Ore-controlling and metallogenic role of interlayer-slide fault in the carbonate formation, southern China

QIAN Jianping; WU Zhengpeng; TANG Zhuanwu; XU Lei; JIA Yuheng

2020 Vol. 39, No. 11

Article Contents

Article navigation > Geological Bulletin of China > 2020 > 39(11): 1850-1857

Next Article Previous Article

QIAN Jianping, WU Zhengpeng, TANG Zhuanwu, XU Lei, JIA Yuheng. Ore-controlling and metallogenic role of interlayer-slide fault in the carbonate formation, southern China[J]. Geological Bulletin of China, 2020, 39(11): 1850-1857.

Citation:

QIAN Jianping, WU Zhengpeng, TANG Zhuanwu, XU Lei, JIA Yuheng. Ore-controlling and metallogenic role of interlayer-slide fault in the carbonate formation, southern China[J]. Geological Bulletin of China, 2020, 39(11): 1850-1857.

Ore-controlling and metallogenic role of interlayer-slide fault in the carbonate formation, southern China

College of Earth Sciences, Guilin University of Technology, Guilin 541004, Guangxi, China

Received Date: 10 March 2020

Revised Date: 05 June 2020

Publish Date: 25 November 2020

Abstract

Abstract

The interlayer-slide faults in the carbonate series are widely distributed in the Paleozoic strata in southern China. These faults constitute an important ore-controlling and forming structure. Determining the basic types, formation mechanism, and ore-controlling effects of the interlayer-slide faults is of great significance in the search for related deposits. Based on the lithological combination of the ore-bearing rock series, structural style and the relationship with the main fault, the authors divided the interlayer-slide faults into four basic types:the compound type of carbonate and shale boundary with interlayer-slide fault, the disconformities boundary with interlayer-slide fault, the thrusting nappe structure with stepped ramp and flat, and steeper slope master fault with gently inclined secondary interlayer-slide faults. The ore-controlling characteristics of different types of interlayer faults and typical examples were introduced and the roles of interlayer faults in ore-controlling and metallogenic process was discussed. Three stages of the formation of the interlayer-slide fault were summarized, which are slide fault in interlayer, interlayer-slide fault and superimposed fault.
- carbonate /
- interlayer-slide fault /
- basic type /
- ore-controlling functions /
- metallogenesis

FullText(HTML)

