中国地质调查局西安地质调查中心主办
高级检索

渭河盆地安仁镇图幅(1：5万)的浅部地质结构特征

,  ,  ,  , 

文章导航 > 西北地质 > 2020 > 53(3): 93-105

上一篇

下一篇

乔建伟, 卢全中, 郑建国, 刘争宏, 刘聪. 2020. 渭河盆地安仁镇图幅(1：5万)的浅部地质结构特征. 西北地质, 53(3): 93-105. doi: 10.19751/j.cnki.61-1149/p.2020.03.008
引用本文: 乔建伟, 卢全中, 郑建国, 刘争宏, 刘聪. 2020. 渭河盆地安仁镇图幅(1：5万)的浅部地质结构特征. 西北地质, 53(3): 93-105. doi: 10.19751/j.cnki.61-1149/p.2020.03.008
shu
QIAO Jianwei, LU Quanzhong, ZHENG Jianguo, LIU Zhenghong, LIU Cong. 2020. Shallow Structural Model of Anren Town Geological Map (1:50000) in Wei River Basin. Northwestern Geology, 53(3): 93-105. doi: 10.19751/j.cnki.61-1149/p.2020.03.008
Citation: QIAO Jianwei, LU Quanzhong, ZHENG Jianguo, LIU Zhenghong, LIU Cong. 2020. Shallow Structural Model of Anren Town Geological Map (1:50000) in Wei River Basin. Northwestern Geology, 53(3): 93-105. doi: 10.19751/j.cnki.61-1149/p.2020.03.008
shu

渭河盆地安仁镇图幅(1：5万)的浅部地质结构特征

  • 1. 机械工业勘察设计研究院有限公司, 陕西 西安 710043;

  • 2. 陕西省特殊岩土性质与处理重点实验室, 陕西 西安 710043;

  • 3. 长安大学地质工程与测绘学院, 陕西 西安 710054;

  • 4. 西部矿产资源与地质工程教育部重点实验室, 陕西 西安 710054

  • 基金项目:

    CMEC科技孵化项目“一带一路沿线国家工程建设条件与应用”（CMEC-KJFH-2018-02），中国地质调查局水工环调查项目“关中盆地渭南地区地裂缝地质灾害调查”（DD20160264），国家自然科学基金面上项目“同沉积作用下地裂缝破裂扩展机理及效应研究”（41877250）

详细信息
    作者简介: 乔建伟(1990-),男,工学博士,工程师,主要从事地质灾害和岩土工程性质方面的研究工作。E-mail:15029207728@163.com

  • 中图分类号: P642;P56

Shallow Structural Model of Anren Town Geological Map (1:50000) in Wei River Basin

  • 1. China Jikan Research Institute of Engineering Investigations and Design, Co., Ltd., Xi'an 710043, Shaanxi, China;

  • 2. Shaanxi Key Laboratory for the Property and Treatment of Special Soil and Rock, Xi'an 710043, Shaanxi, China;

  • 3. School of Geological Engineering and Geomatics, Chang'an University, Xi'an 710054, Shaanxi, China;

  • 4. Key Laboratory of Western China Mineral Resources and Geological Engineering, Xi'an 710054, Shaanxi, China

    摘要
  • 地球浅表部是支撑和维持人类经济社会发展的关键区域，其不仅为人类提供赖以生存的资源需求，还是地质灾害如滑坡、崩塌、泥石流、地面沉降和地裂缝等发生的地质载体。笔者以渭河盆地安仁镇图幅（1：5万）为研究对象，运用野外地质调查、地球物理勘探和工程地质钻探等手段揭示了安仁镇图幅的地貌特征、地层岩性和断裂构造，在此基础上概括了该区的地质结构特征。主要取得以下认识：①双泉-临猗断裂和韩城-华阴断裂将研究区划分为3个地貌单元，即黄土台塬、渭河冲积阶地和黄河冲积平原。各地貌单元地层岩性均可按水文特性划分为隔水层和含水层。②渭河冲积阶地浅部发育4条隐伏正断裂，断裂的位错量随着深度的增加而显著增加，属于典型的生长断层；断裂控制了该区地貌和微地貌的演化过程及地裂缝的发育位置。③安仁镇的浅部地质结构具有以下特征：隔水层与含水层相间分布，隐伏断裂发育其中，浅地表破裂严重。本项研究可为分析该区地质灾害成因、评估地质环境承载力、合理开采地下水和保护生态环境等相关研究提供技术支撑。
    The superficial part of the earth is a key area to maintain human economic development. It not only provides human resources for survival, but also is an engineering carrier of geological hazards, such as landslides, collapses, mudslides, land subsidence and ground fissures. This paper selects Anren town map (1∶50000) as research object and uses series of geological investigation,i.e., field geological survey, geophysical exploration and geological drilling to investigate the geomorphic features, stratum lithology and the fault structure of the geological structure in this area. the main conclusions are as follows: (1) the study areas can be divided into three geomorphic units of loess platform, alluvial terraces of Wei River and alluvial terraces of Yellow River by Shuangquan-Linyi fault and Hancheng-Huayin fault. The lithology of each geomorphic unit is either aquiclude or aquiclude according to hydrological characteristics. (2) Four normal buried faults developed in the shallow alluvial terrace of Wei River, the displacement increasing significantly with their depth and belonging to typical growth fault. Buried faults decide the process of geomorphology and micro-geomorphology and the developing positions of the ground fissures in this area. (3) The shallow geological structure of Anren town is characterized as interphase distribution of water-resisting layer and aquifer, development of buried faults and severe rupture of shallow surface. This paper gives technical support for analyzing the geological disasters, evaluating the carrying capacity of the geological environment, and rationally exploitation of groundwater and ecological environment protection as well.
    • HTML全文
  • 加载中
    • 参考文献(54)

