滇东南个旧-麻栗坡矿集区多期次锡钨成矿作用

李文昌 ,  杨富成 ,  江小均 ,  刘学龙 ,  邓明国 ,  徐忠彪 ,  韩嶂 ,  陆波德

成都理工大学学报(自然科学版) ›› 2026, Vol. 53 ›› Issue (4) : 757 -773.

PDF (3248KB)
成都理工大学学报(自然科学版) ›› 2026, Vol. 53 ›› Issue (4) : 757 -773. DOI: 10.12474/cdlgzrkx.2026052501
成都理工大学70周年校庆专刊

滇东南个旧-麻栗坡矿集区多期次锡钨成矿作用

作者信息 +

Multistage tin and tungsten mineralization in the Gejiu−Malipo ore district, southeast Yunnan

Author information +
文章历史 +
PDF (3325K)

摘要

滇东南个旧-麻栗坡矿集区位于特提斯与环太平洋成矿域交汇部位,隶属于华南板块西南缘。区内围绕个旧、薄竹山、老君山岩体周缘发育世界级锡钨多金属矿床,长期备受关注。本文在前人研究成果基础上,对该区多期多类型锡钨多金属成矿作用开展了研究,对晚白垩世岩浆流体成矿系统进行了总结,取得以下新认识:(1)厘定东南麻栗坡地区发育四期锡钨成矿作用(437~411 Ma、230~203 Ma、160~140 Ma 和 97~79 Ma),而向北西薄竹山-个旧地区则过渡为以晚白垩世岩浆成矿作用(91~76 Ma)为主;(2)晚白垩世成矿岩浆源于古陆边缘富含锡钨多金属成矿元素的古-中元古代变沉积岩的部分熔融;(3)个旧、薄竹山、麻栗坡矿集区发育相似的岩浆穹隆成矿系统,完整的成矿系统包括岩体内发育云英岩型锡钨矿,接触带发育矽卡岩锡钨铜矿,向外依次发育锡钨铅锌银矿、铅锌银矿和银矿;(4)物源及流体演化过程的差异控制了个旧、薄竹山、麻栗坡地区的不同矿化组合。鉴于此,本文构建了多期次、多层位复合成矿模式及晚白垩世岩浆流体成矿系统模型,为区域找矿勘查提供科学指导。

Abstract

The Gejiu−Malipo ore district in southeast Yunnan is located at the junction of the Tethyan and Circum-Pacific metallogenic domains, belonging to the southwestern margin of the South China Block. The area hosts world-class extra-large deposits developed around the Gejiu, Bozhushan, and Laojunshan granitic intrusions, and has long attracted significant research attention. Based on previous studies, this paper investigates multistage and multi-type Sn-W polymetallic mineralization in the region and develops a model of the Late Cretaceous Epoch magmatic-hydrothermal ore-forming system. The following new insights have been obtained: (1) Four episodes of Sn-W mineralization (437–411 Ma, 230–203 Ma, 160–140 Ma, and 97–76 Ma) are identified in the southeastern Malipo area, whereas northwestward into the Bozhushan–Gejiu area, the mineralization transitions to being dominated by Late Cretaceous Epoch magmatic processes. (2) The Late Cretaceous Epoch ore-forming magma originated from partial melting of Paleo- to Mesoproterozoic metasedimentary rocks enriched in Sn-W polymetallic elements along the passive margin of an ancient continent. (3) Similar magmatic dome-related metallogenic systems developed in the Gejiu, Bozhushan, and Malipo ore district, a complete system which includes greisen-type Sn-W deposits within the intrusion, skarn-type Sn-W-Cu deposits along the contact zone, and outward succession of Sn-W-Pb-Zn-Ag deposits, Pb-Zn-Ag deposits, and Ag deposits. (4) Finally, differences in metal sources and fluid evolution processes control the distinct mineral assemblages in the Gejiu, Bozhushan, and Laojunshan areas. Accordingly, this paper establishes a multistage, multi-layer composite metallogenic model and a Late Cretaceous Epoch magmatic-hydrothermal ore-forming system model, providing scientific guidance for regional mineral exploration and prospecting.

