APPLICATION AND PRACTICE OF THE NEOTECTONIC GEOLOGICAL MAPPING METHODS——A CASE STUDY OF 1:50000 MAPPING PILOT IN HULESITAI, INNER MONGOLIA, CHINA

JIA Li-yun; YE Pei-sheng; ZHANG Xu-jiao; HE Ze-xin; YANG Xing-chen; ZHOU Qing-shuo; YE Meng-ni; LIU Xiao-tong; LI Cheng-lu; WU Ze-qun; ZHOU Wei; HE Xiang-li

Volume 23 Issue 2

Apr. 2017

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Article Navigation > Journal of Geomechanics > 2017 > 23(2): 189-205

JIA Li-yun, YE Pei-sheng, ZHANG Xu-jiao, et al., 2017. APPLICATION AND PRACTICE OF THE NEOTECTONIC GEOLOGICAL MAPPING METHODS——A CASE STUDY OF 1:50000 MAPPING PILOT IN HULESITAI, INNER MONGOLIA, CHINA. Journal of Geomechanics, 23 (2): 189-205.

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APPLICATION AND PRACTICE OF THE NEOTECTONIC GEOLOGICAL MAPPING METHODS——A CASE STUDY OF 1:50000 MAPPING PILOT IN HULESITAI, INNER MONGOLIA, CHINA

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
2.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
3.
Beijing Institute of Geology for Mineral Resources, Beijing 100012, China

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Received: 2016-10-03
Published: 2017-04-01

Abstract

Abstract

Neotectonic investigation is the foundation of the study of crustal movement, evaluation for geological hazards, environmental geology and crustal stability. With great theoretical and practical significance, neotectonic investigation is one of the key content of regional geological mapping.The area of the 1:50000 mapping pilot of the Hulesitai, Inner Mongolia, is located at the north boundary of the Hetao fault-subsiding belt. Frequent tectonic activity, complex stratum, variable landforms and extensive development of piedmont faults are all ideal neotectonic materials for studyand investigation in this area. In this article, the investigated objects for 1:50000 geological mappingis described, the survey technology methods combination of "space-ground-deep"is summarized (remotesensing, integrated geophysical,geochemical and detailed field geological survey, ancient earthquake trench with laser scanning, drilling and chronology methods), and its adaptability in the tectonic active area on the basis of predecessors' area method theory is studied. With reference to the "general provisions of 1:50000 regional geological survey," and "1:50000 regional geological survey technical requirements (provisional)" and other relevant technical requirements, the results of geological survey are expressed on the geological map with the digital mapping technology. This methods combination of survey technology is not only an effective exploration of neotectonic investigation mapping method, but also an important reference for the new round of large-scale investigation mapping for other tectonic area.
- neotectonics,
- mapping,
- geological survey method,
- geomorphology

