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Characteristics of seismic reflections in central region of the South China Sea and their geological significance

机译:南海中部地区地震反射特征及其地质意义

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摘要

More than 4000 km 48-channel seismic reflection data from the central region of the South China Sea have been interpreted. Five seismic interface have been distinguished, named T_1, T_2, T_4, T_6 and T_g respectively. Meanwhile, five seismic sequences numbered I-V have been divided with the Ages of Quaternary and Pliocene, Later Miocene, Earlier and Middle Miocene, Oligocene and Pre- Oligocene separately. Sequences I-II overlie all parts of the area. In the continental slope and island Slope, Sequences III_V are mainly found in the grabens.
机译:来自南海中部地区的超过4000公里的48道地震反射数据得到了解释。区分了五个地震界面,分别命名为T_1,T_2,T_4,T_6和T_g。同时,编号为I-V的五个地震序列已分别划分为第四纪和上新世,晚中新世,中新世早期和中新世,渐新世和前渐新世。序列I-II覆盖该区域的所有部分。在大陆坡和岛屿坡中,层序III_V主要出现在grab石中。

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