Volume 13 Issue 2
Jun.  2007
Turn off MathJax
Article Contents
ZHAO Zhen-xiang, DU Jin-feng, 2007. BASIC CHARACTERISTICS OF THE YANSHAN MOVEMENT IN NORTHEASTERN SHANXI -A SUMMARY OF REGIONAL SURVEY OF THE 1: 250000 YINGXIAN COUNTY SHEET. Journal of Geomechanics, 13 (2): 150-162.
Citation: ZHAO Zhen-xiang, DU Jin-feng, 2007. BASIC CHARACTERISTICS OF THE YANSHAN MOVEMENT IN NORTHEASTERN SHANXI -A SUMMARY OF REGIONAL SURVEY OF THE 1: 250000 YINGXIAN COUNTY SHEET. Journal of Geomechanics, 13 (2): 150-162.

BASIC CHARACTERISTICS OF THE YANSHAN MOVEMENT IN NORTHEASTERN SHANXI -A SUMMARY OF REGIONAL SURVEY OF THE 1: 250000 YINGXIAN COUNTY SHEET

More Information
  • Received: 2006-12-11
  • Published: 2007-06-01
  • The Yanshanian crustal activity in northeastern Shanxi was intense and frequent and underwent a process of extension→transpression→uplift and magmatism.The early stage of the Yanshan movement generated an Early Jurassic downfaulted basin and a Middle Jurassic compressional-downwarped coal-accumulating basin.In the middle stage, the Mid-Late Jurassic witnessed the formation of a volcanic downfaulted basin bounded by NW and NE deep faults, intermediate-basic and acid volcanic eruption and hypabyssal and near-surface intermediate-acid magmatic intrusion, and the terminal Late Jurassic witnessed the formation of a number of NNE-trending folds and overthrust zones.In the late stage, in the Early Cretaceous a downfaulted basin and open gentle folds once again formed and the Yixian Formation unconformably rested on volcanic rocks; the Late Cretaceous was a stage of mountain uplift after compressional orogeny, when the Yixian Formation was unconformably overlain by the Zuoyun Formation, accompanied by intrusion of crust-derived granite, and NE-and NE-trending faults were revived, forming a graben-and horst-type fault combination and resulting in mountain uplift.

     

  • loading
  • [1]
    翁文灏.中国东部中生代以来之地壳运动及火山活动[J].中国地质学会会志, 1927, 6 (1):9~36. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000000376384
    [2]
    谢家荣.北平西山地质构造概况[J].中国地质学会会志, 1936, 15 :61~74.
    [3]
    黄汲清.中国地质构造基本特征的初步总结[J].地质学报, 1960, 40 :1~37. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000000377248
    [4]
    赵宗溥.中国东部的燕山运动[J].地质科学, 1963, (3):128~138. http://d.old.wanfangdata.com.cn/Periodical/OA000004417
    [5]
    任纪舜, 陈廷愚, 牛宝贵, 等.中国东部及邻区大陆岩石圈的构造演化与成矿[M].北京:科学出版社, 1990 : 217.
    [6]
    马杏垣, 刘和甫, 王维襄, 等.中国东部中、新生代裂陷作用和伸展构造[J].地质学报, 1983, (1):22~32. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000000377681
    [7]
    王鸿祯, 杨森楠, 李思田.中国东部及邻区新生代盆地发育及大陆边缘区的构造发展[J].地质学报, 1983, 57 (3):213~223. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000000377699
    [8]
    崔盛芹, 吴珍汉, 王建平, 等.华北陆块北缘构造运动序列及区域构造格局[M].北京:地质出版社, 2000 : 326.
    [9]
    赵越.燕山地区中生代造山运动及构造演化[J].地质论评, 1990, 36 (1):1~12. doi: 10.3321/j.issn:0371-5736.1990.01.001
    [10]
    马寅生, 崔盛芹, 曾庆利, 等.燕山地区燕山期的挤压与伸展作用[J].地质通报, 2002, 21 (4/5), 218~223. http://d.old.wanfangdata.com.cn/Periodical/zgqydz200204007
    [11]
    赵越, 崔盛芹, 郭涛, 等.北京西山侏罗纪盆地演化及其构造意义[J].地质通报, 2002, 21 (4/5), 211~217. http://d.old.wanfangdata.com.cn/Periodical/zgqydz200204006
    [12]
    崔盛芹, 吴珍汉, 马寅生, 等.北京地区中新生代陆内造山过程———以十三陵—龙庆峡—八达岭路线观察为基础[J].地质力学学报, 2003, 9 (3):201~219. doi: 10.3969/j.issn.1006-6616.2003.03.002
    [13]
    刘成第, 朱道尊.鹅毛口逆掩断层与推覆体[J].构造地质论丛, 1986 (6):63~70.
    [14]
    武铁山, 吕花荣, 李忠和.试论山西燕山期花岗岩的成因类型[J].山西地质, 1987, 2 (1):9~29.
    [15]
    山西省地质矿产局.山西省岩石地层[M].武汉:中国地质大学出版社, 1997.
    [16]
    陈晋镳, 武铁山.华北区区域地层[M].武汉:中国地质大学出版社, 1997:100~103.
    [17]
    贾炳文.大同侏罗纪含煤地层沉积环境与聚煤特征[M].北京:科学出版社, 1991:86~88.
    [18]
    刘德佑, 胡学智.山西灵丘太白维山推覆构造[J].山西地质, 1987, 2 (2):29~32.
    [19]
    周永娴, 张文陆.山西省重磁资料的初步研究[J].山西地质, 1989, 4 (2):111~114.
    [20]
    任纪舜.从全球看中国大地构造—中国及邻区大地构造图简要说明[M].北京:地质出版社, 1999.
  • 加载中

Catalog

    Figures(15)  / Tables(2)

    Article Metrics

    Article views (354) PDF downloads(9) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return