| 贵州松桃高地隐伏超大型锰矿床主要特征与找矿实践 |
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| 引用本文： | 袁良军,周琦,潘文,姚希财,陈甲才,田景江,沈红钱,谢小峰,张仁彪,谢兴友,郑超,覃永军.贵州松桃高地隐伏超大型锰矿床主要特征与找矿实践[J].贵州地质,2019,36(3):197-206. |
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| 作者姓名： | 袁良军 周琦 潘文 姚希财 陈甲才 田景江 沈红钱 谢小峰 张仁彪 谢兴友 郑超 覃永军 |
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| 作者单位： | 自然资源部基岩区矿产资源勘查工程创新中心,贵阳550003;贵州省地质矿产勘查开发局103地质大队,铜仁554300;贵州省锰矿资源预测评价科技创新人才团队;自然资源部基岩区矿产资源勘查工程创新中心,贵阳550003;贵州省锰矿资源预测评价科技创新人才团队;自然资源部基岩区矿产资源勘查工程创新中心,贵阳550003;贵州省地质矿产勘查开发局103地质大队,铜仁554300;贵州省锰矿资源预测评价科技创新人才团队;中国地质大学地球科学学院,湖北武汉430074;贵州省地质矿产勘查开发局103地质大队,铜仁,554300 |
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| 基金项目： | 本文得到中国地质调查局《中国矿产地质与成矿规律综合集成和服务》(121201103000150020)及其二级项目《贵州锰矿成因与成矿规律》(DD20170346)，贵州省锰矿资源预测评价科技创新人才团队(黔科合平台人才[2018]5618),中国地质调查局发展研究中心(自然资源部矿产勘查技术指导中心)《贵州铜仁松桃锰矿矿集区矿产地质调查》(DD20190166-17),《锰矿勘查与开发大数据管理与智能处理系统研发应用》(黔科合支撑[2017]2951号),《黔东北若干超大型锰矿床三维地质建模与数据挖掘》(黔地矿科合[2017]2号)，《贵州省深部锰矿地球物理精细探测新技术研发》(黔科合支撑[2019]2868号)联合资助。 |
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| 摘 要： | 位于贵州省松桃县乌罗镇高地村的高地锰矿床,是贵州省地质矿产勘查开发局103地质大队应用南华纪锰矿裂谷盆地古天然气渗漏成矿理论和方法,在贵州铜仁松桃国家锰矿整装勘查区找矿实践检验中,继近年新发现普觉、道坨、桃子坪等三个隐伏超大型锰矿床之后,又新发现的隐伏超大型锰矿床。该矿床属于典型的古天然气渗漏沉积型锰矿床,地处李家湾-高地-道坨南华纪地堑盆地中心区域,位于古天然气渗漏喷溢成矿系统的中心相区,以致该矿床的矿体平均厚度、锰矿平均品位是目前该地区该类型所有锰矿床之最。地表发育成矿后期(燕山期)以冷水溪断层(F_3)为代表的犁式正断层,目前控制的隐伏菱锰矿体均分布在其下盘,由于地表相关系列断层均未穿过F_3断层,故深部隐伏锰矿体保存完好,尚未圈边,深部仍有较大找矿潜力。
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| 关 键 词： | 高地超大型锰矿床 地质特征 找矿实践 贵州松桃 |
| 收稿时间： | 2018/11/28 0:00:00 |
Main Characteristics and Prospecting Practice of the Gaodi Concealed Super-large Manganese Deposit in Songtao County, Guizhou Province |
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| YUAN Liang-jun,ZHOU Qi,PAN Wen,YAO Xi-cai,CHEN Jia-cai,TIAN jing-jiang,SHEN hong-qian,XIE Xiao-feng,ZHANG Ren-biao,XIE Xing-you,ZHENG Chao and QIN Yong-jun.Main Characteristics and Prospecting Practice of the Gaodi Concealed Super-large Manganese Deposit in Songtao County, Guizhou Province[J].Guizhou Geology,2019,36(3):197-206. |
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| Authors: | YUAN Liang-jun ZHOU Qi PAN Wen YAO Xi-cai CHEN Jia-cai TIAN jing-jiang SHEN hong-qian XIE Xiao-feng ZHANG Ren-biao XIE Xing-you ZHENG Chao and QIN Yong-jun |
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| Institution: | Engineering Technology Innovation Center of Mineral Resources Explorations in Bedrock Zones, Ministry of Natural Resources, Guiyang 550003, Guizhou.China ;103 Geological Party, Guizhou Bureau of Geology & Mineral Exploration and Development, Tongren 554300, Guizhou.China ;Guizhou Province Manganese Ore Resources Forecasting and Evaluation Technology Innovation Talent Team, Tongren 554300, Guizhou.China,Engineering Technology Innovation Center of Mineral Resources Explorations in Bedrock Zones, Ministry of Natural Resources, Guiyang 550003, Guizhou.China ;Guizhou Province Manganese Ore Resources Forecasting and Evaluation Technology Innovation Talent Team, Tongren 554300, Guizhou.China,Engineering Technology Innovation Center of Mineral Resources Explorations in Bedrock Zones, Ministry of Natural Resources, Guiyang 550003, Guizhou.China ;103 Geological Party, Guizhou Bureau of Geology & Mineral Exploration and Development, Tongren 554300, Guizhou.China ;Guizhou Province Manganese Ore Resources Forecasting and Evaluation Technology Innovation Talent Team, Tongren 554300, Guizhou.China ;Faculty of Earth Sciences,China University of Geoscience,Wuhan 430074, Hubei, China,Engineering Technology Innovation Center of Mineral Resources Explorations in Bedrock Zones, Ministry of Natural Resources, Guiyang 550003, Guizhou.China ;103 Geological Party, Guizhou Bureau of Geology & Mineral Exploration and Development, Tongren 554300, Guizhou.China ;Guizhou Province Manganese Ore Resources