ISSN 1009-6248CN 61-1149/P Bimonthly

Supervisor：China Geological Survey

Sponsored by：XI'an Center of China Geological Survey
Geological Society of China

    • The Core Journals of China
    • The Key Magazine of China Technology
    • CSCD Included Journals
    • Scopus Included Journals
Advance Search
LI Jian-xing, WANG Yong-he, XIAO Pei-xi, et al. The relation between the Altyn Tagh fault and the Cenozonic basin[J]. Northwestern Geology, 2005, 38(2): 19-23.
Citation: LI Jian-xing, WANG Yong-he, XIAO Pei-xi, et al. The relation between the Altyn Tagh fault and the Cenozonic basin[J]. Northwestern Geology, 2005, 38(2): 19-23.
shu

The relation between the Altyn Tagh fault and the Cenozonic basin

  • 1.

    Department of Geology, Northwest University, Xi'an 710069, China;Xi'an Institute of Geology and Mineral Resources, Xi'an 710054, China

  • 2.

    Xi'an Institute of Geology and Mineral Resources, Xi'an 710054, China;Faculty of Earth Sciences, China University of Geosciences, Wuhan, 430074, China

  • 3.

    Xi'an Institute of Geology and Mineral Resources, Xi'an 710054, China

More Information
  • Received Date: March 03, 2005
  • Revised Date: April 14, 2005
  • Published Date: June 04, 2005
    Graphical Abstract
    • Abstract
  • We mapped some Cenozonic strata in Suwushenjie, neighbouring the Altyn Tagh. According to the relation of the distribution of these strata to the Altyn Tagh fault, we believe that the Altyn Tagh did not slip in the early-mid Jurassic and the Jurassic was not controlled by the Altyn Tagh fault; the Altyn Tagh fault began to controlled sedimentation basin since Eocene.It is indicated that the Altyn Tagh fault had slipped in that time. Quaternary deposit is the main sedimentation of the Wuzunxiaoer(the west part of Xorkol)basin. The southea stedge of the basin is controlled by the main Altyn Tagh;on southwest edge,the westeast strike and dip north normal fault confined Quaternary deposit;the north part of the basin is westeast strike and dip north fault which is a dextral strike slip and brittle fault. The west edge of the basin overlapped on bed rock,there is not any sub stantive relation with the Altyn Tagh fault.
    • FullText(HTML)
    • References (17)
  • 国家地震局阿尔金活动断裂课题组.阿尔金活动断裂[M].北京:地震出版社,1992.
    任收麦,葛肖虹,刘永江.晚白垩世以来沿阿尔金断裂带的阶段性走滑隆升[J].地质通报,2004,23(9-10).
    王萍,卢演俦,陈杰.阿尔金断裂东端的旋转构造及其动力学意义[J].中国地震,2004,20(2).
    向宏发,虢顺民,张晚霞,等.阿尔金断裂带东段第四纪以来的水系位错与滑动速率[J],2000,22(2).
    刘永江,叶慧文,葛肖虹,等.阿尔金断裂带变形岩激光微区40Ar/39Ar年龄[J],科学通报,2000,45(19).
    陈文,葛肖虹,叶慧文,等.用激光微区40Ar/39Ar定年技术测定阿尔金断裂系多期活动的时代[J].质谱学报,2000,21(3、4).
    刘永江,葛肖虹,J.censer,等.阿尔金断裂构造活动40Ar/39Ar年龄证据[J].2003,48(12).
    李海兵,杨经绥,史仁灯,等.阿尔金走滑断陷盆地的确定及其与山脉的关系[J].2002,47(1).
    崔军文,张晓卫,李鹏武,等.阿尔金断裂:几何学、性质和生长方式[J].地球学报,2003,23(6).
    郭召杰,张志诚,王建君.索尔库里盆地的形成、演化及其与阿尔金断裂带的关系研究[J].高校地质学报,1998,4(1).
    中国地质调查局,阿尔金-昆仑山地区区域地质调查成果与进展[J].地质通报,2004,23(1).
    崔军文,唐哲民,邓晋福,等.阿尔金断裂系[M].北京:地质出版社,1996.
    王有学,韩果花,姜枚,等.阿尔泰-阿尔金地学断面地壳结构[J].地球物理学报,2004,47(2).
    刘永江,葛肖虹,叶慧文,等.晚中生代以来阿尔金断裂的走滑模式[J].地球学报,2001,22(1).
    刘海涛,马立祥,葛肖虹,等.阿尔金断裂的研究现状及其控油意义[J].西安石油学院学报(自然科学版),2003,18(6).
    王永和,等."阿尔金群"的解体与阿尔金杂岩特征[J].西北地质,2002,35(4).
    校佩曦,等.阿尔金山中段苏吾什杰岩体(群)地质特征[J].西北地质,2003,36(3).
    • Related Articles