关键词

个旧-麻栗坡矿集区 / 锡钨多金属矿床 / 成矿源区 / 多期流体成矿系统

Key words

Gejiu−Malipo ore district / Sn-W polymetallic deposit / ore-forming source area / multi-stage ore-forming fluid system

引用本文

引用格式 ▾
李文昌,杨富成,江小均,刘学龙,邓明国,徐忠彪,韩嶂,陆波德. 滇东南个旧-麻栗坡矿集区多期次锡钨成矿作用[J]. 成都理工大学学报(自然科学版), 2026, 53(4): 757-773 DOI:10.12474/cdlgzrkx.2026052501

登录浏览全文

4963

注册一个新账户 忘记密码

参考文献

[1]

白浩, 2021. 滇东南老君山南捞钨铜矿床地质特征及成因探讨[D]. 北京: 中国地质大学(北京): 1-61.

[2]

Bai H, 2021. Geological characteristics and origin discussion of the Nanlao W-Cu deposit in Laojunshan,SE Yunnan[D]. Beijing: China University of Geosciences (Beijing): 1-61. (in Chinese)

[3]

曹原, 2022. 滇东南白牛厂银多金属矿床中闪锌矿稀散元素的超常富集机制[D]. 昆明: 云南大学: 1-67.

[4]

Cao Y, 2022. The super-enrichment mechanism of spersed elements in sphalerite in Bainiuchang silver polymetallic deposit in southeast Yunnan[D]. Kunming:Yunnan University: 1-67. (in Chinese)

[5]

陈世垒, 李超, 江小均, 等, 2025. 岩浆源区和分异演化对锡成矿作用限制:来自个旧锡矿集区花岗杂岩体斜长石地球化学证据[J/OL]. 矿物学报, 2025-09-18. https://link.cnki.net/urlid/52.1045.p.20250916.2350.001.

[6]

Chen S L, Li C, Jiang X J, et al., 2025. Constraints of the sources and crystallization diffrentiation evolution of magmas on the tin metallogenesis:evidences from geochemical characteristics of plagioclases in granites of the Gejiu tin deposit[J/OL]. Acta Mineralogica Sinica, 2025-09-18. https://link.cnki.net/urlid/52.1045.p.20250916.2350.001.(in Chinese)

[7]

陈智明, 王大鹏, 李山志, 2018. 滇东南南捞铜钨矿床 S-Pb 同位素特征[J]. 矿物学报, 38(2): 196-204.

[8]

Chen Z M, Wang D P, Li S Z, 2018. Sulfur and lead isotopic geochemistry of Nanlao Cu-W deposit in southeastern Yunnan Province,China[J]. Acta Mineralogica Sinica, 38(2): 196-204. (in Chinese)

[9]

邓军, 王庆飞, 陈福川, 等, 2020. 再论三江特提斯复合成矿系统[J]. 地学前缘, 27(2): 106-136.

[10]

Deng J, Wang Q F, Chen F C, et al., 2020. Further discussion on the Sanjiang Tethyan composite metallogenic system[J]. Earth Science Frontiers, 27(2): 106-136. (in Chinese)

[11]

杜胜江, 温汉捷, 张锦让, 等, 2022. 滇东南老君山矿集区马卡钨铍稀有金属矿床花岗岩年代学归属[J]. 矿物学报, 42(3): 257-269.

[12]

Du S J, Wen H J, Zhang J R, et al., 2022. A study on isotopic chronology of granites in the Maka W-Be polymetallic deposit of the Laojunshan ore-concentrated district,SE Yunnan,China[J]. Acta Mineralogica Sinica, 42(3): 257-269. (in Chinese)

[13]

何芳, 张乾, 王大鹏, 等, 2014. 云南都龙 Sn-Zn 多金属矿床成矿物质来源——硫、碳、氧稳定同位素证据[J]. 矿物岩石地球化学通报, 33(6): 900-907.

[14]

He F, Zhang Q, Wang D P, et al., 2014. Ore-forming material sources of the Dulong Sn-Zn polymetallic deposit,Yunnan:evidence from stable S-C-O isotopes[J]. Bulletin of Mineralogy,Petrology and Geochemistry, 33(6): 900-907. (in Chinese)

[15]

蹇龙, 2016. 云南蒙自白牛厂超大型银多金属矿床叠加成矿系统及成矿模式[D]. 昆明: 昆明理工大学: 1-226.