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References

[1]	周飞飞, 杨健. 现代地质填图, 走向特殊地质地貌区[N]. 中国国土资源报, 2016-01-27(006).ZHOU Fei-fei, YANG Jian. Modern geological mapping, to the special geological features area[N]. China Land and Resources Reported, 2016-01-27(006).
[2]	程绍平, 杨桂枝. 国外新构造研究进展述评[J]. 地震地质, 2008, 30(1):31~43. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ200801003.htm CHENG Shao-ping, YANG Gui-zhi. Current advance of overseas research on neotectonics:a review and comments[J]. Seismology and Geology, 2008, 30(1):31~43. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ200801003.htm
[3]	李祥根. 中国新构造运动概论[M]. 北京:地震出版社, 2003. LI Xiang-gen. Introduction to China Neotectonics[M]. Beijing:Seismological Press, 2003.
[4]	刘光勋. 新构造学研究趋势的展望[J]. 地学前缘, 1995, 2(1/2):203~211. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY502.015.htm LIU Guang-xun. The trend in research of neotectonics[J]. Earth Science Frontiers, 1995, 2(1/2):203~211. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY502.015.htm
[5]	胡道功. 探索适合我国地质特点的地质填图新方法[N]. 中国国土资源报, 2014-07-24(005). HU Dao-gong. Explore new method of geological mapping for geological characteristics in China[N]. China Land and Resources News, 2014-07-24(005).
[6]	王涛, 计文化, 胡健民, 等. 专题地质填图及有关问题讨论[J]. 地质通报, 2016, 35(5):633~641. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201605001.htm WANG Tao, JI Wen-hua, HU Jian-min, et al. Geological mapping forspecial issues and a discussion on related topics[J]. Geological Bulletin of China, 2016, 35(5):633~641. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201605001.htm
[7]	赵希涛, 胡道功, 吴中海. 晚新生代地质填图理论与方法的新探索[J]. 地质通报, 2009, 28(10):1419~1429. doi: 10.3969/j.issn.1671-2552.2009.10.008 ZHAO Xi-tao, HU Dao-gong, WU Zhong-hai. An exploration to the theory and methodology of Late Cenozoic geological mapping[J]. Geological Bulletin of China, 2009, 28(10):1419~1429. doi: 10.3969/j.issn.1671-2552.2009.10.008
[8]	张振法. 阴山山链隆起机制及有关问题探讨[J]. 内蒙古地质, 1995, (S):17~35. http://www.cnki.com.cn/Article/CJFDTOTAL-NMGZ5Z1.002.htm ZHANG Zhen-fa. Approach to the mechanism and relative problems of Yinshan chain uplift[J].Geology of Inner Mangolia, 1995, (S):17~35. http://www.cnki.com.cn/Article/CJFDTOTAL-NMGZ5Z1.002.htm
[9]	贾丽云. 内蒙古阴山西段新构造运动与地貌响应[D]. 北京:中国地质大学(北京), 2015. JIA Li-yun. Neotectonics and geomorphic response in western Yin mountains area, Inner Mongolia, northern China[D]. Beijing:China University of Geosciences, 2015.
[10]	潘博. 河套断陷带北缘主要活动断裂带地震危险性研究[D]. 北京:中国地质大学(北京), 2012. PAN Bo. Research on seismic hazard evaluation of active faults on the north boundary of the Hetao fault-depression zone[D]. Beijing:China University of Geosciences, 2012.
[11]	国家地震局《鄂尔多斯周缘活动断裂系》课题组. 鄂尔多斯周缘活动断裂系[M].北京:地震出版社, 1988. Research Group of Active Fault System around the Ordos Massif. Active Fault System Around Ordos Massif[M]. Beijing:Seismological Press, 1988.
[12]	江娃利. 内蒙狼山-色尔腾山山前活动断裂古地震事件识别及同震垂直位移[J]. 地壳构造与地壳应力文集, 2003:45~52. http://www.cnki.com.cn/Article/CJFDTOTAL-SEIS200300005.htm JIANG Wa-li. Paleo-earthquake event and co-seismic vertical deformation recognition along the Langshan-Sertenshan pediment fault, Inner Mongolia[J]. Bulletin of the Institute of Crustal Dynamics, 2003:45~52. http://www.cnki.com.cn/Article/CJFDTOTAL-SEIS200300005.htm
[13]	聂宗笙, 吴卫民, 许桂林, 等. 内蒙古狼山-色尔腾山山前活动断裂带地质图(1:50000)[M].北京:地震出版社, 2013. NIE Zong-sheng, WU Wei-min, XU Gui-lin, et al. Geological Map(1:50000) of the Langshan-Sertenshan Pediment Fault, Inner Mongolia[M]. Beijing:Seismological Press, 2013.
