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郯城-庐江断裂基本特征及其控盆作用

林宗满

林宗满, 2011. 郯城-庐江断裂基本特征及其控盆作用. 地质力学学报, 17 (4): 322-337.
引用本文: 林宗满, 2011. 郯城-庐江断裂基本特征及其控盆作用. 地质力学学报, 17 (4): 322-337.
LIN Zong-man, 2011. CHARACTERISTICS OF TANCHENG-LUJIANG FAULT AND ITS ROLE ON BASIN CONTROLLING. Journal of Geomechanics, 17 (4): 322-337.
Citation: LIN Zong-man, 2011. CHARACTERISTICS OF TANCHENG-LUJIANG FAULT AND ITS ROLE ON BASIN CONTROLLING. Journal of Geomechanics, 17 (4): 322-337.

郯城-庐江断裂基本特征及其控盆作用

详细信息
    作者简介:

    林宗满(1938-), 男, 中国地质科学院地质力学研究所客座研究员, 专业:石油地质、地质力学

  • 中图分类号: P548

CHARACTERISTICS OF TANCHENG-LUJIANG FAULT AND ITS ROLE ON BASIN CONTROLLING

  • 摘要: 郯城-庐江断裂是中国东部一条规模巨大的断裂构造带, 贯穿中国东部大陆, 向南延伸入南海, 向北抵达俄罗斯境内。郯城-庐江断裂成生于早白垩世晚期, 是一条巨型压扭性断裂带。研究认为, 郯城-庐江断裂不存在巨大平移, 它形成于早白垩世晚期, 并控制K2-E断陷盆地带及其相伴的断隆带的发生、发展; 郯城-庐江断裂是一条活动性断裂构造带, 研究它的基本特征及其控盆作用, 有助于认识中国东部乃至东亚地区晚中生代以来的大地构造属性。

     

  • 图  1  郯庐断裂带新沂—泗洪段地质构造图[6]

    Figure  1.  Geological map of Xinyi-Sihong in Tanlu fault zone

    图  2  山东地区构造体系略图[7]

    1—第四系; 2—古近系; 3—上白垩统; 4—下白垩统; 5—侏罗系; 6—古生界; 7—前震旦系; 8—燕山期花岗岩; 9—印支期花岗岩; 10—新华夏系; 11—华夏系; 12—东西构造带; 13—旋卷构造; 14—山字型构造

    Figure  2.  Simplified structural system map of Shandong Province

    图  3  中国东部构造体系与盆地分布图

    Figure  3.  The distribution of the eastern china tectonic systems and basins

    图  4  安徽省构造体系略图

    1—东西向构造带; 2—华夏系; 3—新华夏系压扭性断裂; 4—山字型构造体系; 5—旋卷构造

    Figure  4.  Simplified structural system map of Anhui Province

    图  5  郯庐断裂带安徽肥东元古宇底层中近直立的断裂挤压带

    Figure  5.  The nearly upright compressive fracture zone of Proterozoic on Tanlu fault zone in Feidong, Anhui province

    图  6  郯庐断裂带数公里宽的挤压破碎裂带(安徽肥东桥头集塔堑)

    Figure  6.  The compressive rupture zone up to several kilometers wide in Tan-lu Fault zone

    图  7  辽南、徐淮震旦纪S形古海盆示意图[11]

    Figure  7.  Schematic diagram of S-shaped ancient marine basin of new-Proterozoic in Liaonan-Xuhuai area

    图  8  安徽省中上三叠统黄马青群等厚图

    1—等厚线/ m; 2—煤层; 3—剖面位置及厚度/ m; 4—参考剖面; 5—不完整剖面; 6—山字型东翼弧边界

    Figure  8.  Isopach map of Huangmaqing group of Mid-upper Triassic in Anhui Province

    图  9  郯城—庐江断裂带中段早白垩世岩浆岩分布简图[13]

    K—K-Ar年龄; Ar—40 Ar / 39 Ar年龄; Rb—Rb-Sr年龄; U—U-Pb年龄

    Figure  9.  Distribution of Early Cretaceous igneous rocks along the middle and southern segments of the Tancheng-Lujiang fault zone

    图  10  柏庄—安庄构造剖面图[10]

    ① —大别山(岩)群; ② —构造岩带; ③ —片理化碎粉岩带; ④ —柔皱带; ⑤ —变形砂岩带; ⑥ —粉砂岩带; ⑦ —含砂岩透镜体粉砂岩带; ⑧ —砂岩

    Figure  10.  Structural cross section from Baizhuang to Anzhuang

    图  11  郯庐断裂带上伸展盆地简图

    1—伸展盆地; 2—伸展盆地时代; 3—伸展断裂; 4—左行平移断裂; 5—盆地沉积边界; 6—剖面位置

    Figure  11.  A sketch map showing extensional basins along the Tancheng-Lujiang fault zone

    图  12  郯庐断裂带上伸展盆地剖面图(剖面位置见图 11)

    Ed—东营组; Es1+2 —沙河街组一、二段; Es3 —沙河街组三段; K2w—王氏组; K1q—青山组; Art—泰山群; γ4 —海西期花岗岩; ηO53(2) —燕山晚期石英二长岩; ξ53(2) —燕山晚期正长岩

    Figure  12.  Cross sections of extensional basins along the Tan-Lu fault zone

    表  1  徐淮与辽南地区有关地层对比[11]

    Table  1.   Correlation of the strata in Xuhuai and Liaonan areas

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  • 收稿日期:  2010-12-03
  • 刊出日期:  2011-12-28

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