海洋地质前沿2017，Vol.33Issue(4)：43-48,6.DOI:10.16028/j.1009-2722.2017.04007
东海盆地瓯江凹陷构造样式及其形成机制
STRUCTURAL STYLES AND THEIR FORMING MECHANISM OF THE OUJIANG DEPRESSION IN THE EAST CHINA SEA BASIN
摘要
Abstract
Since late Cretaceous,the Oujiang Sag has suffered from multi-stage tectonic movements and basin evolution with changing tectonic stress field,which leads to the formation of complex structural features and various structural styles.Through interpretation of both the new and old seismic data of the whole area,structural styles and their distribution pattern of the area are summarized,and the forming mechanism analyzed in this paper.According to the results,the main structural styles in the study area can be divided into three kinds,namely,extensional,compressive and composite styles.The extensional structures,which are developed in the western and eastern parts of the depression,can be further divided into horst-like,graben-like,half-graben-like,shovel-like and Domino-like styles,while the compressive structures,which are developed in the southwest of the depression,are mainly fault-nose structures.The complex structural styles are further divided into volcanic rocks,flower-like tectonics and inverted structures,which are main developed in the south-central part of the depression.关键词
瓯江凹陷/构造样式/分布规律/构造运动Key words
Oujiang Sag/structural style/distribution pattern/tectonic movement分类
天文与地球科学引用本文复制引用
韩宝富,杨长清,刘健,杨传胜,杨艳秋,孙晶..东海盆地瓯江凹陷构造样式及其形成机制[J].海洋地质前沿,2017,33(4):43-48,6.基金项目
国家自然基金(41476053) （41476053）
中国地质调查局项目(DD20160153) （DD20160153）
