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地质力学学报:2011,17(4):322-337
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郯城—庐江断裂基本特征及其控盆作用
CHARACTERISTICS OF TANCHENG-LUJIANG FAULT AND ITS ROLE ON BASIN CONTROLLING
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投稿时间:2010-12-03    
中文摘要: 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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林宗满,2011.郯城—庐江断裂基本特征及其控盆作用[J].地质力学学报,17(4):322-337.DOI:
LIN Zong-man,2011.CHARACTERISTICS OF TANCHENG-LUJIANG FAULT AND ITS ROLE ON BASIN CONTROLLING[J].Journal of Geomechanics,17(4):322-337.DOI:

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