Forecasting and Evaluation Technology Innovation Talent Team, Tongren 554300, Guizhou.China,103 Geological Party, Guizhou Bureau of Geology & Mineral Exploration and Development, Tongren 554300, Guizhou.China,103 Geological Party, Guizhou Bureau of Geology & Mineral Exploration and Development, Tongren 554300, Guizhou.China,Engineering Technology Innovation Center of Mineral Resources Explorations in Bedrock Zones, Ministry of Natural Resources, Guiyang 550003, Guizhou.China ;Guizhou Province Manganese Ore Resources Forecasting and Evaluation Technology Innovation Talent Team, Tongren 554300, Guizhou.China,Engineering Technology Innovation Center of Mineral Resources Explorations in Bedrock Zones, Ministry of Natural Resources, Guiyang 550003, Guizhou.China ;103 Geological Party, Guizhou Bureau of Geology & Mineral Exploration and Development, Tongren 554300, Guizhou.China ;Guizhou Province Manganese Ore Resources Forecasting and Evaluation Technology Innovation Talent Team, Tongren 554300, Guizhou.China ;Faculty of Earth Sciences,China University of Geoscience,Wuhan 430074, Hubei, China,103 Geological Party, Guizhou Bureau of Geology & Mineral Exploration and Development, Tongren 554300, Guizhou.China,Engineering Technology Innovation Center of Mineral Resources Explorations in Bedrock Zones, Ministry of Natural Resources, Guiyang 550003, Guizhou.China ;103 Geological Party, Guizhou Bureau of Geology & Mineral Exploration and Development, Tongren 554300, Guizhou.China ;Guizhou Province Manganese Ore Resources Forecasting and Evaluation Technology Innovation Talent Team, Tongren 554300, Guizhou.China,103 Geological Party, Guizhou Bureau of Geology & Mineral Exploration and Development, Tongren 554300, Guizhou.China and Engineering Technology Innovation Center of Mineral Resources Explorations in Bedrock Zones, Ministry of Natural Resources, Guiyang 550003, Guizhou.China ;Guizhou Province Manganese Ore Resources Forecasting and Evaluation Technology Innovation Talent Team, Tongren 554300, Guizhou.China |
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| Abstract: | The Gaodi manganese deposit in Gaodi Village, Wuluo Town, Songtao County, Guizhou Province, is a newly discovered concealed super-large manganese deposit was discovered with the theory and method for the exploration of ancient gas leakage in the Nanhuaji manganese ore rift basin in the 103 Geological Party of the Guizhou Provincial Bureau of Geology and Mineral Exploration and Development, in Tongren, Guizhou. In the prospecting practice test of the Peach National Manganese Mine Ready Exploration Area, following the recent discovery of three concealed super-large manganese deposits such as Pujue, Daoyu and Taoziping, . The deposit belongs to a typical paleo-natural gas leakage sedimentary manganese deposit. It is located in the central area of the Lijiawan-Highland-Daoyu Nanhuaji mantle basin. It is located in the central phase of the paleo-natural gas seepage and spillover ore-forming system, so that the average thickness of the ore body and the average grade of manganese ore are currently the highest of all manganese deposits of this type in the region. In the late stage of surface development and mineralization (Yanshan period), the plough-type normal fault represented by Lengshuixi (F3) is distributed in the lower plate of the current concealed rhombohedral ore body. Since the series related faults have not passed through the F3 fault, The deep concealed manganese ore body is well preserved and has not been circled, and there is still a large potential for prospecting in the deep. |
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| Keywords: | Gaodi super-large manganese deposit Geological characteristics Prospecting practice Songtao Guizhou |
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