[16]

Jian L, 2016. Superimposed mineralization system and metallogenic model of Bainiuchang super large polymetallic deposits,southeastern Yunnan,China[D]. Kunming: Kunming University of Science and Technology: 1-226. (in Chinese)

[17]

蒋少涌, 赵葵东, 姜海, 等, 2020. 中国钨锡矿床时空分布规律、地质特征与成矿机制研究进展[J]. 科学通报, 65(33): 3730-3745.

[18]

Jiang S Y, Zhao K D, Jiang H, et al., 2020. Spatiotemporal distribution,geological characteristics and metallogenic mechanism of tungsten and tin deposits in China:an overview[J]. Chinese Science Bulletin, 65(33): 3730-3745. (in Chinese)

[19]

李开文, 张恺, 郭君功, 等, 2018. 云南白牛厂银多金属矿床硫同位素组成及滇东南多金属矿找矿远景[J]. 金属矿山,(10): 138-140.

[20]

Li K W, Zhang K, Guo J G, et al., 2018. Sulfur isotopic composition of Bainiuchang Ag-polymetallic deposit and the prospecting prospective for polymetallic deposit of southern Yunnan Province[J]. Metal Mine,(10): 138-140. (in Chinese)

[21]

李开文, 张乾, 王大鹏, 等, 2013. 云南蒙自白牛厂多金属矿床锡石原位 LA-MC-ICP-MS U-Pb 年代学[J]. 矿物学报, 33(2): 203-209.

[22]

Li K W, Zhang Q, Wang D P, et al., 2013. LA-MC-ICP-MS U-Pb geochronology of cassiterite from the Bainiuchang polymetallic deposit,Yunnan Province,China[J]. Acta Mineralogica Sinica, 33(2): 203-209. (in Chinese)

[23]

李睿昱, 覃小锋, 王宗起, 等, 2024. 滇东南板仑磁铁矿集区矽卡岩矿物学、地球化学特征及其形成机制[J]. 岩石学报, 40(4): 1205-1230.

[24]

Li R Y, Qin X F, Wang Z Q, et al., 2024. Mineralogical,geochemical characteristics and formation mechanism of skarns in Banlun magnetite ore cluster area,southeastern Yunnan[J]. Acta Petrologica Sinica, 40(4): 1205-1230. (in Chinese)

[25]

李晓波, 2005. 云南省蒙自县白牛厂银多金属矿床成矿地质特征及成矿模式[D]. 长沙: 中南大学: 1-90.

[26]

Li X B, 2005. The ore-forming geological features and metallogenic pattern of Bainiuchang poly-metal deposit in Mengzi County,Yunnan Province[D]. Changsha: Central South University: 1-90. (in Chinese)

[27]

李正荣, 邓明国, 陈应华, 等, 2026. 滇东南长田白钨−萤石矿床成因:来自金红石 U-Pb 定年和黄铁矿原位硫同位素制约[J]. 矿物学报, 46(2): 185-199.

[28]

Li Z R, Deng M G, Chen Y H, et al., 2026. The genesis of the Changtian scheelite-fluorite deposit in the southeastern Yunnan:constraints from the rutile U-Pb dating data and in-situ sulfur isotopes of pyrites[J]. Acta Mineralogica Sinica, 46(2): 185-199. (in Chinese)

[29]

刘明军, 杨光树, 陈爱兵, 等, 2023. 滇东南马卡铅锌钨矿床成因:闪锌矿 Rb-Sr、锡石 U-Pb 定年和硫化物原位硫、铅同位素制约[J]. 岩石学报, 39(6): 1861-1879.

[30]

Liu M J, Yang G S, Chen A B, et al., 2023. Genesis of the Maka Pb-Zn-W deposit in southeastern Yunnan:constraints from sphalerite Rb-Sr dating,cassiterite U-Pb dating and in-situ S,Pb isotopes of sulfide[J]. Acta Petrologica Sinica, 39(6): 1861-1879. (in Chinese)

[31]

刘学龙, 李文昌, 张世涛, 等, 2024. 滇东南薄竹山矿集区晚白垩世岩浆活动及锡银铅锌钨多金属成矿作用[J]. 沉积与特提斯地质, 44(2): 437-453.

