海洋地质与第四纪地质2012，Vol.32Issue(3)：55-62,8.DOI:10.3724/SP.J.1140.2012.03055
北黄海盆地西部坳陷地质构造特征及演化
STRUCTURAL FEATURES AND EVOLUTIONARY STAGES OF THE WESTERN DEPRESSION OF THE NORTH YELLOW SEA BASIN
摘要
Abstract
The North Yellow Sea Basin is located in the southeastern part of the North China Platform. It is bounded by the Liaodong uplift to the north, and the northern Korean block to the east. The Basin is subdivided into six distinguished sub-grade tectonic units. The western depression, lying in the west part of the basin, is a sub-unit with complicated structural features. There are five main faults and some subordinate faults, including extensional, transpressional and reverse faults, dominated by the normal, as the results of the multiple stages of tectonic evolution of the North Yellow Sea Basin from Mesozoic to Cenozoic, which consists of the stages of Mesozoic rift-depression, Paleocene superimposed rifting and Neocene depression.关键词
断层/构造样式/构造演化/西部坳陷/北黄海盆地Key words
western depression/ faulting/ structural styles/ tectonic evolution/ North Yellow Sea Basin分类
海洋科学引用本文复制引用
王立飞,郭丽华,聂鑫..北黄海盆地西部坳陷地质构造特征及演化[J].海洋地质与第四纪地质,2012,32(3):55-62,8.基金项目
国家“海洋地质保障工程”专项重点科研项目(GZH20110205) （GZH20110205）
