| 有关内蒙古地质构造的一线之见——江苏响水至内蒙古满都拉地学断面北段研究报道之一 |
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| 引用本文： | 马杏垣,王楫,李双庆,刘德简,白云虹,周春平,黄国华.有关内蒙古地质构造的一线之见——江苏响水至内蒙古满都拉地学断面北段研究报道之一[J].地震地质,1988,10(4):45. |
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| 作者姓名： | 马杏垣 王楫 李双庆 刘德简 白云虹 周春平 黄国华 |
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| 作者单位： | 国家地震局地质研究所
(马杏垣，白云虹，周春平)，内蒙古自治区地矿局地质研究队
(王楫)，内蒙古自治区地震局
(李双庆，刘德简)，国家地震局地质研究所(黄国华) |
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| 摘 要： | 本文概述了江苏响水至内蒙古满都拉地学断面北段——包头至满都拉的地质观察结果。内容包括从太古宙乌拉山群到第四系、基底构造到新构造特征的七个方面。重点论述了渣尔泰群和白云鄂博群的构造性质,它们约在14亿年前才褶皱回返,代表了华北地台基底固结最迟的地段。造成这一事件的构造运动,拟称为色尔腾运动。此外,还讨论了华北地台北侧陆缘区加里东期和华力西期的构造
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| 关 键 词： | 地学断面 坳拉槽 地斜 |
A REPORT OF GEOLOGICAL OBSERVATIONS ON NORTHERN SEGMENT (BAOTOU TO MONDULA) OF THE GEOSCIENCE TRANSECT FROM XIANGSHUI,JIANGSU, TO MANDULA, NEI MONGGOL |
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| Ma Xing-yuan,Wang Ji,Li Shuangqing,Liu De-jian Bai Yun-hong,Zhou Chun-ping,Huang Guo-hua Institute of Geology,State Seismological Bureau. Geological Investigation Team of Nei Mongol Autonomous Region Bureau of Geology and Mineral Resources. Seismological Bureau of Nei Mongol Autonomous Region..A REPORT OF GEOLOGICAL OBSERVATIONS ON NORTHERN SEGMENT (BAOTOU TO MONDULA) OF THE GEOSCIENCE TRANSECT FROM XIANGSHUI,JIANGSU, TO MANDULA, NEI MONGGOL[J].Seismology and Geology,1988,10(4):45. |
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| Authors: | Ma Xing-yuan Wang Ji Li Shuangqing Liu De-jian Bai Yun-hong Zhou Chun-ping Huang Guo-hua Institute of Geology State Seismological Bureau Geological Investigation Team of Nei Mongol Autonomous Region Bureau of Geology and Mineral Resources Seismological Bureau of Nei Mongol Autonomous Region |
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| Institution: | Ma Xing-yuan,Wang Ji,Li Shuangqing,Liu De-jian Bai Yun-hong,Zhou Chun-ping,Huang Guo-hua 1) Institute of Geology,State Seismological Bureau.2) Geological Investigation Team of Nei Mongol Autonomous Region Bureau of Geology and Mineral Resources.3) Seismological Bureau of Nei Mongol Autonomous Region. |
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| Abstract: | Geological and structural features from Archaean to neotectonics along the Geosci-ence Transect corridor from Baotou to Mandula have been accounted. Particular attention has been paid to the middle Proterozoic Chartai aulacogen and Bayan Obo geocline. Both of them were folded during the Seerteng movement about 1400 Ma ago and became the latest consolidated part of the North China platform basement. The Caledonian and Variscan fold belts of the northern marginal tracts have also been discussed |
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| Keywords: | Geoscience transect Aulacogen Geocline |
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