|
|
Development and evolution of Shenxian Mountains overthrust nappe structure in the middle and north section of Taihang Mountains |
HE Jiaoyue, WANG Jingui, SHEN Zongyi, GUO Bin, CHEN Yuanyuan, JI Hong, ZHANG Liguo, ZHANG Pengcheng |
Regional Geological Survey Institute of Hebei Province, Langfang 065000, China |
|
|
Abstract The deformation characteristics, evolution mechanism and metallogenic relationship of overthrust nappe structure in Taibaiwei Mountains which is the main ore-controlling factor of polymetallic deposits in the middle and north section of Taihang Mountains, have been studied in detail by predecessors, but Shenxian Mountains overthrust nappe structure in southeastern Taihang Mountains is rarely studied. Based on the first-hand data in the field, the geometrical characteristics of the overthrust nappe structure in Shenxian Mountains were statistically analyzed. The distribution, occurrence pattern, deformation mechanism of each unit (Feilai Peak, overthrust nappe fault, exotic rock series (nappe) and autochthone) were analyzed. And the kinematics characteristics were studied based on the assemble pattern, the development thickness of relevant stratum, and the geometric relationship between each overthrust nappe fault and cut stratum. The overall nappe direction of the overthrust nappe structure in Shenxian Mountains is from NW to SE, with the average distance of total thrust about 23.3km. Combined with the precedence relationship between the geological body cut by the nappe structure and the covered and reconstructed performance, the authors discussed the development and evolution process of the overthrust nappe structure in Shenxian Mountains. This overthrust nappe structure has gone three stages, namely the initial activity in Middle and Late Hualixi - Early Yanshan Period, main development in Middle and Late Yanshan Period and reform activity in Late Himalaya Period, which provides tectonic geological data for further study on the strata, magmatic rocks, and the relationship between minerals and structures in this overthrust nappe structure belt.
|
Received: 08 April 2019
|
|
|
|
|
[1] 米会斌,李好斌,张廷,等.灵丘南山中生代逆冲推覆构造特征及其意义[J].科学技术与工程,2015,15(28):112-119,124. [2] 陈超. 太行山中北段构造控矿作用研究[D].北京:中国地质大学(北京),2013. [3] 门文辉,张海东,黄水文,等.山西灵丘支家地银铅锌矿床地质特征、找矿标志及矿床成因探讨[J].西北地质,2012,45(增刊1):140-143. [4] 申旭辉,汪一鹏.太白维山山前断裂活动特征的初步研究[J].华北地震科学,1994,12(3):17-26. [5] 王永超. 太行山北段褶皱逆冲事件及其地层记录[D].北京:中国地质大学(北京),2014. [6] 张长厚,李程明,邓洪菱, 等.燕山—太行山北段中生代收缩变形与华北克拉通破坏[J].中国科学:地球科学,2011,41(5):593-617. [7] 牛树银,国连杰,许传诗,等.太行山中北段褶皱构造序列[J].华北地质矿产杂志,1995,10(2):190-196. [8] 曹毅. 太行山北段忻州—五台—蔚县一带中生代逆冲构造变形[D].北京:中国地质大学(北京),2012. [9] 许博,刘阳.太行神仙山髫髻山组火山岩锆石SHRIMP U-Pb年龄及其地质意义[J].矿物岩石地球化学通报,2012,31(3):257-260. [10] 张苏楠. 太行山王安镇杂岩体地球化学特征及成因探讨[D].西安:长安大学,2014. [11] 盛肖宁. 