  • 张猛刚,雷祥义. 地球表层系统浅论[J]. 西北地质,2005,38(2):99-101.

    ZHANG Menggang, LEI Xiangyi. A discussion on the earth surface system[J]. Northwestern Geology, 2005, 38(2):99-101.

    黄润秋. 20世纪以来中国的大型滑坡及其发生机制[J]. 岩石力学与工程学报, 2007, 26(03):433-454.

    HUANG Runqiu. Large-Scale Landslides and Their Sliding Mechanisms in China Since the 20thCentury[J]. Chinese Journal of Rock Mechanics and Engineering, 2007, 26(03):433-454.

    彭建兵,范文,李喜安,等. 汾渭盆地地裂缝成因研究中的若干关键问题[J]. 工程地质学报, 2007, 15(4):433-440.

    PENG Jianbing, FAN Wen, LI Xian, et al. Key problems in the causative mechanism research of ground fissures in Fenwei basin[J]. Journal of Engineering Geology, 2007, 15(4):433-440.

    崔鹏. 我国泥石流防治进展[J]. 中国水土保持科学, 2009, 7(5):7-13, 31.

    CUI Peng. Advances in debris flow prevention in China[J]. Science of Soil and Water Conservation, 2009, 7(5):7-13, 31.

    化建新,郑建国,等. 工程地质手册(第五版)[M]. 北京:中国建筑工业出版社, 2018.

    HUA Jianxin, ZHENG Jianguo, et al.Engineering geology manual[M]. Beijing:China Architecture & Building Press, 2018.

    何登发,单帅强,张煜颖,等. 雄安新区的三维地质结构:来自反射地震资料的约束[J]. 中国科学:地球科学, 2018, 48(09):1207-1222.

    HE Dengfa, SHAN Shuaiqiang, ZHANG Yuying, et al. 3-D geologic architecture of Xiong'an New Area:Constraints from seismic reflection data[J]. Science China Earth, Science, 2018, 48(09):1207-1222.

    陈志新,袁志辉,彭建兵,等. 渭河盆地地裂缝发育基本特征[J]. 工程地质学报, 2007, 15(04):441-447.

    CHEN Zhixin, YUAN Zhihun, PENG Jianbing, et al. Basic Characteristics about Ground Fractures' Development of Weihe Basin[J]. Journal of Engineering Geology, 2007, 15(04), 441-447.

    杜蕾,谢婉丽. 城市地质环境承载力研究进展及展望[J]. 防灾科技学院学报, 2018, 20(2):15-20.

    DU Lei, XIE Wanli. Research Progress and Prospect of Urban Geological Environment Carrying Capacity[J]. Journal of Institute of Disaster Prevention, 2018, 20(2):15-20.

    张茂省,王尧. 基于风险的地质环境承载力评价[J]. 地质通报,2018,37(2-3):467-475.

    ZHANG Maosheng, WANG Xiao. Research on the evaluation of the carrying capacity of geological environment based on its risk level[J]. Geological Bulletin of China, 2018, 37(2-3):467-475.

    张茂省,王化齐,王尧,等. 中国城市地质调查进展与展望[J]. 西北地质,2018, 51(4):1-9.

    ZHANG Maosheng, WANG Qihua, WANG Yao, et al. Progress and prospect of urban geological survey in China[J]. Northwestern Geology, 2018, 51(4):1-9.

    王斌. 渭河盆地新生代沉积演化盆山耦合与风尘沉积[D]. 南京大学, 2014.

    WANG Bin. Cenozoic sedimentary evolution of the Weihe basin:Basin-Orogen coupling and eolian sediments[D]. Nanjing University, 2014.

    刘林,芮会超,杨莉. 渭河单冲压陷盆地的厘定及其控藏作用[J]. 西北地质, 2018, 51(2):186-202.

    LIU Lin, RUI Huichao, YANG Li. Definition of the Weihe single-thrusting compressional basin and its reservoir-forming condition[J].Northwestern Geology, 2018, 51(2):186-202.

    张世民. 汾渭地堑系盆地发育进程的差异及其控震作用[J]. 地质力学学报, 2000, 02:30-37.

