluton domes, are proposed. Conclusions The W-Sn mineralization in the Jiangnan Orogen is not restricted to S-type granites; S-, I- and A-type granites constitute differentiated metallogenic systems. The W-Sn-enriched meta-sedimentary rock basement of the Shuangqiaoshan Group provides primary ore-forming materials, while crust-mantle interaction supplies heat and partial components; magma differentiation and fluid evolution dominate metal precipitation. Significance This work improves the regional understanding of W-Sn metallogenesis and provides theoretical support for the deep exploration of strategic critical minerals, not only in Northern Jiangxi-Southern Anhui provinces but also in other areas with similar geological conditions. -
图 1 江南造山带岩浆岩及钨−锡矿床分布图（据Su and Jiang, 2017；Shu et al., 2019修改）
D-1—大湖塘钨矿床；D-2—朱溪钨矿床；D-3—香炉山钨矿床；D-4—阳储岭钨矿床；D-5—塔前钨矿床；D-6—东源钨矿床；D-7—百丈岩钨矿床；D-8，高家塝钨矿床；D-9—大邬尖钨矿床；D-10—竹溪岭钨矿床；D-11—彭山锡矿床；D-12—西坞口W-Sn-Rb矿床；J-1—怀玉地体；J-2—鄣公地体；J-3—九岭地体；J-4—湘北地体；J-5—桂北地体；①—郯城−庐江断裂带；②—石台−九江−吉首断裂带；③—樟树墩−德兴−歙县断裂带；④—赣江隐伏断裂；⑤—汨罗–湘潭隐伏断裂；⑥—城步–永福断裂；⑦—绍兴–萍乡–祁东–全州–龙胜–永福缝合带；⑧—政和–大埔断裂带
Figure 1. Distribution of magmatic rocks and related tungsten and tin deposits in the Jiangnan Orogen (modified after Su and Jiang, 2017; Shu et al., 2019)
D-1–Dahutang W deposit; D-2–Zhuxi W deposit; D-3–Xianglushan W deposit; D-4–Yangchuling W deposit; D-5–Taqian W deposit; D-6–Dongyuan W deposit; D-7–Baizhangyan W deposit; D-8–Gaojiabang W deposit; D-9–Dawujian W deposit; D-10–Zhuxiling W deposit; D-11–Pengshan Sn deposit; D-12–Xiwukou W-Sn-Rb deposit; J-1–Huaiyu terrane; J-2–Zhanggong terrane; J-3–Jiuling terrane; J-4–Northern Hunan terrane; J-5–Northern Guangxi terrane; ①–Tancheng–Lujiang fault zone; ②–Shitai–Jiujiang–Jishou fault zone; ③–Zhangshudun–Dexing–Shexian fault zone; ④–Ganjiang buried fault; ⑤–Miluo–Xiangtan buried fault; ⑥–Chengbu–Yongfu fault; ⑦–Shaoxing–Pingxiang–Qidong–Quanzhou–Longsheng–Yongfu suture zone; ⑧–Zhenghe–Dapu fault zone
图 2 朱溪矿区岩浆岩中锆石和磷灰石及与成矿有关热液矿物年龄总汇
年龄数据为各文献报道的加权平均年龄、等时线年龄或谐和年龄结果；年龄数据来源于Pan et al.（2017，2018）、Song et al.（2018b，2019，2021，2023b）、Zhang et al.（2020a，2020b，2021b）、Hong et al.（2022）、Qiu et al.（2024）、Ouyang et al.（2025）、Yang et al.（2025b）和Zhao et al.（2023，2026）；图中蓝灰色垂直背景区域代表该区成岩成矿年龄主要区间
Figure 2. Compilation of published ages for zircon and apatite from magmatic rocks and ore-related hydrothermal minerals from the Zhuxi ore district
Ages are weighted mean, isochron, or concordia ages reported by Pan et al. (2017, 2018), Song et al. (2018b, 2019, 2021, 2023b), Zhang et al. (2020a, 2020b, 2021b), Hong et al. (2022), Qiu et al. (2024), Ouyang et al. (2025), Yang et al. (2025b), and Zhao et al. (2023, 2026); The grayish-blue shaded vertical bands indicate the main age intervals of diagenesis and mineralization in the study area.