太行山中生代侵入岩地球化学特征及构造环境[D].北京:中国地质大学(北京),2016. [12] 王志云. 河北省涞源王安镇岩体地球化学特征及成因研究[D].北京:中国地质大学(北京),2013. [13] 陈斌,田伟,翟明国,等.太行山和华北其它地区中生代岩浆作用的锆石U-Pb年代学和地球化学特征及其岩浆成因和地球动力学意义[J].岩石学报,2005,21(1):13-24. [14] 蔡剑辉,阎国翰,常兆山,等.王安镇岩体岩石地球化学特征及成因探讨[J].岩石学报,2003,19(1):81-92. [15] 夏帅,牛树银,王雨豪,等.河北涞源县东团堡—黄土岗地区成矿地质作用分析[J].科技视界,2016(4):265,282. [16] 夏帅. 河北省苇家峪金矿成矿地质特征及构造研究[D].石家庄:河北地质大学,2016. [17] 郭长华,刘志明,陆树文,等.河北省涞源县连巴岭—东团堡地区金-多金属矿地质特征及找矿方向[J].地质找矿论丛,2010,25(2):112-117. [18] 白丽琴,贺斐,高雄.冀西南款—红岭子金多金属矿田成矿地质特征及控矿因素分析[J].西部资源,2012(2):53-56. [19] 罗易. 镰巴岭铅锌多金属矿床成矿物质来源及成因研究[D].石家庄:石家庄经济学院,2012. [20] 吴继莲,门文辉,陆春云,等.河北涞源连巴岭铅锌矿地质特征及成矿模式[J].西北地质,2012,45(S1):163-166. [21] Li J H,Niu X L,Chen Z,et al.Discovery of deep-level foreland thrust-fold structures in Taihang Mt.and its implication for early tectonic evolution of North China[J].Prog Nat Sci,2005,15(3):229-238. [22] 张醒,张浩亮.太行山北段岩体测年方法分析及其岩体形成演化[J].世界有色金属,2016(17):48-50. [23] 刘少峰,林成发,刘晓波,等.冀北张家口地区同构造沉积过程及其与褶皱-逆冲作用耦合[J].中国科学:地球科学,2018,48(6):705-731. [24] 史肖飞,刘少峰,林成发.燕山构造带西段千家店盆地生长构造与生长地层[J].中国科学:地球科学,2019,49(7):1116-1133. [25] 卢俊浩,张达,狄永军,等.赣东北船坑—铜山推覆构造及其与同构造成矿岩浆的关系[J].中国地质调查,2016,3(3):29-37. [26] 李猛,王超,张鑫,等.柴达木盆地北缘鱼卡地区构造混杂岩带解剖填图新进展[J].中国地质调查,2017,4(5):40-47. [27] Elliott D.A discussion on natural strain and geological structure-the energy balance and deformation mechanisms of thrust sh-eets[J].Phil Trans Roy Soc A,1976,283(1312):289-312. [28] Lowell J D.Structural styles in petroleum exploration[M].Tulsa:OGCL Publications,1985. [29] 河北省区域地质矿产调查研究所.中国区域地质志·河北志[M].北京:地质出版社,2017,1134-1138. |
[1] |
QIN Yulong, ZHAN Hanyu, WU Wenhui, LI Zheng, XIONG Changli, XU Yunfeng, LI Mingze. Geological structure revelation based on geochemical anomalies: A case study in Huiyuan Temple area of Sichuan Province[J]. , 2020, 7(3): 55-60. |
[2] |
YAN Shengwu, WU Wenxiang, LI Xiaoping, YANG Hui, MA Jiyue, XIONG Fuhao. Discovery and significance of Suxiong Formation ancient volcanic apparatus in Xiaoxiangling area of western Yangtze Block[J]. , 2019, 6(3): 47-55. |
[3] |
DI Wen, ZHUANG Wenming, LI Rui, WANG Jianrong, CHEN Junfeng, YU Deyan. Characteristics of Late Mesozoic extensional structures of Meixian in Guangdong Province[J]. , 2016, 3(6): 49-56. |
[4] |
LU Junhao, ZHANG Da, DI Yongjun, BI Minfeng, XIONG Guangqiang, QIN Xiaofeng. The relationship between thrust-fault and the syntectonic magmatism in Chuankeng-Tongshan, northeastern Jiangxi Province[J]. , 2016, 3(3): 29-37. |
[5] |
GAO Yong, DING Hualei, GUO Ruijun, LIU Yuanyuan, WANG Jianbin. Structural deformation of Gonglujing—Sangejing ductile shear zone in the Beishan orogenic belt, and its geological significance[J]. , 2016, 3(1): 26-34. |
[6] |
ZHANG Xiao-yang, ZOU Guang-jun. New Understanding of the Dayong-Guzhang-Jishou Fault[J]. , 2015, 2(1): 1-8. |
|
|
|
|