内蒙古苏左旗南部华北板块北缘中新元古代—古生代裂解—汇聚事件的地质记录

张臣 吴泰然. 内蒙古苏左旗南部华北板块北缘中新元古代—古生代裂解—汇聚事件的地质记录[J]. 岩石学报, 2001, 17(2): 199-205.
引用本文: 张臣 吴泰然. 内蒙古苏左旗南部华北板块北缘中新元古代—古生代裂解—汇聚事件的地质记录[J]. 岩石学报, 2001, 17(2): 199-205.
ZHANG Chen and WU TaiRanDepartment of Geology,Peking University,Beijing 100871,China. Crack and assembly events of Meso-Neoproterozoic-Palaeozoic continental blocks in the sourthern area of Suzuoqi, Inner Mongolia[J]. Acta Petrologica Sinica, 2001, 17(2): 199-205.
Citation: ZHANG Chen and WU TaiRanDepartment of Geology,Peking University,Beijing 100871,China. Crack and assembly events of Meso-Neoproterozoic-Palaeozoic continental blocks in the sourthern area of Suzuoqi, Inner Mongolia[J]. Acta Petrologica Sinica, 2001, 17(2): 199-205.

内蒙古苏左旗南部华北板块北缘中新元古代—古生代裂解—汇聚事件的地质记录

  • 基金项目:

    国家自然科学基金(编号:40072072)资助项目.

Crack and assembly events of Meso-Neoproterozoic-Palaeozoic continental blocks in the sourthern area of Suzuoqi, Inner Mongolia

  • 内蒙古苏左旗南部温都尔庙群是不同时代、不同环境下的岩石组合经构造作用拼贴在一起的构造拼贴体。根据岩石组合、岩石地球化学和同位素年龄将其解体为古元古代宝音图解、中、新元古代温都尔庙群和早古生代蛇绿混杂堆积。宝音图群为陆缘拉张解体阶段源自结晶基底的裂解古陆块。中、新元古代温都尔庙群及赋存在早古生代蛇绿混杂堆积中的超镁铁岩、基性火山岩和硅质岩的洋壳组合代表中、新元古代-早古生代陆缘拉张解体阶段的拉张过渡壳,早古生代末-晚古生代初,本区构造体制由拉张转化为挤压,苏左旗南部出露的蛇绿混杂岩带以及大量的蚀变闪长岩、英云闪长岩、花岗闪长岩、二长花岗岩和钾长花岗岩代表本区晚古生代会聚阶段的挤压性过渡壳。
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  • [1]

    [1]Bureau of Geology and Mineral Resources of Inner Mongolia Autonomous Aegion. 1991. Regional Geology of Inner Mongolia Autonomous Region. Beijing: Geological Publishing House (in Chinese)

    [2]

    [2]Department of Peking University. 1993. Synopsis of 1 : 50000geological map on Erdenibulage and Baiyinbaolidao region (in Chinese)

    [3]

    [3]Hu Xiao, Xu Chuanshi and Niu Shuyin. 1990. Evolution of the early Paleozoic continental margin in northern margin of the north China Platform. Beijing: Peking University Publishing House (in Chinese)

    [4]

    [4]Li Shujing and Gao Dezhen. 1995. New discoveries of geological structures in Sonid Zuoqi of Inner Mongolia and discussion on tectonic features. Geoscience, 9(2): 130- 141 (in Chinese with English abstract )

    [5]

    [5]Shao Ji′ an. 1991. Crust evolution in the middle part of the northern margin of Sino Korean Plate. Beijing: Peking University Publishing House (in Chinese)

    [6]

    [6]Shen Baofeng and Luo Hui. 1981. The geology of metamorphosed marine volcano-outflow iron deposits of Baorihan and other districts in Xilin Gol Meng of Neimonggol. Bull. Tianjing Inst.Geol. M. R. , Chinese Acad. Geol. Sci. , 3:31-47 (in Chinese with English abstract)

    [7]