图 3 朱溪矿区岩浆岩Sr-Nd-Hf同位素组成
图a中的虚线区域分别为江南W-Mo矿带、大湖塘W-Cu矿带和新元古代双桥山群岩石的数据（Song et al. 2018b）；图b中Hf地壳演化线（1.0 Ga、1.5 Ga、2.0 Ga、2.5 Ga）据Vervoort et al.（1999）计算；CHUR— 球粒陨石均一储库（Chondritic Uniform Reservoir）；朱溪矿区Sr-Nd-Hf同位素数据来源于Pan et al.（2018）、Song et al.（2018b，2021，2023b）、Zhang et al.（2020b）和Ouyang et al.（2025）a—朱溪矿区岩浆岩Sr-Nd同位素图解；b—朱溪矿区岩浆岩锆石Hf同位素图解
Figure 3. Sr–Nd–Hf isotopic compositions of magmatic rocks from the Zhuxi ore district
(a) Sr–Nd isotope diagram of magmatic rocks in the Zhuxi ore district; (b) Hf isotope diagram of zircon from magmatic rocks in the Zhuxi ore districtThe three regions with dashed outlines in panel a are data for Jiangnan W–Mo and Dahutang W–Cu magmatic rocks and Neoproterozoic strata (after Song et al. 2018b and references therein); The Hf crustal evolution lines (e.g., 1.0 Ga, 1.5 Ga, 2.0 Ga, and 2.5 Ga) in panel b are calculated after Vervoort et al. (1999), the Zhuxi Sr–Nd–Hf isotopic composition data are sourced from Pan et al. (2018), Song et al. (2018b, 2021, 2023b), Zhang et al. (2020b), and Ouyang et al. (2025).
图 4 大湖塘矿床两阶段成矿模式图（据蒋少涌等，2015；胡大龙，2023修改）
Wol—黑钨矿；Sch—白钨矿；Ccp—黄铜矿；Mol—辉钼矿；Cst—锡石；Stn—黝锡矿；Mus—白云母；Tur—电气石；Pl—斜长石；Kfs—钾长石；Ap—磷灰石a—大湖塘矿床第1阶段（150~144 Ma）成矿模式图；b、c—第1阶段不同矿段的矿化特征及矿物组合；d—大湖塘矿床第2阶段（138~130 Ma）成矿模式图；e、f—第2阶段不同矿段的矿化特征及矿物组合
Figure 4. Two-stage metallogenic model for the Dahutang ore deposit (modified after Jiang et al., 2015; Hu, 2023)
(a) The ore-forming model of the first stage (150–144 Ma) of the Dahutang deposit; (b and c) The mineralization characteristics and mineral assemblages of various ore sections in the first stage; (d) The ore-forming model of the second stage (138–130 Ma) of the Dahutang deposit; (e and f) The mineralization characteristics and mineral assemblages of different ore sections in the second stage Wol–wolframite; Sch–scheelite; Ccp–chalcopyrite; Mol–molybdenite; Cst–cassiterite; Stn–stannite; Mus–muscovite; Tur–tourmaline; Pl–plagioclase; Kfs–K-feldspar; Ap–apatite
图 5 香炉山钨矿成矿模式简图
a—香炉山钨矿床岩浆作用与成矿示意图（据戴盼，2018修改）；b—香炉山钨矿床矿化空间展布模式图（据吴胜华等，2014修改）
Figure 5. Schematic metallogenic model for the Xianglushan W deposit
(a) Schematic model illustrating magmatism and mineralization of the Xianglushan tungsten deposit (modified after Dai, 2018); (b) Spatial distribution model of mineralization types of the Xianglushan tungsten deposit (modified after Wu et al., 2014)