References

[1]	马杏垣, 索书田.论滑覆及岩石圈内多层次滑脱构造[J].地质学报, 1984, 19(3):205-213. Google Scholar
[2]	彭美丽, 易金, 姚蓉, 等.华南多层推滑构造系的物理模拟实验[J].大地构造与成矿学, 2011, 35(2):198-206. Google Scholar
[3]	王步清, 彭恩生, 唐诗佳, 等.广西泗顶铅锌矿层间滑动带地质特征及控矿作用[J].广西地质, 2000, 13(2):35-38. Google Scholar
[4]	常印佛, 刘学圭.关于层控式矽卡岩型矿床——以安徽省内下扬子坳陷中一些矿床为例[J].矿床地质, 1983, 2(1):11-20. Google Scholar
[5]	孙岩, 沈修志, 黄钟瑾.层滑断裂与层控矿床——以苏皖南部上古生界的地层为例[J].地质论评, 1984, 30(5):430-436. Google Scholar
[6]	凌其聪, 周贵斌, 黄许陈, 等."层控式"矽卡岩征床特征及成矿机制[J].贵金属地质, 1998, 7(2):91-95. Google Scholar
[7]	吴淦国, 张达, 臧文拴.铜陵矿集区构造滑脱与分层成矿特征研究[J].中国科学, 2003, 33(4):300-308. Google Scholar
[8]	黄许陈, 储国正.铜陵狮子山矿田多位一体(多层楼)模式[J].矿床地质, 1993, 12(3):221-252. Google Scholar
[9]	储国正.铜陵狮子山矿田构造及其控岩控矿作用的研究[J].安徽地质, 1992, 2(2):1-14. Google Scholar
[10]	刘经华, 李卉, 徐兆文, 等.冬瓜山层状铜矿成矿地质背景及成因[J].地质学刊, 2009, 33(2):133-137. Google Scholar
[11]	杨汉壮, 陈尚周.广东凡口铅锌矿层间滑动构造及其控矿作用[J].地质与勘探, 2006, 42(2):44-48. Google Scholar
[12]	原桂强, 贾会业, 宋玉伟, 等.凡口铅锌矿狮岭南深部矿床地质特征及找矿方向[J].地质学刊, 2019, 43(1):1-7. Google Scholar
[13]	毛健全, 杜定全, 潘年勋, 等.滑脱构造与黔西南地区金矿浅析[J].贵州工学院学报, 1990, 19(3):44-49. Google Scholar
[14]	钱建平.黔西南微细浸染型金矿基本特征和几点认识[J].桂林工学院学报, 2001, 21(1):27-34. Google Scholar
[15]	何丰胜, 毛健全, 杜定全.戈塘矿区层滑构造研究[J].贵州工业大学学报, 1997, 26(2):10-16. Google Scholar
[16]	袁远, 董从芳, 刘伯胜.广西黑水沟-大树脚锌多金属矿地质特征及外围找矿远景分析[J].2012, 3(3): 330-333. Google Scholar
[17]	张开均, 李扬.皖南台阶式逆冲断层控矿[J].地质与勘探, 1994, 30(3):14. Google Scholar
[18]	张开均, 施央申.长江中下游多金属成矿带逆冲推覆构造的控矿作用初探[J].江苏地质, 1996, 20(3):172-176. Google Scholar
[19]	郭振春.黔西南灰家堡金矿田"两层楼"模式及找矿意义[J].黄金地质, 2002, 8(4):18-23. Google Scholar
[20]	张蕾, 杜定全, 张晗彬, 等.黔西南灰家堡金矿田的构造控矿模式研究——"两层楼"模式的构造意义[J].黄金, 2012, 33(9):13-18. Google Scholar
[21]	吴松洋, 丁俊, 陈明, 等.贵州戈塘金矿滑脱构造及其与成矿的关系[J].金属矿山, 2014, (7):106-109. Google Scholar
[22]	刘帅, 张培兴, 熊灿娟, 等.贵州戈塘金矿SBT地球化学研究[J].贵州大学学报(自然科学版), 2013, 30(5):43-48. Google Scholar
[23]	黎应书, 祡大博, 贺磊.广东省仁化县凡口铅锌矿田构造体系[J].有色金属(矿山部分), 2018, 70(1):46-49. Google Scholar
[24]	李存有.高龙金矿同位素地球化学特征及其地质意义[J].贵金属地质, 1994, 3(2):123-130. Google Scholar
[25]	钱建平.黔西北威宁-水城铅锌矿带动力成矿作用研究[J].地质地球化学, 2001, 29(3):134-139 Google Scholar
[26]	刘俊来, 俞保祥, Weber K.浅成断层带的低温脆-韧性破裂共生机制[J].科学通报, 1999, 44(8):864-869. Google Scholar
[27]	刘俊来, 岛田充彦.实验变形岩石低温破裂作用的微观机制[J].地质科学, 1999, 34(2):242-250. Google Scholar
[28]	Griggs D T, Blacic J D.Quartz:Anomalous weakness of synthetic crystals[J].Science, 1965, 147(3655):292-295. doi: 10.1126/science.147.3655.292 CrossRef Google Scholar
[29]	Griggs D T. A model of hydrolytic weakening in quartz[J]. J.Geophys. Res., 1974, 79(11):1653-1611. doi: 10.1029/JB079i011p01653 CrossRef Google Scholar
[30]	Kekulawala K, Paterson M S. Boland J N. Hydrolytic weakening in quartz[J].Tectonophysics, 1978, 46(1/2):T1-T6. Google Scholar
[31]	Kronenberg A K, Tullis J. Flow strengths of quartz aggregates:grain size and pressure effects due to hydrolytic weakening[J]. Journal of Geophysical Research, 1984, 89(B6):4281-4297. doi: 10.1029/JB089iB06p04281 CrossRef Google Scholar
[32]	钱建平.广西灌阳地区碳酸盐岩层滑断裂构造地球化学系统[J].矿物学报, 1994, 14(4):348-356. Google Scholar
[33]	白嘉芬, 王长怀, 纳荣仙.云南金顶铅锌矿床地质特征及成因初探[J].矿床地质, 1985, 4(1):1-10. Google Scholar
[34]	张乾.云南金顶铅锌矿床成因研究[J].地质找矿论丛, 1991, 6(2):47-58. Google Scholar
[35]	杨开庆, 董法先, 王建平, 等.海南石碌矿区铁、金、铜、钻矿构造动力成矿作用的研究[J].中国地质科学院地质力学研究所所刊, 1988, 第11号:83-152. Google Scholar
[36]	杨兴科, 宫同伦.铅峒山铅锌矿床动力热液成矿特征[J].西安地质学院学报, 1992, 14(1):35-42. Google Scholar
[37]	钱建平.伸展作用与高龙金矿成矿作用研究[C]//全国矿床资源发展战略及隐伏矿床寻找学术研讨会.2001. Google Scholar
[38]	沈远超, 刘铁兵, 杨金中.层间滑动角砾岩型金矿床的地质特征及成矿远景[J].矿物岩石地球化学通报, 2000, 19(4):271-272. Google Scholar
[39]	钱建平.构造动力成矿理论若干问题的探讨[J].地质地球化学, 2002, 30(4):1-6. Google Scholar
[40]	夏玉成, 王生全, 樊怀仁.显德汪井田构造薄煤带形成机理及预测[J].河北煤炭, 1997, (2):27-29. Google Scholar
[41]	琚宜文, 姜波, 王桂梁, 等.层滑构造煤岩体微观特征及其应力应变分析[J].地质科学, 2004, 39(1):50-62. Google Scholar
[42]	靳尊秀.层间滑动构造探讨[J].河北煤炭, 1988, (3):50-53. Google Scholar