    [7]Tang Kedong. 1992. Tectonic evolution and minerogenetic regularities of the fold belt along the northern margins of Sino Korean plate. Beijing: Peking University Publishing House (in Chinese)

    [8]

    [8]Wang Quan, Liu Xueya, and Li Jinyi. 1991. Plate tectonics between Cathaysia and Angaraland in China. Beijing: Peking University Publishing House. 1-151 (in Chinese)

    [9]

    [9]Xiao Rongge, Sui Decai, Luo Zhaohua, Zhang Weijie and Li Shujing. 1995. Discovery of Early Proterozoic metamorphic complex in north Inner Mongolia. Geoscience, 9 (2) : 142 - 148(in Chinese with English abstract)

    [10]

    [10]Xu Bei, Chen Bin, Zhang Chen and Bai Zhiqiang. 1994. Sm-Ndisochron and significance of the Wuhuaaobao block in northern margin of Sino-Koren Plate. Scientia Geologica Sinica, 29(2): 168~172 (in Chinese with English abstract)

    [11]

    [11]Xu Bei, Chen Bin, Zhang Chen and Bai Zhiqiang. 1994. The age and tectonic significance of ferrian metamorphic series in the middle segment of the northern margin of the North China Plate.Geological Review, 40(4): 307- 311 (in Chinese with English abstract)

    [12]

    [12]Zhang Chen, Wu Tairan. 1999. Features and tectonic implications of the ophiolitic melange in the southern Suzuoqi, Inner Mongolia. Scientia Geologica Sinica, 34 (3): 381 - 389 (in Chinese with English abstract)

    [13]

    [13]Zhang Chen, WuTairan. 1999. Rock assemblage of Baiyinduxi group and its tectonic interpretation in Boin Sum region Inner Mongolia. Geological Journal of China Universities. 5 (2): 175-182 (in Chinese with English abstract)

    [14]

    [14]北京大学填图队.1993.额尔德尼布垃格幅、白音宝力道幅1/5万地质图说明书

    [15]

    [15]胡晓,许传诗,牛树银.1009.华北地台北缘早古生代大陆边缘演化.北京:北京大学出版社

    [16]

    [16]李述靖,高德臻.1995.内蒙古苏尼特左旗地区若干地质构造新发现及其构造属性的初步探讨.现代地质,9(2):130-141

    [17]

    [17]内蒙古自治区地质矿产局.1991.内蒙古自治区区域地质志.北京:地质出版社

    [18]

    [18]邵济安.1991.中朝板块北缘中段地壳演化.北京:北京大学出版社沈保丰,骆辉.1981.内蒙古锡盟包日汗等地变质海相火山喷溢型铁矿的地质特征.中国地质科学院天津地质矿产研究所所刊第3号,31-47

    [19]

    [19]唐克东等.1992.中朝板块北侧褶皱带构造演化及成矿规律.北京:北京大学出版社

    [20]

    [20]王荃,刘雪亚,李锦轶.1991.中国华夏与安加拉古陆间的板块构造.北京:北京大学出版社

    [21]

    [21]肖荣阁,隋德才,罗照华等.1995.内蒙古北部早元古代变质岩系的发现及其岩石学研究.现代地质,9(2):142-148

    [22]

    [22]徐备,陈斌,张臣等.1994.华北板块北缘中段含铁变质岩系的时代和构造环境初探.地质论评,40(4):307-311.

    [23]

    徐备,陈斌,张臣等.1994.中朝板块北缘乌花敖包地块Sm-Nd同位素等时线年龄及其意义.地质科学,29(2):168-172

    [24]

    [24]张臣.1999.内蒙古苏尼特左旗侵入岩谱系单位划分及岩浆演化特征.中国区域地质,18(1):46-53

    [25]

    [25]张臣,吴泰然.1999.内蒙古苏左旗南部早古生代蛇绿混杂岩特征及其构造意义.1999.地质科学,34(3):381-389

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出版历程
修回日期:  2000-12-06
刊出日期:  2001-05-31

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