图 6 江西阳储岭W-Mo矿床中不同类型白钨矿的典型照片（Xiong et al.，2025）
a—二长花岗斑岩内发蓝色荧光的白钨矿（紫外灯下）；b—背散射图像显示花岗斑岩内星点状白钨矿颗粒（红色虚线圈为白钨矿原位微区微量元素分析所留下）；c—矿脉内荧光特征的大颗粒白钨矿（直径>1 cm）显示出复杂的黄色—蓝色荧光特征（阴极发光条件下）；d—白钨矿显示出生长环带特征（紫外灯下)
Figure 6. Representative images of different types of scheelite from the Yangchuling W–Mo deposit, Jiangxi Province (Xiong et al., 2025)
(a) Scheelite disseminated in monzogranite porphyry, showing blue fluorescence under ultraviolet (UV) light; (b) Backscattered electron image of disseminated, fine-grained scheelite coexisting with zircon, apatite, and K-feldspar in granite porphyry; the red circle represents the micro-area of in situ trace element analysis of scheelite; (c) A large scheelite grain (>1 cm in diameter) from an ore vein, showing complex yellow-to-blue cathodoluminescence; (d) Scheelite showing growth zoning under UV light
图 7 东源斑岩型W-Mo矿床成因模式图（据Dong et al., 2025a修改）
SchA—产于石英–钾长石脉中的白钨矿；SchB—产于石英–绢云母–钾长石脉中的白钨矿；SchC—最晚期白钨矿，穿切早期SchA和SchB；SchA、SchB和SchC及其相关脉体和矿化均产于斑状黑云母花岗岩中。Scha—产于石英–黑云母–白云母–黄铁矿–黄铜矿脉中的白钨矿；Schb—产于石英–白云母–斜长石–黝帘石–黄铁矿脉中的白钨矿；Scha和Schb及其相关脉体和矿化均产于煌斑岩中
Figure 7. Genetic model of the Dongyuan porphyry W–Mo deposit (modified after Dong et al., 2025a)
SchA denotes scheelite in quartz–K-feldspar veins, SchB denotes scheelite in quartz–sericite–K-feldspar veins, and SchC represents the latest-stage scheelite that crosscuts the earlier SchA and SchB; these scheelites and their associated veins and mineralization occur in porphyritic biotite granite. Scha denotes scheelite in quartz–biotite–muscovite–pyrite–chalcopyrite veins, whereas Schb denotes scheelite in quartz–muscovite–plagioclase–epidote–pyrite veins; these scheelites and their associated veins and mineralization occur in lamprophyre.
图 8 江南造山带W-Sn矿床花岗岩锆石U-Pb年龄−εHf（t）图
MMEs—暗色微粒包体；CHUR—球粒陨石均一储库朱溪矿床数据收集自Pan et al. （2018）；大湖塘矿床数据收集自Huang and Jiang （2014）；东源矿床数据收集自Zhang et al. （2021a）；阳储岭矿床数据收集自Song et al. （2023a）；香炉山矿床数据收集自Li et al. （2020）；西坞口矿床数据收集自陈雪峰等 （2019）
Figure 8. Zircon U-Pb age-εHf(t) diagram of W–Sn deposits in the Jiangnan Orogen