[32]

Liu X L, Li W C, Zhang S T, et al., 2024. The Late Cretaceous magmatism and Sn-Ag-Pb-Zn-W polymetallic mineralization in Bozhushan ore concentration area,southeast Yunnan[J]. Sedimentary Geology and Tethyan Geology, 44(2): 437-453. (in Chinese)

[33]

刘益, 孔志岗, 陈港, 等, 2021. 滇东南官房钨矿床石榴子石原位 LA-SF-ICP-MS U-Pb 定年及地质意义[J]. 岩石学报, 37(3): 847-864.

[34]

Liu Y, Kong Z G, Chen G, et al., 2021. In-situ LA-SF-ICP-MS U-Pb dating of garnet from Guanfang tungsten deposit in southeastern Yunnan Province and its geological significance[J]. Acta Petrologica Sinica, 37(3): 847-864. (in Chinese)

[35]

刘玉平, 李朝阳, 谷团, 等, 2000. 都龙锡锌多金属矿床成矿物质来源的同位素示踪[J]. 地质地球化学, 28(4): 75-82.

[36]

Liu Y P, Li C Y, Gu T, et al., 2000. Isotopic constraints on the source of ore-forming materials of Dulong Sn-Zn polymetallic dsposit,Yunnan[J]. Geology-Geochemistry, 28(4): 75-82. (in Chinese)

[37]

刘忠, 曹淑云, 董彦龙, 等, 2022. 滇东南老君山片麻岩穹窿变形构造与剥露过程[J]. 中国科学:地球科学, 52(1): 53-80.

[38]

Liu Z, Cao S Y, Dong Y L, et al., 2021. Deformation structure and exhumation process of the Laojunshan gneiss dome in southeastern Yunnan of China[J]. Science China Earth Sciences, 64(12): 2190-2216.

[39]

毛景文, 程彦博, 郭春丽, 等, 2008. 云南个旧锡矿田:矿床模型及若干问题讨论[J]. 地质学报, 82(11): 1455-1467.

[40]

Mao J W, Cheng Y B, Guo C L, et al., 2008. Gejiu tin polymetallic ore-field:deposit model and discussion for several points concerned[J]. Acta Geologica Sinica, 82(11): 1455-1467. (in Chinese)

[41]

米雪, 2025. 滇东南白牛厂银铅锌多金属矿床岩浆活动及成矿作用研究[D]. 昆明: 昆明理工大学: 1-98.

[42]

Mi X, 2025. Study on magmatic activity and mineralization of the Bainiuchang silver-lead-zinc polymetallic deposit in southeastern Yunnan[D]. Kunming: Kunming University of Science and Technology: 1-98. (in Chinese)

[43]

阙朝阳, 2016. 云南麻栗坡南温河-洒西一带钨成矿系统及找矿方向研究[D]. 北京: 中国地质大学(北京): 1-233.

[44]

Que C Y, 2016. Tungsten metallogenic system and prospecting direction in the Nanwenhe-Saxi area,Malipo County,Yunnan Province[D]. Beijing: China University of Geosciences (Beijing): 1-233. (in Chinese)

[45]

盛夏, 张达, 阙朝阳, 等, 2023. 滇东南洒西钨铍矿床成矿流体来源和演化:来自流体包裹体和 H-O 同位素证据[J]. 地质科技通报, 42(1): 158-169.

[46]

Sheng X, Zhang D, Que C Y, et al., 2023. Sources and evolution of ore-forming fluids from the Saxi tungsten-beryllium deposit in southeastern Yunnan Province:evidence from fluid inclusions and H-O isotopes[J]. Bulletin of Geological Science and Technology, 42(1): 158-169. (in Chinese)

[47]

王安建, 李建武, 刘固望, 等, 2025. 全球矿产资源形势报告[R]. 北京: 中国地质科学院全球矿产资源战略研究中心.