  • Related Articles

    LI Lin, ZHU Lifeng, LI Zhengguo, LI Ke, LI Qing. 2022: Technology Research on the Constructing of Urban Geological 3D Model in Condition of Complex Faults. Northwestern Geology, 55(4): 133-139. DOI: 10.19751/j.cnki.61-1149/p.2022.04.012
    CHEN Guo-zhong, LIANG Zhi-lu, MA Hong-shun, ZHANG Yuan-ning, WANG Jian-long, LI Peng-bing. 2013: The Establishment of Geological Model and Totalresources Estimate of the Zaozigou Gold Deposit, Hezuo, Gansu Province. Northwestern Geology, 46(4): 173-181.
    SHEN Gui-chun, DU ZHONG-wei, ZHANG Xian-fu, CHAO Chen-gang. 2012: Application of High-precision Magnetic Survey in the Exploration of the Iron-polymetallic Deposit in West Nalinggele River of Qinghai, and Its Geological Characteristics. Northwestern Geology, 45(1): 293-297.
    ZHNA WEN-quan, ZHANG Ai-kui, MENG Jun-hai, GUO Kun-ming, MA Jin-zhong. 2012: Application Inversion technology into Dune with High-Precision Magnetic Survey. Northwestern Geology, 45(1): 277-282.
    FENG Xu-hui, LI Bai-shun, REN Jin-li, GAO Yong-hao. 2010: Probe into the Gradient Correction in Pre-processing of Magnetic Data. Northwestern Geology, 43(2): 150-155.
    KOU Yu-cai, LI Zhan-ye, WANG Ying-xiao, MENG Jun-hai. 2010: Geologic-Geophysical Model of Skarn Iron-Polymetallic Deposit in Galinge Region. Northwestern Geology, 43(2): 20-31.
    ZHAO Guang-jiang, HOU Yu-shu, YANG Ji-quan. 2006: Geological Characteristics and Metallogenic Model of Ershiyizhan Gold and Copper Deposits in Heilongjiang Province. Northwestern Geology, 39(4): 33-39.
    CAO De-zhi, WANG Yu-de, MA Zhan-lan, ZHAO Ren-fu. 2006: Geological Characteristics and Prospecting Model of the Guomis-Gadaban Metallogenic Zone. Northwestern Geology, 39(3): 12-19.
    ZHAO Shi-jun, ZHAO Xi-kui, YANG Shao-chun. 2005: Similar analysis of geological structure physical model. Northwestern Geology, 38(4): 14-18.
    KANG Xian. 2002: Geological model on the Lower Paleozoic carbonate reservoir in Ortos basin. Northwestern Geology, 35(3): 106-112.

Catalog

    Get Citation
    PDF
    XML
    Article views (2691) PDF downloads (3488) Cited by()
    Turn off MathJax
    Article Contents
    Abstract
    References
    Related Articles

    Address：No. 555 Cangtai West Road, Chang'an District, Xi'an 710119, ChinaPostCode：710119

    Tel：+86-29-89238533E-mail： xbdzbjb@163.com

    Copyright : Editorial Office of Northwestern Geology陕ICP备13001446号

    Supported by: Beijing Renhe Information Technology Co., Ltd.  Baidu Analytics

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return