Application of tectono-geochemistry method for weak information extraction of Carlin-type gold deposits in Yunnan-Guizhou-Guangxi, SW China

被引:5
作者
Li, Songtao [1 ,2 ,3 ]
Xu, Liangyi [3 ]
Wang, Zepeng [2 ,3 ]
Yang, Chengfu [2 ,3 ]
Tan, Lijin [3 ]
Nie, Rong [3 ]
Meng, Minghua [3 ]
Li, Junhai [2 ,3 ]
Zhang, Bingqiang [3 ]
Liu, Jianzhong [2 ,4 ,5 ,6 ]
机构
[1] Guizhou Educ Univ, Sch Geog & Resources, Guiyang 550018, Peoples R China
[2] Minist Nat Resources, Engn Technol Innovat Ctr Mineral Resources Explora, Guiyang 550081, Peoples R China
[3] Guizhou Bur Geol & Mineral Explorat & Dev, Geol Team 105, Guiyang 550018, Guizhou, Peoples R China
[4] Guizhou Bur Geol & Mineral Explorat & Dev, Guiyang 550004, Peoples R China
[5] Guizhou Univ, Coll Resources & Environm Engn, Guiyang 550025, Peoples R China
[6] Guizhou Bur Geol & Mineral Explorat & Dev, Beijing Rd 203, Guiyang 550004, Peoples R China
基金
中国国家自然科学基金;
关键词
Tectono-geochemistry; Weak information extraction; Concealed deposit; Carlin-type gold deposit; Dian-Qian-Gui Golden Triangle; YOUJIANG BASIN; SOUTHWEST; PROVINCE; EXPLORATION; GEOCHRONOLOGY; ELEMENT; GEOLOGY; BASALTS; NEVADA; AREA;
D O I
10.1016/j.oregeorev.2023.105813
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Following decades of exploration of Carlin-type gold deposits in the Yunnan, Guizhou, and Guangxi provinces of China (known as the Dian-Qian-Gui Golden Triangle), surface mines are almost exhausted and undiscovered gold orebodies are deeply buried; thus, surficial geochemical information associated with concealed gold ore-bodies is poor. In this study, we compared methods of extracting this weak information based on soil geochemistry and tectono-geochemistry, and then applied the tectono-geochemical method to the Huijiabao and Nibao gold ore fields to evaluate its validity and identify favorable prospecting targets for deep-mineral explo-ration. We analyzed 8,842 soil geochemical samples and 4,049 tectono-geochemical samples from the Nibao gold ore field and its surroundings, and 253 tectono-geochemical samples from the Huijiabao gold ore field by sta-tistical analysis and geochemical mapping. Tectono-geochemical samples were less abundant, accounting for only approximately 60 % of the number of soil geochemical samples; however, the number and proportion of high-value samples were greater and the elemental content was typically higher. Primary geochemical infor-mation related to deep-seated Carlin-type gold orebodies is profoundly affected by structures such as faults, anticlines, joints, and fissures, and was effectively identified by the tectono-geochemical technique, which fo-cuses on tectonic and altered rocks. Conversely, soil geochemical information derived from these primary sources was significantly weaker because of the high mixing and homogeneity of elements during weathering. Eleven tectono-geochemical high composite anomalies of Au, Hg, Sb, As, and W were recognized in the east of the Nibao ore field, with Baogudi, Shuijingwan, Jiaozishan, Houzipo, Anzhe, and Hetaoshu predicted to be future targets of deep-mineral exploration. The Nayang-Yandengpo target was delineated according to high tectono-geochemical composite anomalies of Au, Hg, Sb, As, and Tl in the southeast part of the Huijiabao ore field, and nine concealed gold orebodies were identified at depths of 800-1,400 m through 37 boreholes, with a total gold resource of 16,338 kg and an average grade of 3.74 g/t. Successful case studies and applications demonstrate the effec-tiveness of tectono-geochemical information extraction method for detecting subtle signals from concealed orebodies, which will promote future deep exploration of the Dian-Qian-Gui Golden Triangle.
引用
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页数:18
相关论文
共 58 条
[1]   Primary geochemical haloes and alteration zoning applied to gold exploration in the Zarshuran Carlin-type deposit, northwestern Iran [J].
Aliyari, Farhang ;
Yousefi, Tohid ;
Abedini, Ali ;
Calagari, Ali Asghar .
JOURNAL OF GEOCHEMICAL EXPLORATION, 2021, 231
[2]   Thermal and isotopic profiling of the Pipeline hydrothermal system: Application to exploration for Carlin-type gold deposits [J].
Arehart, Greg B. ;
Donelick, Raymond A. .
JOURNAL OF GEOCHEMICAL EXPLORATION, 2006, 91 (1-3) :27-40
[3]  
Arne D.C., 2008, GeoScience Victoria Gold Undercover Report 4Department of Primary Industries
[4]  
Ashley R.P., 1991, Ore Geology Reviews, V6, P133, DOI DOI 10.1016/0169-1368(91)90018-3
[5]   Geochemistry and geochronology of native copper mineralization related to the Emeishan flood basalts, Yunnan Province, China [J].
Bing-Quan, Zhu ;
Yao-Guo, Hu ;
Zheng-Wei, Zhang ;
Xue-Jun, Cui ;
Tong-Mo, Dai ;
Guang-Hao, Chen ;
Jian-Hua, Peng ;
Yong-Ge, Sun ;
De-Han, Liu ;
Xiang-Yang, Chang .
ORE GEOLOGY REVIEWS, 2007, 32 (1-2) :366-380
[7]   Finding deeply buried deposits using geochemistry [J].
Cameron, EM ;
Hamilton, SM ;
Leybourne, MI ;
Hall, GEM ;
McClenaghan, MB .
GEOCHEMISTRY-EXPLORATION ENVIRONMENT ANALYSIS, 2004, 4 :7-32
[8]  
Deng X.W., 2004, Miner. Resour. Geol., V18, P318
[9]   Geochronology and geochemistry of Permian basalts in western Guangxi Province, Southwest China: Evidence for plume-litho sphere interaction [J].
Fan, Weiming ;
Zhang, Chunhong ;
Wang, Yuejun ;
Guo, Feng ;
Peng, Touping .
LITHOS, 2008, 102 (1-2) :218-236
[10]   Hydrothermal apatite as a robust U-Th-Pb chronometer for the Carlin-type gold deposits in the Youjiang basin, SW China [J].
Gao, Wei ;
Hu, Ruizhong ;
Huang, Yong ;
Zhu, Jingjing ;
Li, Qiuli ;
Mei, Lu ;
Bi, Xianwu ;
Liu, Jianzhong .
MINERALIUM DEPOSITA, 2024, 59 (01) :109-131