[14]	杨晓平, 冉勇康, 胡博, 等. 内蒙古色尔腾山山前断裂带乌加河段古地震活动日[J]. 地震学报, 2003, 25(1):62~71. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXB200301007.htm YANG Xiao-ping, RAN Yong-kang, HU Bo, et al. Paleoseismic activity on Wujiahe segment of Serteng piedmont fault, Inner Mongolia[J]. ActaSeismologicaSinica, 2003, 25(1):62~71. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXB200301007.htm
[15]	Jia L Y, Zhang X J, He Z X, et al. Late Quaternary climatic and tectonic mechanisms driving river terrace development in an area of mountain uplift:a case study in the Langshan area, Inner Mongolia, northern China[J]. Geomorphology, 2015, 234:109~121. doi: 10.1016/j.geomorph.2014.12.043
[16]	贾丽云, 张绪教, 叶培盛, 等. 阴山西段河流阶地发育的年代序列及其对构造隆升的指示意义[J]. 地质学报, 2017, 91(1):249~265. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201701015.htm JIA Li-yun, ZHANG Xu-jiao, YE Pei-sheng, et al. Chronology sequence of the river terraces development in western Yinshan Mountains, China:implications for the tectonic uplifting[J]. ActaGeologicaSinica, 2017, 91(1):249~265. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201701015.htm
[17]	程绍平, 李传友, 杨桂枝, 等. 内蒙古狼山-色尔腾山的剥蚀面序列和景观发育的控制因素[J]. 第四纪研究, 2006, 26(1):99~107. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200601012.htm CHENG Shao-ping, LI Chuan-you, YANG Gui-zhi, et al. The denudational-surface sequence and controls on the landscapte development in the Langshan Mountains-Seertengshan Mountains, Inner-Mongolia[J]. Quaternary Sciences,2006, 26(1):99~107. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200601012.htm
[18]	何泽新, 张绪教, 贾丽云, 等. 内蒙古狼山山前台地成因及其新构造运动意义[J]. 现代地质, 2014, 28(1):98~108. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ201401010.htm HE Ze-xin, ZHANG Xu-jiao, JIA Li-yun, et al. Genesis of piedmont terraces and its Neotectonic Movement significance in Langshan Mountain area, Inner Mongolia[J]. Geoscience, 2014, 28(1):98~108. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ201401010.htm
[19]	徐步, 李焕康, 吴之理, 等. 中华人民共和国乌拉特后旗K-48-(24)、临河县幅1:20万区域地质调查报告[R]. 白彦花:内蒙古自治区第一区域地质调查队, 1982. Jia L Y, Zhang X J, Ye P S, et al. Development of the alluvial and lacustrine terraces on the northern margin of the Hetao Basin, Inner Mongolia, China:implications for the evolution of the Yellow River in the Hetao area since the late Pleistocene[J]. Geomorphology, 2016, 263:87~98.
[20]	XU Bu, LI Huan-kang, WU Zhi-li, et al. The 1:200000 geological Survey report of Wulatehouqi K-48-(24), Linhexian K-48-(30)[R]. Baiyanhua:No. 1 Regional Geological Survey Team, Inner Mongolia, China, 1982.
[21]	Darby B J, Ritts B D. Mesozoic structural architecture of the Lang Shan, North-Central China:intraplate contraction, extension, and synorogenic sedimentation[J]. Journal of Structural Geology, 2007, 29(12):2006~2016. doi: 10.1016/j.jsg.2007.06.011
[22]	张岳桥, 廖昌珍. 晚中生代-新生代构造体制转换与鄂尔多斯盆地改造[J]. 中国地质, 2006, 33(1):28~40. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200601002.htm ZHANG Yue-qiao, LIAO Chang-zhen. Transition of the Late Mesozoic-Cenozoic tectonic regimes and modification of the Ordos basin[J]. Geology in China, 2006, 33(1):28~40. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200601002.htm
[23]	汪良谋, 董瑞树, 张裕明, 等. 河套地区新生代地质构造和地震活动的某些特点-兼谈鄂尔多斯周边新生代断陷盆地的形成机制田[J].华北地震科学, 1984, 2(4):8~16. http://www.cnki.com.cn/Article/CJFDTOTAL-HDKD198404001.htm WANG Liang-mou, DONG Rui-shu, ZHANG Yu-ming, et al. Characteristics of the Hetao area Cenozoic geological structure and earthquake activity:formation mechanism of Cenozoic faulted basins in Erdos surrounding[J]. North China Earthquake Sciences, 1984, 2(4):8~16. http://www.cnki.com.cn/Article/CJFDTOTAL-HDKD198404001.htm
