| 徐良易,刘建中,王泽鹏,李俊海,杨成富,李松涛,谢卓君,谭礼金,谭亲平,王大福,靳晓野,刘婧珂,李应辉,张兵强,万大学,陈发恩,李磊,何金坪,谭代卫,汪小勇.基于中国南方卡林型金矿多层次构造滑脱成矿系统的黔西南卡林型金矿找矿突破[J].矿产勘查,2026,17(8):1374-1397 |
| 基于中国南方卡林型金矿多层次构造滑脱成矿系统的黔西南卡林型金矿找矿突破 |
| Exploration breakthrough of Carlin-type gold deposits in Southwest Guizhou: Insights from the multi-level structural detachment metallogenic system in Southern China |
| 投稿时间:2026-05-21 |
| DOI:10.20008/j.kckc.202608007 |
| 中文关键词: 卡林型金矿 构造滑脱 构造蚀变体 找矿突破 黔西南 |
| 英文关键词: Carlin-type gold deposits structural detachment structural alteration body ore-prospectingbreakthrough southwestern of Guizhou Province |
| 基金项目:本文受国家重点研发计划项目“南盘江—右江地区金锑矿床找矿预测与勘查示范”课题(2023YFC2906804)、深地国家科技重大专项“滇黔桂毗连区锡锑金矿高效探测技术研发与应用”课题(2024ZD1001704)、自然资源部-科技创新团队“贵州省卡林型金矿成矿与找矿创新团队”(ZRC-TD2023006)、贵州省科技计划项目“贵州省金+玉矿探矿顶尖专家团队”(黔科合人才CXTD〔2025〕002)联合资助。 |
| 作者 | 单位 | | 徐良易 | 贵州大学资源与环境工程学院,贵州贵阳 550025 贵州省地质矿产勘查开发局 105地质大队,贵州贵阳 550018 | | 刘建中 | 贵州大学资源与环境工程学院,贵州贵阳 550025 贵州省地质矿产局,贵州贵阳 550018 贵州省地质调查院,贵州贵阳 550085 | | 王泽鹏 | 贵州省地质矿产勘查开发局 105地质大队,贵州贵阳 550018 | | 李俊海 | 贵州省地质矿产勘查开发局 105地质大队,贵州贵阳 550018 | | 杨成富 | 贵州省地质矿产勘查开发局 105地质大队,贵州贵阳 550018 | | 李松涛 | 贵州师范学院地理与资源学院,贵州贵阳 550018 | | 谢卓君 | 中国科学院地球化学研究所矿床地球化学国家重点实验室,贵州贵阳 550081 | | 谭礼金 | 贵州省地质矿产勘查开发局 105地质大队,贵州贵阳 550018 | | 谭亲平 | 中国科学院地球化学研究所矿床地球化学国家重点实验室,贵州贵阳 550081 | | 王大福 | 贵州大学资源与环境工程学院,贵州贵阳 550025 贵州省地质矿产勘查开发局 105地质大队,贵州贵阳 550018 | | 靳晓野 | 中国地质大学武汉资源学院,湖北武汉 430074 | | 刘婧珂 | 贵州省地质矿产勘查开发局 105地质大队,贵州贵阳 550018 | | 李应辉 | 贵州省地质矿产勘查开发局 105地质大队,贵州贵阳 550018 | | 张兵强 | 贵州大学资源与环境工程学院,贵州贵阳 550025 贵州省地质矿产勘查开发局 105地质大队,贵州贵阳 550018 | | 万大学 | 贵州省地质矿产勘查开发局 105地质大队,贵州贵阳 550018 | | 陈发恩 | 贵州省地质矿产勘查开发局 105地质大队,贵州贵阳 550018 | | 李磊 | 贵州省地质矿产勘查开发局 105地质大队,贵州贵阳 550018 | | 何金坪 | 贵州省地质矿产勘查开发局 105地质大队,贵州贵阳 550018 | | 谭代卫 | 贵州大学资源与环境工程学院,贵州贵阳 550025 贵州省地质矿产勘查开发局 105地质大队,贵州贵阳 550018 | | 汪小勇 | 贵州省地质矿产勘查开发局 105地质大队,贵州贵阳 550018 |
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| 中文摘要: |
| 南盘江—右江地区是中国卡林型金矿主要集中地,贵州黔西南卡林型金矿累计查明金资源量 742.46 t,是“滇—黔—桂”金三角重要组成部分。为实现南盘江—右江地区卡林型金矿找矿新突破,提出黔西南构造蚀变体(SBT)为区域卡林型金矿重要找矿标志,逐步完善区域构造蚀变体概念及判别指标。历经三十余年产学研结合,构建了以构造蚀变体为核心的与隐伏花岗岩有关的“中国南方卡林型金矿多层次构造滑脱成矿系统”为开展区域成矿与找矿预测提供理论指导。基于建立的成矿模式和找矿预测模型,团队发现和探明了 1个,超大型(水银洞)、3个特大型(紫木凼、泥堡、架底)、1个大型(者相),1个中型(大麦地)及多个小型金矿床,取得了黔西南地区中、上二叠统茅口组和龙潭组或峨眉山玄武岩组间滑脱构造的灰家堡金矿田、泥堡金矿田、架底金矿田找矿突破。 |
| 英文摘要: |
| The Nanpanjiang-Youjiang region is a major concentration area of Carlin-type gold deposits inChina. Among these, the Carlin-type gold deposits in southwestern Guizhou stand out as the most significant compo.nent of the "Yunnan-Guizhou-Guangxi" Golden Triangle, with a cumulative identified gold resource of 742.46tons. The structural alteration body (SBT) in southwestern Guizhou has become a key prospecting indicator for re.gional Carlin-type gold deposits. Its definition has been progressively refined, and corresponding diagnostic criteriahave been established, providing a theoretical foundation for achieving new breakthroughs in Carlin-type gold pros.pecting in the Nanpanjiang-Youjiang region. Following over three decades of integration among industry, academia,and research, we have developed the "multi-level structural detachment metallogenic system of Carlin-type gold de.posits in South China", which centers on the SBT and is associated with concealed granite. This system providestheoretical support for further research on regional metallogeny and mineral exploration. Based on the establishedmetallogenic model and exploration prediction methods, we have successfully discovered one super-large (Shuiyin.dong), three extra-large (Zimudang, Nibao, Jiadi), one large (Zhexiang), one medium (Damaidi), and several smallCarlin-type gold deposits. These achievements have led to ore-prospecting breakthroughs in the Huijiabao, Nibao,and Jiadi gold ore fields, which are located in the detachment structures between the Middle-Upper Permian Ma.okou Formation and the Longtan Formation or the Emeishan Basalt Formation in southwestern Guizhou. |
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