MMEs–mafic microgranular enclaves; CHUR–chondritic uniform reservoir Data for the following deposits are from the respective sources: Zhuxi deposit–Pan et al. (2018); Dahutang deposit–Huang and Jiang (2014); Dongyuan deposit–Zhang et al. (2021a); Yangchuling deposit–Song et al. (2023a); Xianglushan deposit–Li et al. (2020); Xiwukou deposit–Chen et al. (2019).
表 1 大湖塘W-Cu-Mo-Sn矿床中各类岩体定年结果
Table 1. Summary of geochronological data for various igneous rocks in the Dahutang W–Cu–Mo–Sn deposit
矿区 矿段 岩石/矿物类型 测试方法 成岩时代/Ma 数据来源 北部 石门寺 似斑状黑云母花岗岩 锆石U-Pb定年 147.4±0.6 Mao et al., 2015 北部 石门寺 似斑状黑云母花岗岩 锆石U-Pb定年 148.3±1.9 Mao et al., 2015 北部 石门寺 似斑状黑云母花岗岩 独居石U-Pb定年 150.0±0.7 叶海敏等, 2016 北部 石门寺 似斑状黑云母花岗岩 锆石U-Pb定年 147.7±7.9 李宏伟等, 2021 北部 石门寺 似斑状黑云母花岗岩 锆石U-Pb定年 138 项新葵等, 2012 北部 石门寺 细粒黑云母花岗岩 锆石U-Pb定年 146.1±0.6 Mao et al., 2015 北部 石门寺 细粒黑云母花岗岩 锆石U-Pb定年 144.7±0.5 Mao et al., 2015 北部 石门寺 细粒黑云母花岗岩 独居石U-Pb定年 149.0±1.0 叶海敏等, 2016 北部 石门寺 细粒二云母花岗岩 锆石U-Pb定年 146.6±1.4 张志辉, 2014 北部 石门寺 斑状黑云母花岗岩 锆石U-Pb定年 146.3±0.61 张志辉, 2014 北部 石门寺 白云母花岗岩 锆石U-Pb定年 146.42±0.49 张志辉, 2014 北部 石门寺 花岗斑岩 锆石U-Pb定年 146.0±0.78 项新葵等, 2015 北部 石门寺 花岗斑岩 锆石U-Pb定年 143.0±0.8 Mao et al., 2015 北部 石门寺 花岗斑岩 锆石U-Pb定年 143.1±1.2 Mao et al., 2015 北部 石门寺 花岗斑岩 锆石U-Pb定年 151.0±l.1 张志辉, 2014 北部 石门寺 花岗斑岩 独居石U-Pb定年 148.2±1.2 叶海敏等, 2016 北部 石门寺 花岗斑岩 锆石U-Pb定年 154.36±0.83 张志辉等，2020 北部 石门寺 花岗斑岩 锆石U-Pb定年 135 项新葵等, 2012 北部 大岭上 花岗斑岩 锆石U-Pb定年 130.4±1.6 彭花明等, 2015 北部 大岭上 中—细粒白云母花岗岩 锆石U-Pb定年 133.7±0.5 Huang and Jiang, 2014 北部 大岭上 细粒二云母花岗岩 锆石U-Pb定年 130.7±1.1 Huang and Jiang, 2014 中部 平苗 中—粗粒白云母花岗岩 锆石U-Pb定年 145.7±0.6 余振东等, 2020 中部 平苗 斑状二云母花岗岩 锆石U-Pb定年 146.4 Yang et al., 2022 中部 平苗 黑云母花岗斑岩 锆石U-Pb定年 143.4 Yang et al., 2022 中部 平苗 花岗斑岩 锆石U-Pb定年 149.1±1.1 孟亚飞和蒋少涌, 2015 中部 一矿带 花岗斑岩 锆石U-Pb定年 139.0±1.2 陈茂松等，2020 中部 一矿带 似斑状白云母花岗岩 白云母40Ar-39Ar定年 142.09±0.88 Song et al., 2018a 中部 一矿带 细粒白云母花岗岩 白云母40Ar-39Ar定年 138.79±1.75 Song et al., 2018a 中部 一矿带 细粒白云母花岗岩 白云母40Ar-39Ar定年 140.4±0.61 Song et al., 2018a 中部 一矿带 热液角砾岩型矿体中黑云母 黑云母40Ar-39Ar定年 149.2±1.1 Song et al., 2018a 中部 东陡崖 似斑状白云母花岗岩 锆石U-Pb定年 144.2±1.4 胡大龙，2023 中部 东陡崖 中—细粒白云母花岗岩 锆石U-Pb定年 133.6±1.6 胡大龙，2023 中部 槽头港 中—粗粒白云母花岗岩 锆石U-Pb定年 142.2±1.8 胡大龙，2023 中部 槽头港 斑状二云母花岗岩 锆石U-Pb定年 133.5±0.8 胡大龙，2023 中部 槽头港 似斑状黑云母花岗岩 锆石U-Pb定年 145.7±1.8 胡大龙，2023 南部 狮尾洞 似斑状白云母花岗岩 锆石U-Pb定年 144.2±1.3 黄兰椿和蒋少涌, 2012 南部 狮尾洞 似斑状二云母花岗岩 锆石U-Pb定年 144.0±0.6 Huang and Jiang, 2014 南部 狮尾洞 斑状二云母花岗岩 锆石U-Pb定年 130.3±1.1 Huang and Jiang, 2014 南部 狮尾洞 花岗斑岩 锆石U-Pb定年 134.6±1.2 黄兰椿和蒋少涌, 2013 南部 狮尾洞 黑云母花岗斑岩 锆石U-Pb定年 143.7±2.4 褚平利等，2019 南部 狮尾洞 细粒白云母花岗岩 白云母40Ar-39Ar定年 137.60±2.68 Song et al., 2018a 南部 昆山 似斑状花岗岩 锆石U-Pb定年 151.7±1.3 张明玉等，2016 南部 毛公洞 白云母花岗岩 锆石U-Pb定年 144.5±2.2 胡大龙，2023 
