| 郯城-庐江断裂基本特征及其控盆作用 |
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| 引用本文： | 林宗满.郯城-庐江断裂基本特征及其控盆作用[J].地质力学学报,2011,17(4):322-337. |
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| 作者姓名： | 林宗满 |
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| 作者单位： | 中国地质科学院地质力学研究所, 北京 100081 |
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| 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。
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| 关 键 词： | 郯城—庐江断裂 左行平移 压扭性断裂 控盆作用 |
| 收稿时间： | 2010/12/3 0:00:00 |
CHARACTERISTICS OF TANCHENG-LUJIANG FAULT AND ITS ROLE ON BASIN CONTROLLING |
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| LIN Zong-man.CHARACTERISTICS OF TANCHENG-LUJIANG FAULT AND ITS ROLE ON BASIN CONTROLLING[J].Journal of Geomechanics,2011,17(4):322-337. |
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| Authors: | LIN Zong-man |
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| Institution: | Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China |
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| Abstract: | Tancheng-Lujiang Fault is a large scale fault belt in the east of China which has a long history of study and many achievements have been obtained.Based on the studies of predecessors,this paper advanced some new opinions as such: large scale strike-slip displacement of the fault may not exit;it formed in late stage of Early Cretaceous;it played a remarkable role on basin controlling. |
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| Keywords: | Tancheng-Lujiang Fault sinistral strike-slip compress-shearing basin controlling |
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