曾母盆地

曾母盆地位于南海西南海域，是一个总面积约17×104km2的新生代含油气盆地。

Zengmu Basin , situated in the southwestern South China Sea , is a Cenozoic oil / gas-bearing basin with total area of 17 × 10 ~ ( 4 ) km ~ ( 2 ) .

曾母盆地西部构造样式初步分析

Preliminary analysis of structural styles in the west Zengmu basin

南沙海域曾母盆地的油气勘探开发现状

Progress of gas-oil prospecting at Zengmu basin , Nansha , South China Sea

南海曾母盆地新生代晚期构造沉降分析

Analyses of Late Cenozoic Tectonic Subsidence of Zengmu Basin in South China Sea

南海曾母盆地油气地质条件及其分布特征

Hydrocarbon geological conditions and distribution characteristics of Zengmu basin in southern South China Sea

南沙海域曾母盆地西部油气地质条件初步分析

Petroleum geology of west part of Zengmu basin of Nansha area , South China Seas

南沙海域曾母盆地发育各种类型的构造样式，本文研究与油气聚集和圈闭关系密切的典型构造样式。

There are various structural styles in the Zengmu basin of the Nansha sea area .

南海曾母盆地南部陆架边缘三角洲沉积特征

Analysis of the Shelf-Margin Delta in the south of Zengmu basin , south China Sea

南海曾母盆地地质构造特征及演化历史

Zengmu basin : geologic structure and evolution

曾母盆地西部岩石圈特性与有效弹性厚度：来自构造模拟的约束

Lithospheric characteristics and effective elastic thickness of Western Zengmu basin , South China sea : constraints from tectonic modeling

文章认为，曾母盆地是发育在块体会聚带上的周缘前陆盆地；

The article considered that the Zengmu basin is a peripheral foreland basin developed in block of convergent belt ;

南海西南部曾母盆地早中新世以来沉降史分析

Analysis of the subsidence history of the Zengmu basin in the southwest South China Sea since the early Miocene

廷贾断裂的掀斜作用使曾母盆地和文莱盆地沉积了巨厚的新生代沉积物。

It is due to the development of Tingjia fault that the thick Cenozoic sediments might be deposited in basins of Zengmu and Wenlai .

曾母盆地是南沙块体向南俯冲与婆罗洲块体发生软碰撞而形成的一个周缘前陆盆地，经历了四个不同的构造演化阶段。

Zengmu Basin is a peripheral foreland basin , formed from southern subduction of Nansha Block and gentle collision with Borneo Block , and experienced four stages of tectonic evolution .

南沙地块与加里曼丹-西南巴拉望地块发生碰撞后，在其东南边缘由于岩石圈弯曲而产生了曾母盆地和文莱-沙巴盆地。

After the collision of the Nansha block and the Kalimantan-Southwest Palawan block , the Zengmu basin and the Brunei-Sabah basin were produced as the winding of the lithosphere of the southeast margin .

南部的曾母盆地是一个显著的高地热异常区，它起因于年轻的构造拉张，其地幔热流高达中央海盆洋壳的地幔热流值。

Zengmu basin and Sunda shelf on the south part are apparently thermal anomalous units , whose mantle heat flow values reach that of the central basin of SCS , which probably results from the young tectonic extension in this region .