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The geophysical characteristics of the gabbro in Nzega area, Tanzania and its construct meaning |
Jie CAO, Shui-Ping LI( ), Zheng-Hao LIU, Jian-Tao SI, Yong-An LIANG, Fu-Li GAO |
No.2 Institute of Geological & Mineral Resources Survey of Henan, Zhengzhou 450001, China |
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Abstract A research area in Nzega region of Tanzania is covering so severe by fourth system that conventional geological prospecting methods are not available. In order to understand the stratigraphic or lithological boundary of the study area and to construct the production environment, it provides guidance function and effective prospecting information for the selected target area, carries out 1:10 000 the ground high-precision magnetic survey, delineate multiple linear magnetic anomaly zone of beaded displays for NW-SE and NE-SW. Based on the magnetic characteristics of gabbro, It is speculated that the magnetic anomaly belt is caused by intrusive gabbro dyke, thus clarifying the distribution characteristics of the linear structure in the study area. Combination of regional structure and distribution of gold deposits (points), that research the shear zone for NW-SE is the most close structure with gold mineralization relationship, to look for tectonic altered rock type and shear zone type gold deposit;After the surface engineering of the shear tectonic belt (SZ6) for NW-SE was revealed, gold mineralized alteration zone was discovered.
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Received: 11 December 2017
Published: 24 October 2018
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岩石名称 | 块数 | 磁化率κ/10-5 SI | 测定位置 | 变化范围 | 常见值 | 残坡积 | 16 | 10~14 | 12 | 钻孔 | 风化壳 | 26 | 11~21 | 16 | 钻孔 | 花岗岩 | 8 | 24~32 | 28 | 研究区地表 | 辉长岩 | 8 | 305~827 | 506 | 研究区外地表 | 辉长岩 | 52 | 1070~2070 | 1575 | 钻孔 | 变凝灰质砂岩 | 21 | 7~41 | 24 | 研究区地表 | 变凝灰质砂岩 | 131 | 9~27 | 18 | 钻孔 | 构造蚀变岩 | 232 | 12~34 | 22 | 钻孔 | 构造角砾岩 | 231 | 18~88 | 53 | 钻孔 |
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[1] |
李水平, 袁杨森, 司建涛 , 等. 坦桑尼亚姆瓦莫拉金矿综合找矿模式[J]. 中国地质, 2016,43(4):1409-1419.
|
[2] |
柳建新, 孙欢乐, 陈波 , 等. 重磁方法在国内外金属矿中的研究进展[J]. 地球物理学进展, 2016,31(2):713-722.
|
[3] |
朱丹, 刘天佑, 杨宇山 . 鄂东南地区岩体重磁异常场特征及找矿方向[J]. 物探与化探, 2017,41(4):587-593.
|
[4] |
杜化宇, 李晓禄, 杨玉勤 . 长山壕地区金矿航放航磁特征研究[J]. 物探与化探, 2017,41(3):421-428.
|
[5] |
崔志强 . 高精度航空物探在重要成矿带资源调查中的应用[J]. 物探与化探, 2018,42(1):38-49.
|
[6] |
崔玉良, 王根厚, 梁晓 . 西藏玛依岗日地区辉长岩地球化学特征及其构造意义[J]. 现代地质, 2017,31(2):258-266.
|
[7] |
程华, 李水平, 邵江波 , 等. 坦桑尼亚Maheiga金矿区航空、地面磁力异常特征与找矿研究[J]. 黄金科学技术, 2015,23(4):24-29.
|
[8] |
姜高珍, 李以科, 王安建 , 等. 坦桑尼亚苏库玛兰德绿岩带金矿地质特征及找矿思路[J]. 地质与勘探, 2015,51(6):1193-1199.
|
[9] |
李水平, 杨东朝, 程华 , 等. 坦桑尼亚条带状含铁建造磁化率参数统计特征及其应用[J]. 地质与勘探, 2013,49(4):784-790.
|
[10] |
李水平, 王建光, 程华 , 等. 钻孔岩芯岩(矿)石磁化率参数特征并用于地层岩性划分[J]. 物探与化探, 2013,37(5):775-778.
|
[11] |
郭友钊, 张振海, 张杰 , 等. 北山成矿带黑山铜镍硫化物矿区物性特征及其找矿意义[J]. 物探与化探, 2017,41(4):662-666.
|
[12] |
张翔, 江民忠, 汪远志 , 等. 利用高精度航磁资料研究滁州—六合地区断裂构造[J]. 物探与化探, 2017,41(2):231-241.
|
[13] |
蔡文军, 冯春圆, 倪卫冲 , 等. 伊春地区铅锌多金属矿的航磁异常特征分析与研究[J]. 物探与化探, 2016,40(5):869-875.
|
[14] |
王少帅, 邓国武, 汪冰 , 等. 高精度磁测与激电测深在航磁异常查证中的应用[J]. 物探与化探, 2016,40(5):916-922.
|
[15] |
李水平 . 低磁纬度地区ΔT异常处理解释方法在坦桑尼亚某地区金矿预查中的应用[J]. 物探与化探, 2009,33(6):657-659.
|
[16] |
李水平, 白德胜, 程华 , 等. 坦桑尼亚某金矿的磁力、激电异常特征[J]. 物探与化探, 2012,36(5):737-740.
|
[17] |
李水平, 王建光, 白德胜 , 等. 坦桑尼亚Maheiga金矿地球物理特征及找矿标志[J]. 地球物理学进展, 2014,29(5):2395-2400.
|
[18] |
史建民, 林泽付, 胡鑫 . 大兴安岭地区航磁异常特征与地质构造、成矿带的关系探讨[J]. 地球物理学进展, 2014,29(1):110-115.
|
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