ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
闽北邵武地区水系沉积物地球化学特征及找矿预测
  
关键词:stream sediment survey  geochemistry features  Banling–Zhangcuo prospecting target area  Shaowu
基金项目:中国地质调查局地质调查项目(编号: DD20190816)
作者单位E-mail
韩志坤 中化地质矿山总局河南地质局 898446019@qq.com 
栗克坤 中化地质矿山总局河南地质局  
张青松 中化地质矿山总局河南地质局  
张静杰 中化地质矿山总局河南地质局  
闫晓博 中化地质矿山总局河南地质局  
靳乾峰 中化地质矿山总局河南地质局  
蒋济勇 中化地质矿山总局河南地质局  
刘增政 中化地质矿山总局河南地质局  
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摘要:
Geochemical Characteristics and Prospecting Prediction of Stream Sediments in Shaowu Area, Northern Fujian Province
      Shaowu area is located in the W-Sn-Mo-Au-Ag-Pb-Zn-Nb-Ta-(pyrolytic)-fluorite metallogenic belt (Ⅲ-81) of the Central Zhejiang–Wuyishan (uplift), and in the southwest of the fluorite metallogenic sub-belt (Ⅳ-1) of the northwest Fujian, which has good prospecting prospects. In this study, the geochemical characteristics of elements, R clustering correlation, anomaly characteristics of single element, etc., show that F, Au, Pb, Zn, Nb, Ta and other elements have a certain prospecting potential, and there are 652 anomalies of order elements and 26 comprehensive anomalies. On the basis of the anomalies of stream sediments, screening and evaluation sequence and main anomaly interpretation results, combined with background of the metallogenic geologic structures, 4 areas were delineated, including Cunwei–Xialu lead-zinc mine, Wujiatang–Nanshanxia fluorite ore, Zhuling–Yanbantian fluorite ore and lead-zinc mine, and Banling–Zhangcuo fluorite ore prospecting prediction, for the prospecting direction and the next step prospecting work providing important references; The prospecting prediction area of Banling–Zhangcuo fluorite deposit were optimized, and the anomaly were verified by means of geological survey and trough exploration, and better prospecting results were obtained.
ZHOU Bo-wen,WANG Chun-lian,YOU Chao,LIU Dian-he,LIU Si-han,YU Xiao-can,YAN Kai,LIU Xue.2022.Geochemical Characteristics and Prospecting Prediction of Stream Sediments in Shaowu Area, Northern Fujian Province[J].Acta Geoscientica Sinica,43(3):411-420.
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