    ZHANG Shimin. Basin evolutionary differences and seismotectonics of Fenwei graben system[J].Journal of Geomechanics, 2000, 02:30-37.

    王景明.渭河地堑断裂构造研究[J]. 地质论评, 1984, (03):217-223.

    WANG Jingming. A study on the tectonics of Weihe graben[J]. Geological Review, 1984, (03):217-223.

    易明初. 新构造运动及渭延裂谷构造[M]. 北京:地震出版社, 1993.

    YI Mingchu. Neotectonic movement and Weihe rift structure[M]. Beijing:Seismological Press, 1993.

    任隽.渭河盆地深部地壳结构探测与盆地构造研究[D]. 西安:长安大学,2012.

    REN Jun.Deep crustal structure exploration and basin structure study in the Weihe Basin[D]. Xi'an:Chang'an University, 2012.

    瞿伟,张勤,王庆良,等. 渭河盆地现今地壳水平形变特征及区域构造活动性[J]. 武汉大学学报(信息科学版), 2011, 36(07):830-834.

    QU Wei, ZHANG Qin, WANG Qingliang, et al. Research on present crustal horizontal deformation feature of Weihe Basin and its tectonic activity[J]. Geomatics and Information Science of Wuhan University, 2011, 36(7):830-834.

    权新昌. 渭河盆地断裂构造研究[J]. 中国煤田地质, 2005, 17(03):1-4,8.

    QUAN Xinchang. Weihe basin faulted structure study[J]. Coal Geology of China, 2005, 17(03):1-4,8.

    刘志武,周立发. 渭河盆地新生代构造-沉积格局与油气成藏潜力初探[J]. 福州大学学报(自然科学版), 2015, 43(05):708-714.

    LIU Zhiwu, ZHOU Lifa. The Cenozoic tectonic and sedimentary framework and preliminary study on the hydrocarbon accumulation potential of the Weihe basin[J]. Journal of Fuzhou University (Natural Science Edition), 2015, 43 (05):708-714.

    彭建兵,张俊,苏生瑞,等. 渭河盆地活动断裂与地质灾害[M]. 西安:西北大学出版社,1992.

    PENG Jianbing, ZHANG Jun, SU Shengrui, et al. Active fault and Geo-hazard in Weihe Basin[M]. Xi'an:Northwestern University Press, 1992.

    刘瑞平,朱桦,杨炳超,等. 大荔潜水含水层中氟的赋存规律及水化学成因[J]. 西北地质,2008, 41(4):134-140.

    LIU Runping, ZHU Hua, YANG Bingchao, et al. Occurrence pattern and hydrochemistry cause of the shallow groundwater fluoride in the Dali county, Shaanxi province[J]. Northwestern Geology, 2008, 41(4):134-140.

    王景明. 关中平原区的新华夏系构造[J]. 西北地震学报, 1981, 3(02):69-77.

    WANG Jingming. The neocathaysian structural system of Guanzhong plain[J]. Northwestern Seismological Journal, 1981,3(02):69-77.

    乔建伟. 基于地球关键带理论的渭北台塬地裂缝成因机理研究[D]. 西安:长安大学,2018.

    QIAO Jianwei. Study on the formation mechanism of ground fissures in Weibei terrace based on earth's critical zone theory[D]. Xi'an:Chang'an University, 2018.

    李高阳,李陈侠,李晓妮. 1501年渭南朝邑7.0级地震发震断裂初探[J]. 华南地震, 2018, 38(S1):108-111.

    LI Gaoyang, LI Chenxia, LI Xiaoni. Preliminary study on the seismogenic faults of Chaoyi M7.0 earthquake in 1501[J]. South China Journal of Seismology, 2018, 38(S1):108-111.

    杜建军. 渭河盆地东南缘主要断裂晚更新世以来的活动性和灾害效应[D]. 北京:中国地质科学院,2016.

    DU Jianjun. Activity of main faults and related geohazard effects in Southeast of Weihe basin[D]. Beijing:Chinese Academy of Geological Sciences, 2016.

    National Research Council. New research opportunities in the earth science[M]. Washington DC:National Academy Press, 2001.

    NSF. Frontiers in Exploration of the Critical Zone[R/OL]. 2005. http://www.czen.org/file/czen/EZEN_Booklet.pdf.

    LIN H. Earth's critical zone and hydropedology:concepts, characteristics and advance[J]. Hydrology and Earth System Science, 2010, 14:25-45.

    QIAO JW, PENG JB, DENG YH, et al. Earth fissures in Qinglong Graben in Yuncheng Basin, China[J]. Journal of Earth System Science, 2018, 127:10.

    • 相关文章
  • 施引文献
  • 资源附件(0)
  • 加载中
计量
  • 文章访问数:  853
  • PDF下载数:  462
  • 施引文献:  0
出版历程
收稿日期:  2019-04-04
修回日期:  2019-10-30

目录

    版权所有：中国地质调查局发展研究中心 copyright @2020
    返回