[48]

Wang A J, Li J W, Liu G W, et al., 2025. Report on the global mineral resources situation[R]. Beijing:Global Mineral Resources Strategy Research Center,Chinese Academy of Geological Sciences. (in Chinese)

[49]

王彩艳, 任涛, 王蝶, 等, 2020. 滇东南南秧田超大型钨矿床流体包裹体及 H、O 同位素研究[J]. 大地构造与成矿学, 44(1): 103-118.

[50]

Wang C Y, Ren T, Wang D, et al., 2020. Fluid inclusion and hydrogen-oxygen isotope study of the Nanyangtian super large tungsten deposit,southeastern Yunnan Province[J]. Geotectonica et Metallogenia, 44(1): 103-118. (in Chinese)

[51]

王小娟, 刘玉平, 缪应理, 等, 2014. 都龙锡锌多金属矿床 LA-MC-ICP-MS 锡石 U-Pb 测年及其意义[J]. 岩石学报, 30(3): 867-876.

[52]

Wang X J, Liu Y P, Miao Y L, et al., 2014. In-situ LA-MC-ICP-MS cassiterite U-Pb dating of Dulong Sn-Zn polymetallic deposit and its significance[J]. Acta Petrologica Sinica, 30(3): 867-876. (in Chinese)

[53]

王忠强, 李超, 张定才, 等, 2020. 滇东南南秧田钨矿床白钨矿原位 Sr 同位素对成矿的指示[J]. 岩矿测试, 39(2): 285-299.

[54]

Wang Z Q, Li C, Zhang D C, et al., 2020. Implication of in situ Sr isotope of scheelite for tungsten mineralization:a case study of the Nanyangtian scheelite deposit,southeast Yunnan,China [J]. Rock and Mineral Analysis, 39(2): 285-299. (in Chinese)

[55]

许赛华, 任涛, 白鑫, 等, 2022. 滇东南都龙 Sn-Zn 多金属矿床交生硫化物微区主量元素、硫同位素特征及成因研究[J]. 矿床地质, 41(4): 741-750.

[56]

Xu S H, Ren T, Bai X, et al., 2022. In-situ major elements and sulfur isotope analysis of intergrowth sulfide in Dulong Sn-Zn polymetallic deposit,SE Yunnan and study on their genesis[J]. Mineral Deposits, 41(4): 741-750. (in Chinese)

[57]

张洪培, 2007. 云南蒙自白牛厂银多金属矿床——与花岗质岩浆作用有关的超大型矿床[D]. 长沙: 中南大学: 1-162.

[58]

Zhang H P, 2007. Bainiuchang super-large silver-polymetallic ore deposit related to granitic magmatism in Mengzi,Yunnan,China[D]. Changsha:Central South University: 1-162. (in Chinese)

[59]

张娟, 毛景文, 程彦博, 等, 2012. 个旧卡房层状铜矿床金云母和云英岩化白云母 40Ar-39Ar 同位素年龄及意义 [J]. 矿床地质, 31(6): 1149-1162.

[60]

Zhang J, Mao J W, Cheng Y B, et al., 2012. 40Ar-39Ar phlogopite dating of stratified ore body and muscovite dating of greisens from Xinshan granite intrusion of Kafang tin-copper deposit in Gejiu area,Yunnan Province[J]. Mineral Deposits, 31(6): 1149-1162. (in Chinese)

[61]

张庆鸽, 赵晓瑜, 邓明国, 等, 2025. 滇东南南秧田钨矿床成因:来自硫化物原位微量元素及硫同位素证据[J]. 矿物岩石地球化学通报, 44(3): 646-661.

[62]

Zhang Q G, Zhao X Y, Deng M G, et al., 2025. Genesis of the Nanyangtian W deposit in southeastern Yunnan:evidences from in situ analyses of trace element and sulfur isotope in sulfides[J]. Bulletin of Mineralogy,Petrology and Geochemistry, 44(3): 646-661. (in Chinese)

[63]

Carter A, Clift P D, 2008. Was the Indosinian orogeny a Triassic mountain building or a thermotectonic reactivation event?[J]. Comptes Rendus Géoscience, 340(2/3): 83-93.

[64]

Chen Y H, Li W C, Lan T G, et al., 2025. Two magmatic-hydrothermal events in Xinzhai Sn polymetallic deposit,Yunnan Province,China:constraints from cassiterite U-Pb geochronology and elemental compositions of single fluid inclusions[J]. Gondwana Research, 144: 123-150.

