CHARACTERISTICS OF TANCHENG-LUJIANG FAULT AND ITS ROLE ON BASIN CONTROLLING
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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。
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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Key words:
- Tancheng-Lujiang Fault /
- sinistral strike-slip /
- compress-shearing /
- basin controlling
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