| 贵州赫章县猪拱塘铅锌矿床主矿体地质特征及找矿标志 |
| |
| 引用本文： | 吴大文,何良伦,蔡京辰,王军,柏光辉,杨天,金翔霖,黄庆.贵州赫章县猪拱塘铅锌矿床主矿体地质特征及找矿标志[J].贵州地质,2019,36(4):299-306. |
| |
| 作者姓名： | 吴大文 何良伦 蔡京辰 王军 柏光辉 杨天 金翔霖 黄庆 |
| |
| 作者单位： | 贵州省地矿局113地质大队,贵州 六盘水,553000;赫章鼎盛鑫矿业发展有限公司,贵州 赫章,553200 |
| |
| 基金项目： | 贵州省地矿局重大地质科研项目“黔西北地区铅锌找矿攻关(黔地矿纪要(2015)14号)”、贵州省科技支撑计划课题(黔科合支撑[2019]2865)、赫章鼎盛鑫矿业发展有限公司(GZDK113D2016063)项目联合资助。 |
| |
| 摘 要： | 贵州赫章猪拱塘铅锌矿床是贵州省内发现的首个中低温热液型超大型铅锌矿床。铅锌矿体严格受北西向断裂构造控制,主要赋存于北西向F1、F2及隐伏F20、F30断裂破碎带及次级断裂破碎带内。根据矿体的空间展布特点,以控容矿断裂作为矿体对比连接的依据,圈定69个铅锌矿体,探明铅锌金属资源量275万吨。Ⅰ-1号主矿体为区内规模最大铅锌矿体,呈似层状、透镜状产出于猪拱塘断层(F1)破碎带内,赋矿围岩建造为二叠系中统栖霞组(P2q)泥灰岩、灰岩、白云质灰岩建造。矿体长度1 640 m,平均厚11. 01 m,铅平均2. 81%,锌平均8. 71%。铅锌资源量182万吨,占矿床总资源量的57%,资源量规模达特大型。通过对Ⅰ-1号主矿体地质特征及找矿标志详细论述,为矿床总体特征及成矿规律总结提供依据。
|
| 关 键 词： | 贵州猪拱塘 主矿体 铅锌矿床 地质特征 找矿标志 |
| 收稿时间： | 2019/4/19 0:00:00 |
Zhugongtang Lead-zinc Deposit in Hezhang, Guizhou |
| |
| WU Da-wen,HE Liang-lun,CAI Jing-chen,WANG Jun,Bai Guang-hui,YANG Tian,JIN Xiang-lin and HUANG Qing.Zhugongtang Lead-zinc Deposit in Hezhang, Guizhou[J].Guizhou Geology,2019,36(4):299-306. |
| |
| Authors: | WU Da-wen HE Liang-lun CAI Jing-chen WANG Jun Bai Guang-hui YANG Tian JIN Xiang-lin and HUANG Qing |
| |
| Institution: | 113 Geological Party, Guizhou Bureau of Geology and Mineral Exploration & Development of,Liupanshui 553000, Guizhou, China,113 Geological Party, Guizhou Bureau of Geology and Mineral Exploration & Development of,Liupanshui 553000, Guizhou, China,113 Geological Party, Guizhou Bureau of Geology and Mineral Exploration & Development of,Liupanshui 553000, Guizhou, China,113 Geological Party, Guizhou Bureau of Geology and Mineral Exploration & Development of,Liupanshui 553000, Guizhou, China,Hezhang Dingshengxin Mining Development Co, Ltd, Hezhang 553200, Guizhou, China,113 Geological Party, Guizhou Bureau of Geology and Mineral Exploration & Development of,Liupanshui 553000, Guizhou, China,113 Geological Party, Guizhou Bureau of Geology and Mineral Exploration & Development of,Liupanshui 553000, Guizhou, China and 113 Geological Party, Guizhou Bureau of Geology and Mineral Exploration & Development of,Liupanshui 553000, Guizhou, China |
| |
| Abstract: | Zhugongtang lead-zinc deposit in Hezhan gis the first medium-low temperature hydrothermal and super-large lead-zinc deposit discovered in Guizhou province. The lead-zinc ore body strictly controlled by the faulted structures in NW mainly occurs in the faulted fracture zones and secondary faulted fracture zones of F1 and F2 in NW, as well as the concealed F20 and F30. According to the spatial characteristics of the ore body, 69 lead-zinc ore bodies were delineated, and 2.75 million tons of lead-zinc metal resources were proven with ore-controlling and ore-hosting structures as the ore bodies for comparison. The main ore body of I-1, formed in the fracture zone of Zhugongtang fault(F1), is the largest lead-zinc ore body in the area, and it appears in bedded and lenticular shapes. The host rocks are composed of marl, limestone, and dolomitic limestone in the Permian Qixia group(P2q). The length and average thickness of the ore body are 1 640 m and 11.01 m respectively, whilethe average lead and zinc levels are 2.81% and 8.71% respectively. The amount of lead and zinc is up to 1.82 million tons, accounting for 57% of the total resources of the deposit. Its proven resources have reached asuper-huge scale. The geological characteristics and of the main ore body of I-1 weredescribed in detail, therefore, this paper can provide an evidence for the overall characteristics and metallogenic regularity of ore deposits. |
| |
| Keywords: | |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
| 点击此处可从《贵州地质》浏览原始摘要信息 |
| 点击此处可从《贵州地质》下载免费的PDF全文 |
|