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表 2 大湖塘W-Cu-Mo-Sn矿床成矿年龄汇总
Table 2. Summary of mineralization ages of the Dahutang W–Cu–Mo–Sn deposit
序号 矿区 矿段 测试方法 成矿时代/ Ma 数据来源 1 北部 石门寺 辉钼矿Re-Os定年 143.7±1.2 丰成友等, 2012 2 北部 石门寺 辉钼矿Re-Os定年 149.6±1.4 项新葵等, 2013 3 北部 石门寺 辉钼矿Re-Os定年 139.2±1.0 Mao et al., 2013 4 北部 石门寺 辉钼矿Re-Os定年 143.9±1.0 张志辉, 2014 5 北部 石门寺 辉钼矿Re-Os定年 145.1±1.0 叶泽宇等, 2016 6 北部 石门寺 辉钼矿Re-Os定年 146.81±0.59 Song et al., 2018a 7 北部 石门寺 辉钼矿Re-Os定年 141.50±1.43 Song et al., 2018a 8 北部 石门寺 辉钼矿Re-Os定年 138.91±0.87 Song et al., 2018a 9 北部 石门寺 辉钼矿Re-Os定年 140.96±1.15 Song et al., 2018a 10 北部 石门寺 辉钼矿Re-Os定年 144.02±0.96 Song et al., 2018a 11 北部 石门寺 辉钼矿Re-Os定年 149.6±1.2 刘更更等，2024 12 北部 石门寺 辉钼矿Re-Os定年 139.18±0.97 刘更更等，2024 13 北部 石门寺 辉钼矿Re-Os定年 145.1±1.0 刘更更等，2024 14 北部 石门寺 辉钼矿Re-Os定年 140.6±1.2 刘更更等，2024 15 北部 石门寺 辉钼矿Re-Os定年 141.79±0.97 刘更更等，2024 16 北部 石门寺 辉钼矿Re-Os定年 140.6±1.2 叶泽宇等，2016 17 北部 石门寺 黑钨矿U-Pb定年 147.8±2.8 胡大龙，2023 18 北部 大岭上 黑钨矿U-Pb定年 131.7±3.5 胡大龙，2023 19 中部 一矿带 辉钼矿Re-Os定年 137.9±2.0 张勇等, 2017 20 中部 一矿带 黑钨矿U-Pb定年 149.8±3.0 胡大龙，2023 21 中部 一矿带 黑钨矿U-Pb定年 135.4±3.7 胡大龙，2023 22 中部 槽头港 黑钨矿U-Pb定年 135.3±4.8 胡大龙，2023 23 中部 东陡崖 锡石U-Pb定年 136.3±3.8 胡大龙，2023 24 中部 东陡崖 锡石U-Pb定年 145.7±7.6 胡大龙，2023 25 中部 东陡崖 锡石U-Pb定年 146.4±5.7 胡大龙，2023 26 中部 东陡崖 锡石U-Pb定年 144.5±5.9 胡大龙，2023 27 南部 狮尾洞 黑钨矿U-Pb定年 134.6±4.4 胡大龙，2023 28 南部 狮尾洞 白钨矿Sm-Nd定年 142.4±8.9 蒋少涌等，2015 29 南部 狮尾洞 白云母40Ar-39Ar定年 138.63±0.85 Song et al., 2018a 30 南部 狮尾洞 辉钼矿Re-Os定年 140.9±3.6 丰成友等, 2012 31 南部 狮尾洞 辉钼矿Re-Os定年 131.96±1.34 Song et al., 2018a 32 南部 狮尾洞 辉钼矿Re-Os定年 130.42±1.92 Song et al., 2018a 33 南部 狮尾洞 辉钼矿Re-Os定年 134.80±1.58 Song et al., 2018a 34 南部 狮尾洞 辉钼矿Re-Os定年 134.75±1.22 Song et al., 2018a 35 南部 狮尾洞 辉钼矿Re-Os定年 135.16±1.22 Song et al., 2018a 36 南部 狮尾洞 辉钼矿Re-Os定年 141.07±2.37 Song et al., 2018a 37 南部 狮尾洞 辉钼矿Re-Os定年 146.97±1.13 Song et al., 2018a 38 南部 昆山 辉钼矿Re-Os定年 151.0±1.3 张明玉等，2016 39 南部 昆山 辉钼矿Re-Os定年 150.0±1.0 张明玉等，2016 40 南部 昆山 辉钼矿Re-Os定年 148.7±0.7 林锐华等，2023
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