THRUST NAPPE STRUCTURE DISCOVERED IN WAFANGDIAN DIAMOND METALLOGENIC BELT OF LIAONING PROVINCE

ZHANG Guo-ren; ZHONG Mi-shan; PAN Yu-qi; FU Hai-tao; LI Xian-dong; GAO Yong-zhao; GAO Fu-liang; WU Zi-jie; WANG Hai-peng

2020 Vol. 29, No. 3

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Article navigation > Geology and Resources > 2020 > 29(3): 294-298

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ZHANG Guo-ren, ZHONG Mi-shan, PAN Yu-qi, FU Hai-tao, LI Xian-dong, GAO Yong-zhao, GAO Fu-liang, WU Zi-jie, WANG Hai-peng. THRUST NAPPE STRUCTURE DISCOVERED IN WAFANGDIAN DIAMOND METALLOGENIC BELT OF LIAONING PROVINCE[J]. Geology and Resources, 2020, 29(3): 294-298.

Citation:

THRUST NAPPE STRUCTURE DISCOVERED IN WAFANGDIAN DIAMOND METALLOGENIC BELT OF LIAONING PROVINCE

1.
Liaoning Institute of Geological Exploration Co., Ltd., Dalian 116100, Liaoning Province, China
2.
Liaoning Geological Exploration and Mining Group, Shenyang 110032, China

More Information

Corresponding author: ZHONG Mi-shan, 278929624@qq.com

Received Date: 13 April 2020

Revised Date: 26 April 2020

Publish Date: 28 June 2020

Abstract

Abstract

Through structural analysis and 3D geological structure survey, the thrust nappe structure is discovered in the diamond metallogenic belt of Wafangdian area, which consists of the external slip system in hanging wall, autochthonous system in footwall and thrust fault. The thrust nappe that generally pushes from SEE to NWW in nearly horizontal low angle was formed in the Middle-Late Jurassic. Based on the discovery, it is inferred that there is great prospecting potential in the footwall, which provides new thoughts for diamond prospecting and basic geological research.
- thrust nappe structure /
- diamond /
- metallogenic belt /
- deep prospecting /
- Wafangdian City /
- Liaoning Province

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References

[1]	赵建军, 李靖, 王书, 等.辽宁瓦房店金刚石矿集区区域成矿控制条件及资源潜力预测[J].地质与资源, 2011, 20(1):40-44. Google Scholar
[2]	赵春强, 张志斌, 时溢, 等.辽南金刚石成矿背景研究进展及讨论[J].地质与资源, 2018, 27(2):149-159. Google Scholar
[3]	万方来, 蒋金晶, 王煊, 等.辽宁省瓦房店金伯利岩矿区构造特征及其控矿作用[J].地质通报, 2019, 38(1):62-67. Google Scholar
[4]	付海涛.辽宁省瓦房店地区金刚石原生矿找矿信息研究[J].地质找矿论丛, 2005, 20(4):281-285, 290. Google Scholar
[5]	付海涛.辽宁瓦房店地区环状构造与金伯利岩关系的几点认识[J].西部资源, 2019(3):14-16. Google Scholar
[6]	付海涛.瓦房店地区金刚石找矿值得注意的两个问题[J].地球科学前沿, 2019, 9(5):328-333. Google Scholar
[7]	杨占兴, 王彬娜.辽宁瓦房店30号金伯利岩管地球化学特征及金刚石矿床成因[J].世界地质, 2016, 35(2):378-386. Google Scholar
[8]	万方来, 蒋金晶.华北地台金刚石找矿前景及成矿预测[J].地质与资源, 2015, 24(3):218-225. Google Scholar
[9]	迟广成, 李国武, 肖刚, 等.辽宁瓦房店和山东蒙阴金伯利岩中铬铁矿成分特征及指示意义[J].地质与资源, 2013, 22(1):76-80. Google Scholar
[10]	刘飞, 杨经绥, 连东洋, 等.博茨瓦纳和中国含金刚石金伯利岩的地质特征及对寻找类似岩体的启示[J].中国地质, 2019, 46(1):43-76. Google Scholar
[11]	安战锋, 贾志业, 王萌, 等.辽宁瓦房店地区金刚石航磁调查飞行方法探讨[J].物探与化探, 2017, 41(1):111-115. Google Scholar
[12]	孟琪.辽宁金刚石的过去、现在和未来[J].岩石矿物学杂志, 2016, 35(S1):191-194. Google Scholar
[13]	居易, 朱仁智, 倪培, 等.瓦房店30号岩管金伯利岩中尖晶石成分特征及其意义[J].矿物岩石地球化学通报, 2016, 35(6):1217-1225. Google Scholar
[14]	付海涛.辽宁瓦房店地区50号金伯利岩管深部找矿问题研究[J].中国非金属矿工业导刊, 2019(3):34-36. Google Scholar
[15]	付海涛, 单学东, 康宁, 等.三维建模技术在30号岩管勘查中的应用[J].地球科学前沿, 2017, 7(5):645-652. Google Scholar
[16]	付海涛.三维建模技术在金刚石勘查中的应用——以辽宁省瓦房店地区为例[J].地质通报, 2019, 38(1):51-55. Google Scholar
[17]	崔克英, 庞庆邦, 徐英奎.论辽南韧性推覆构造基本特征[J].辽宁地质, 1986(2):45-59. Google Scholar
[18]	李显东, 陈荣度, 单学东, 等.辽东半岛南部盖层褶皱与构造演化[J].辽宁地质, 2000, 17(3):190-198. Google Scholar
[19]	刘英才, 付俊彧, 赵春荆, 等.《东北地区1:150万大地构造相图》的编制[J].地质与资源, 2020, 29(1):1-6. Google Scholar
[20]	孙中任, 赵雪娟, 张晓丽, 等.东北地区北西向构造的成因与特征[J].地质与资源, 2019, 28(1):1-6, 56. Google Scholar
[21]	万天丰.中国大地构造学纲要[M].北京:地质出版社, 2004:135-147. Google Scholar
[22]	朱志澄, 宋鸿林.构造地质学[M].武汉:中国地质大学出版社, 1990:195-213. Google Scholar
[23]	宋鸿林, 张长厚, 王根厚.构造地质学[M].北京:地质出版社, 2013:175-192. Google Scholar