[65]

Cheng Y B, Mao J W, Liu P, 2016. Geodynamic setting of Late Cretaceous Sn-W mineralization in southeastern Yunnan and northeastern Vietnam[J]. Solid Earth Sciences, 1(3): 79-88.

[66]

Cheng Y B, Mao J W, Rusk B, et al., 2012. Geology and genesis of Kafang Cu-Sn deposit,Gejiu district,SW China[J]. Ore Geology Reviews, 48: 180-196.

[67]

Cheng Y B, Mao J W, Spandler C, 2013. Petrogenesis and geodynamic implications of the Gejiu igneous complex in the western Cathaysia block,South China[J]. Lithos, 175/176: 213-229.

[68]

Cheng Y B, Spandler C, Kemp A, et al., 2019. Controls on cassiterite (SnO2) crystallization:evidence from cathodoluminescence,trace-element chemistry,and geochronology at the Gejiu tin district [J]. American Mineralogist, 104(1): 118-129.

[69]

Du S J, Wen H J, Liu S R, et al., 2020. Mineralogy and metallogenesis of the Sanbao Mn-Ag (Zn-Pb) deposit in the Laojunshan ore district,SE Yunnan Province,China[J]. Minerals, 10(8): 650.

[70]

Gilley L D, Harrison T M, Leloup P H, et al., 2003. Direct dating of left-lateral deformation along the Red River shear zone,China and Vietnam[J]. Journal of Geophysical Research:Solid Earth, 108(B2): 2127.

[71]

Guo J, Zhang R Q, Li C Y, et al., 2018. Genesis of the Gaosong Sn-Cu deposit,Gejiu district,SW China:constraints from in situ LA-ICP-MS cassiterite U-Pb dating and trace element fingerprinting [J]. Ore Geology Reviews, 92: 627-642.

[72]

Han Z, Li C, Chen Y K, et al., 2025. Trace element geochemistry and Sr-Nd isotopic characteristics of scheelite from the Gejiu Sn-Cu-(W) ore district:constraints on tungsten sources and evolution of W-bearing hydrothermal fluids[J]. Acta Geologica Sinica (English Edition), 99(4): 1093-1104.

[73]

Lai J H, Chen Y H, Deng M G, et al., 2026. In-situ texture and geochemistry of scheelite from the Maka W polymetallic deposit:implications for late Yanshanian W metallogeny in southeastern Yunnan Province,China[J/OL]. Acta Geochimica, 2026-04-10. https://link.springer.com/article/10.1007/s11631-026-00866-2.

[74]

Li W B, Deng M G, Weng Q, et al., 2025. Arsenopyrite reveals the deuteric origin of the Saxi tungsten deposit,SW China[J]. Acta Geochimica, 44(6): 1276-1292.

[75]

Liao S L, Chen S Y, Deng X H, et al., 2014. Fluid inclusion characteristics and geological significance of the Xi’ao copper-tin polymetallic deposit in Gejiu,Yunnan Province[J]. Journal of Asian Earth Sciences, 79: 455-467.

[76]

Liu S Y, Liu Y P, Ye L, et al., 2021. Genesis of Dulong Sn-Zn-in polymetallic deposit in Yunnan Province,South China:insights from cassiterite U-Pb ages and trace element compositions[J]. Minerals, 11(2): 199.

[77]

Liu Y B, Dong G C, Santosh M, et al., 2025. Two phases of high potassic-shoshonitic magmatism and coeval Sn polymetallic mineralization in the Bozhushan orefield,Southwestern China[J]. Geoscience Frontiers, 16(6): 102157.

[78]

Liu Y B, Zhang L F, Mo X X, et al., 2020. The giant tin polymetallic mineralization in Southwest China:integrated geochemical and isotopic constraints and implications for Cretaceous tectonomagmatic event[J]. Geoscience Frontiers, 11(5): 1593-1608.

[79]

Liu Y B, Zhang L F, Santosh M, et al., 2023. Multi-stage metallogeny in the southwestern part of South China,and paleotectonic and climatic implications:a high precision geochronologic study[J]. Geoscience Frontiers, 14(3): 101536.