[24]	叶梦旎, 张绪教, 叶培盛, 等. SPOT-6与无人机航测技术在第四纪地质及活动构造填图中的应用-以内蒙古1:50000呼勒斯太苏木等四幅填图试点为例[J]. 地质力学学报, 2016, 22(2):366~378. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20160216&flag=1 YE Meng-ni, ZHANG Xu-jiao, YE Pei-sheng, et al. Application of spot-6 and the UAV aerial technology in quaternary geology and tectonic mapping:taking the 1:50000 mapping pilot of the Hulesitai area, Inner Mongolia as an example[J]. Journal of Geomechanics, 2016, 22(2):366~378. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20160216&flag=1
[25]	徐锡伟, 计凤桔, 于贵华, 等. 用钻孔地层剖面记录恢复古地震序列:河北夏垫断裂古地震研究[J]. 地震地质, 2000, 22(1):9~19. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ200001001.htm XU Xi-wei, JI Feng-ju, YU Gui-hua, et al. Reconstruction of paleoearthouake sequence using stratigraphic records from drill logs:a study at the Xiadian fault, Beijing[J]. Seismology and Geology, 2000, 22(1):9~19. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ200001001.htm
[26]	江娃利. 北京平原夏垫断裂潘各庄钻孔晚更新世晚期以来古地震事件分析[A]. 中国地震局地质研究所. 活动断裂研究[M]. 北京:地震出版社, 2001, 140~147. JIANG Wa-li. Pleoearthquake analysis on the Pangezhuang drill of Xiadianfalut in Beijing plain[A]. Institute of Geology, China Earthquake Administration.Research of the Active Falut[M]. Beijing:Seismological Press, 2001, 140~147.
[27]	邓起东, 徐锡伟, 张先康, 等. 城市活动断裂探测的方法和技术[J]. 地学前缘, 2003, 10(1):93~104. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200301019.htm DENG Qi-dong, XU Xi-wei, ZHANG Xian-kang, et al. Methods and techniques for surveying and prospecting active faults in urban areas[J]. Earth Science Frontiers, 2003, 10(1):93~104. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200301019.htm
[28]	叶培盛, 张绪教, 贾丽云, 等. 内蒙古1:5万呼勒斯太苏木、塔尔湖、复兴城、吉尔嘎郎图填图试点区调报告[R]. 北京:中国地质科学院地质力学研究所, 2017. YE Pei-sheng, ZHANG Xu-jiao, JIA Li-yun, et al. Report of the 1:50, 000 pilot mapping of Hulesitaisumu (K48E017024), Taerhuzhen (K48E018024), Fuxingcheng (K48E019024), and Jiergalangtuxiang (K48E020024)[R]. Beijing:Institute of Geomechanics, Chinese Academy of Geological Sciences, 2017.
[29]	梁兴中, 陈继镛,冯家岷. α石英E'心断代零点研究[J]. 核技术, 1993, 16(4):213~216. http://www.cnki.com.cn/Article/CJFDTOTAL-HJSU199304004.htm LIANG Xing-zhong,CHEN Ji-yong, FENG Jia-min. A study on resetting for E' centre dating of α-quartz[J]. Nuclear Techniques 1993, 16(4):213~216. http://www.cnki.com.cn/Article/CJFDTOTAL-HJSU199304004.htm
[30]	梁兴中, 高钧成. 断裂成矿年龄的α石英ESR研究[J]. 矿物岩石, 1999, 19(2):69~71. http://www.cnki.com.cn/Article/CJFDTOTAL-KWYS902.014.htm LIANG Xing-zhong, GAO Jun-cheng. Study on the α-quartz dating of fault-related ore mineralization[J].Journal of Mineralogy and Petrology,1999, 19(2):69~71. http://www.cnki.com.cn/Article/CJFDTOTAL-KWYS902.014.htm
[31]	梁兴中, 庹先国. 断层最新活动年龄的ESR年代学研究及初步应用[J]. 物理, 1998, (2):114~116. http://www.cnki.com.cn/Article/CJFDTOTAL-WLZZ802.011.htm LIANG Xing-zhong, TUO Xian-guo. Electron spin resonance dating method research and its application on the latest geology fault activity age[J]. Physics, 1998, (2):114~116. http://www.cnki.com.cn/Article/CJFDTOTAL-WLZZ802.011.htm
[32]	程维明, 周成虎. 多尺度数字地貌等级分类方法[J]. 地理科学进展, 2014, 33(1):23~33. doi: 10.11820/dlkxjz.2014.01.003 CHENG Wei-ming, ZHOU Cheng-hu. Methodology on hierarchical classification of multi-scale digital geomorphology[J]. Progress in Geography, 2014, 33(1):23~33. doi: 10.11820/dlkxjz.2014.01.003