摘要
台湾海峡沉积盆地新生代以来构造演化经历了早第三纪陆缘裂谷、晚第三纪挤压收缩和第四纪隆起封闭等发育阶段,属残留陆缘裂谷,具有良好的油气远景,其中,海峡中部油气远景最佳。
Cenozoic tectonic evolution of sedimentary basin .of Taiwan Strait has undergone the stages of continental margin riftings in early Tertiary, compress in Late Tertiary, and uplift- closed in Quaternary. It's a remnant continental margin rift, and has better hydrocarbon potential. In central part of the Strait, hydrocarbon potential is best.
出处
《东海海洋》
1994年第1期31-38,共8页
Donghai Marine Science
基金
福建省科委重点课题
关键词
台湾海峡
油气藏
沉积盆地
演化
Taiwan Strait, basin, hydrocarbon potential, evolution, continental margin