[80]

Lu B D, Li W C, Liu X L, et al., 2024. U-Pb dating of monazite in the Bainiuchang silver polymetallic deposit,Yunnan Province,and its limitation on Mesozoic mineralization[J]. China Geology, 7(3): 592-595.

[81]

Maluski H, Lepvrier C, Jolivet L, et al., 2001. Ar-Ar and fission-track ages in the Song Chay Massif:early Triassic and Cenozoic tectonics in northern Vietnam[J]. Journal of Asian Earth Sciences, 19(1/2): 233-248.

[82]

Mao J W, Ouyang H G, Song S W, et al., 2019. Geology and metallogeny of tungsten and tin deposits in China[M]//Chang Z S,Goldfarb R J. Mineral deposits of China. Litteton:Society of Economic Geologists,Special Publication: 411-482.

[83]

Ni P, Pan J Y, Han L, et al., 2023. Tungsten and tin deposits in South China:temporal and spatial distribution,metallogenic models and prospecting directions[J]. Ore Geology Reviews, 157: 105453.

[84]

Ren T, Zhang Q, Wang C Y, et al., 2024. Fluid inclusions and H-O isotopes of the super-large Nanyangtian tungsten deposit in southeastern Yunnan,southwestern China[J]. Journal of Geochemical Exploration, 267: 107593.

[85]

Romer R L, Hahne K, 2010. Life of the Rheic Ocean:scrolling through the shale record[J]. Gondwana Research, 17(2/3): 236-253.

[86]

Romer R L, Kroner U, 2016. Phanerozoic tin and tungsten mineralization-tectonic controls on the distribution of enriched protoliths and heat sources for crustal melting[J]. Gondwana Research, 31: 60-95.

[87]

Romer R L, Kroner U, 2022. Provenance control on the distribution of endogenic Sn-W,Au,and U mineralization within the Gondwana-Laurussia plate boundary zone[M]//Kuiper Y D,Murphy J B,Nance R D, et al. New developments in the Appalachian-Caledonian-Variscan orogen. Boulder:Geological Society of America: 25-46.

[88]

Sun B, Liu Y, Kong Z G, et al., 2025. Multiple-stage W mineralization in the Guanfang W deposit,southeastern Yunnan Province,China:insights from scheelite in-situ trace elemental and Sr isotopic analyses [J]. Acta Geochimica, 44(1): 112-127.

[89]

Sun X, Xu H C, Yang Z M, et al., 2026. Crustal recycling and metamorphic dehydration govern the fertility of granite-associated tin systems[J]. Communications Earth & Environment, 7(1): 381.

[90]

Tang Z C, Zhao X Y, Deng M G, et al., 2026. Scheelite geochemistry constrains the origin of W mineralization in the Laojunshan district,southeast Yunnnan,China:comparative studies from the Nanyangtian,Changtian and Saxi deposits[J]. Ore Geology Reviews, 190: 107179.

[91]

Wang C Y, Han R S, Huang J G, et al., 2019. The 40Ar-39Ar dating of biotite in ore veins and zircon U-Pb dating of porphyrtic granite dyke in the Nanyangtian tungsten deposit in SE Yunnan,China[J]. Ore Geology Reviews, 114: 103133.

[92]

Wang T, Liu X L, Zhang S T, et al., 2025. Petrographic and geochemical evidence from pyrite for the genesis of the Bainiuchang Ag-polymetallic deposit southeastern Yunnan[J]. Scientific Reports, 15(1): 39247.

[93]

Wolf M, Romer R L, Franz L, et al., 2018. Tin in granitic melts:the role of melting temperature and protolith composition[J]. Lithos, 310/311: 20-30.

[94]

Xie H J, Zhu C H, Zhang Q, et al., 2009. Sulfur isotopic composition of the Bainiuchang super-large Ag polymetallic deposit,Yunnan Province,China:implications for the source of sulfur in ore-forming fluids[J]. Chinese Journal of Geochemistry, 28(3): 284-292.

[95]

Xu R, Romer R L, Glodny J, 2021. External fluids cause alteration and metal redistribution in the granite-hosted Tangziwa Sn-Cu deposit,Gejiu district,China[J]. Lithos, 382/383: 105937.

