缅甸第四特区景缅金矿床元素地球化学特征及找矿预测
[Abstract]:The research topic of this paper comes from the Sino-Myanmar cooperation project "Geological Prospecting of Jingmen Gold Mine area in the fourth Special Zone of Myanmar", which was undertaken by Professor he Mingyou. Through this study, the geochemical characteristics of gold and its closely related elements are discussed, and the ore-prospecting targets are delineated. It provides data support and scientific basis for the qualitative evaluation of prospecting potential and prospecting prospect in this area. Therefore, this thesis has important scientific research significance and practical application value. This paper chooses the gold ore area as the research object, closely combines the project research task, emphatically studies the element geochemistry characteristic of the gold deposit area. The data were collected by 1: 5000 soil geochemistry measurement method and rock geochemistry measurement method respectively. According to the data obtained by X-ray fluorescence instrument and atomic absorption spectrometry, the data processing and correlation analysis were carried out by using SPSS and Sufer software. On this basis, multi-element geochemical anomalies and prospecting targets are delineated. The research contents include: regional geological background, deposit geological structure, metallogenic geological conditions, prospecting and prediction. Through the above research, we can get the following understanding: 1. The geochemistry survey of soil can be used as an important and effective prospecting method in this area. By using the method of soil geochemistry survey, the prospecting target area can be quickly reduced and the geological prospecting can be provided more directly. The results of factor analysis show that the contribution rate of factor 1 is 46.346, which represents magmatic information, especially the information of iron group element migration, and factor 2 (AsPbPbPbBHG) contribution rate is 20.372.The contribution rate of factor 1 represents the information of medium and low temperature hydrothermal solution, and it may also be the information of fault, and it is also possible that the contribution rate of factor 2 is 20.372, and that the contribution rate of factor 2 is 20.372.The contribution rate of factor 1 is 46.346mg, and the contribution rate of factor 2 is 20.372.The contribution rate of factor 2 is 20.372. The contribution rate of factor 3 (SB ~ (2 +) is 10.388, which represents the information of polymetallic mineralization such as tin (or Sn-rich granite), and factor 4 (Ca) contribution rate of (Ca) is 6.42828), which represents the information of polymetallic mineralization such as WGZn-Cu, and has experienced calcification geological process in the later stage. The best indicator element for gold prospecting in soil geochemistry in this area is the indicating orebody of As-PbPbPbBiHgPbBiHgTiTi-BaCoCoFE-NiCr-Cr-Mn orebody. Three anomalous areas can be found from the single element anomaly map and the comprehensive element anomaly map obtained from the data processing of soil survey by sufer software. The anomalous field is the most promising area because of its strong intensity and large scale. It should be regarded as the key exploration area, and the three most promising prospecting target area .4 should be delineated accordingly. The rock survey data show that the Au-Ag content is the highest in silicified rocks. The results of factor analysis show that the association correlation of Au-As-Bi-Ag-Bi-ZZN Cu-Sb-Pb-Bi assemblage is very good. The results are as follows: 1. Using soil and rock element analysis data, cluster analysis, factor analysis and cumulative frequency method were used to process the data to extract the abnormal information of au element and delineate the gold anomaly field. It is also pointed out that as HgPb can be used as an effective prospecting marker for gold 2. According to the anomalous characteristics of element assemblage, metallogenic geological background and ore-controlling factors, three main ore-prospecting targets are delineated. The direction of prospecting in the area in the future is determined.
【学位授予单位】:成都理工大学
【学位级别】:硕士
【学位授予年份】:2017
【分类号】:P618.51
【参考文献】
相关期刊论文 前10条
1 王少芳;杨雨凡;;缅甸第四特区景缅金矿区土壤地球化学特征及找矿远景预测研究[J];世界有色金属;2017年05期
2 王少芳;何明友;葛婉婷;刘洋;童立立;宋文平;;缅甸第四特区景缅金矿区土壤地球化学特征及找矿远景预测研究[J];矿物学报;2015年S1期
3 陈喜峰;曾普胜;;缅甸曼德勒省Singu地区基达堡金矿床地质特征与成因初探[J];矿物学报;2013年S2期
4 王卫星;曹淑萍;程绪江;王丽瑛;李攻科;刘永涛;;蓟县地区锰硼矿地质地球化学特征及其找矿方向[J];矿产与地质;2013年03期
5 王文涛;李增达;宋炯;;太行山成矿带岩性影响较大元素的异常圈定及方法研究[J];科技广场;2011年10期
6 吴良士;;缅甸区域成矿地质特征及其矿产资源(二)[J];矿床地质;2011年02期
7 吴良士;;缅甸区域成矿地质特征及其矿产资源(一)[J];矿床地质;2011年01期
8 戴慧敏;宫传东;鲍庆中;孙中任;尤宏亮;金鑫;高飞;;区域化探数据处理中几种异常下限确定方法的对比——以内蒙古查巴奇地区水系沉积物为例[J];物探与化探;2010年06期
9 陈永清;黄静宁;卢映祥;夏庆霖;孙明祥;李建荣;;中缅毗邻区金腊Pb-Zn-Ag多金属矿田元素、稳定同位素和流体包裹体地球化学[J];地球科学(中国地质大学学报);2009年04期
10 卢映祥;刘洪光;黄静宁;张宏远;陈永清;;东南亚中南半岛成矿带初步划分与区域成矿特征[J];地质通报;2009年Z1期
相关会议论文 前1条
1 施俊法;李友枝;金庆花;唐金荣;;浅谈地质调查科技创新[A];中国地质矿产经济学会青年分会2006年学术交流论文汇编[C];2006年
相关硕士学位论文 前10条
1 何益;攀枝花层状岩体钪的地球化学特征及富集规律[D];成都理工大学;2016年
2 葛婉婷;缅甸第四特区曼排钨矿床元素地球化学研究[D];成都理工大学;2016年
3 梁学玉;埃塞俄比亚纳格莱Ⅱ地球化学异常特征与评价[D];成都理工大学;2016年
4 胡庭先;重庆文峰地区1:5万水系沉积物地球化学数据信息处理[D];成都理工大学;2014年
5 谢晋;老挝阿文金矿成矿模式与找矿靶区评价[D];中国地质大学(北京);2014年
6 樊连杰;内蒙古中东部草原景观区多金属矿地球化学勘查方法研究[D];中国地质大学(北京);2013年
7 汪等;西藏申扎—班戈地区区域地球化学异常及找矿评价[D];成都理工大学;2013年
8 李昭坤;内蒙古珠斯楞地区铜资源地球化学勘查及资源潜力评价[D];长安大学;2012年
9 黄瑞;化探数据处理方法研究[D];成都理工大学;2005年
10 邹林;青海阿尔茨托山地区化探找矿信息的快速识别与综合评价[D];中南大学;2004年
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