[96]

Xu Z B, Li W C, Yang F C, et al., 2025. Late Cretaceous Sn-W mineralization along the northeastern margin of the Laojunshan granite complex in the southeastern Yunnan Sn-W Belt,SW China[J]. Ore Geology Reviews, 186: 106928.

[97]

Yan D P, Zhou M F, Wang C Y, et al., 2006. Structural and geochronological constraints on the tectonic evolution of the Dulong−Song Chay tectonic dome in Yunnan Province,SW China[J]. Journal of Asian Earth Sciences, 28(4/5/6): 332-353.

[98]

Yang F C, Romer R L, Jiang X J, et al., 2025. Recurrent granite-related mineralization along former Tethys sutures in South-Western China[J]. Ore Geology Reviews, 180: 106584.

[99]

Yang F C, Romer R L, Li W C, et al., 2026. Former long-lived passive margins-cradles for major Sn,W,and Au provinces[J]. Ore Geology Reviews, 193: 107316.

[100]

Yang G S, Wen H J, Ren T, et al., 2020. Geochronology,geochemistry and Hf isotopic composition of Late Cretaceous Laojunshan granites in the western Cathaysia block of South China and their metallogenic and tectonic implications[J]. Ore Geology Reviews, 117: 103297.

[101]

Yuan S D, Williams-Jones A E, Romer R L, et al., 2019. Protolith-related thermal controls on the decoupling of Sn and W in Sn-W metallogenic provinces:insights from the Nanling region,China[J]. Economic Geology, 114(5): 1005-1012.

[102]

Zhang J W, Dai C G, Huang Z L, et al., 2015. Age and petrogenesis of Anisian magnesian alkali basalts and their genetic association with the Kafang stratiform Cu deposit in the Gejiu supergiant tin-polymetallic district,SW China[J]. Ore Geology Reviews, 69: 403-416.

[103]

Zhang Y H, Zhang S T, Tan S C, et al., 2016. The genetic relationship between the Large Guanfang W deposit and granitic intrusions,in Yunnan Province,southwest China:evidence from U-Pb and Re-Os geochronology and Pb and Sr isotopic characteristics[J]. Ore Geology Reviews, 79: 332-345.

[104]

Zhang Y H, Zhou J X, Tan S C, et al., 2020. Genesis of the oxidized Sn ores in the Gejiu district,Yunnan Province,SW China[J]. Ore Geology Reviews, 121: 103474.

[105]

Zhang Y H, Zhou J X, Tan S C, et al., 2022. New insights into the petrogenesis of the Bozhushan W-Sn mineralization-associated granites,Yunnan Province,SW China:evidence of microgranitoid enclaves[J]. Ore Geology Reviews, 145: 104906.

[106]

Zhang Z, Yang J H, Hu R Z, et al., 2024. Constraints of in-Situ elemental compositions and U-Pb ages of cassiterite on the origin of the Cretaceous Gejiu and Dulong tin deposits,SW China:implications for the linkage of tin belts in SE Asia[J]. Lithos, 488/489: 107832.

[107]

Zhao P L, Chu X, Williams-Jones A E, et al., 2022. The role of phyllosilicate partial melting in segregating tungsten and tin deposits in W-Sn metallogenic provinces[J]. Geology, 50(1): 121-125.

[108]

Zhao X Y, Deng M G, Li W C, et al., 2024. In situ U-Pb dating of garnet,vesuvianite,and scheelite from the Nanyangtian tungsten deposit reveals an Early Cretaceous W mineralization event in southeast Yunnan,China[J]. Gondwana Research, 133: 72-90.

[109]

Zhu J, Tan S C, Yang J Y, et al., 2024. What controls Sn-W mineralization in granite batholith:a case study from the world-class Dulong Sn-Zn polymetallic ore deposit of SW China[J]. Ore Geology Reviews, 166: 105968.

基金资助

云南省科技厅重大科技专项计划(202202AG050006)

深地国家科技重大专项(2024ZD1001702)

云南省科技厅高层次科技人才及创新团队选拔专项(202305AT350004,202205AS350015)

AI Summary AI Mindmap
PDF (3248KB)

5

访问

0

被引

详细

导航
相关文章

AI思维导图

/

〈 〉