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1)  Dead Sea basin
死海盆地
2)  the East China Sea Basin
东海盆地
1.
By means of inclusion thermometry and authigenic illite dating data,the oil and gas migration and accumulation model in the central anticlinal zone in the Xihu Sag of the East China Sea Basin has been studied.
利用包裹体测温和成岩矿物伊利石测年数据资料,对东海盆地西湖凹陷中央背斜带油气运移及成藏的基本模式进行了研究。
2.
A detailed sequence stratigraphy of Tertiary in the East China Sea Basin has been researched based on the previous work by way of sedimentology, biostratigraphy, log stratigraphy and seismic stratigraphy in this paper.
在前人研究成果基础上,运用沉积学、生物地层学、测井地层学及地震地层学,对东海盆地第三系进行了较系统的层序地层学研究,结果表明东海盆地第三系可划分为5个二级层序(层序组)和12个三级层序以及若干次一级层序。
3)  South China Sea Basin
南海盆地
1.
Constrains and growing trend of biological reef in South China Sea Basin;
南海盆地生物礁形成条件及发育趋势
2.
The magnetic anomalies of the South China Sea Basin indicate that its oce.
南海盆地磁异常显示其洋壳是新老不一、厚薄不匀的新洋壳的拼合叠覆体。
4)  East China Sea basin
东海盆地
1.
Carbonate cements and their formation mechanism in Palaeogene sandstones of Lishui sag,East China Sea basin;
东海盆地丽水凹陷古近系储层砂岩中碳酸盐胶结物及形成机制
2.
Accumulation and distribution of natural gases in Xihu Sag, East China Sea Basin;
东海盆地西湖凹陷天然气成藏及分布规律
3.
Formation of the LS36-1 oil and gas structure in the Lishui Sag, East China Sea Basin;
东海盆地丽水凹陷LS36-1构造成藏机理研究
5)  Marine basin
海相盆地
6)  Bohai basin
渤海盆地
1.
Geochemical investigation for oil and gas in middle sag of Bohai Basin;
渤海盆地中部凹陷油气地球化学勘查
2.
Choosing one well separately in eight main sags of the Bohai basin and analysing the subsidence history of each well, we come to a conclusion that the subsidence characteristics of different sags were different.
在渤海盆地8个主要凹陷各选取一口井,对每口井构造沉降史特征进行分析,结果表明渤海盆地的构造沉降特征各凹陷不统一,南部和北部先沉降,再逐渐向中部迁移,最后以中部沉降为主,沉降中心明显由周缘向盆地中心迁移,反映构造活动的阶段性和地区差异性。
3.
On the basis of the data obtained from the GPS networks in the Bohai basin and its adjacent areas in the past decade,the present-day tectonic movement,internal deformation and strain field in this region are analyzed.
根据近十多年来渤海盆地周围地区GPS网的观测资料,分析了这一地区的现今构造运动、内部形变与应变场。
补充资料:海盆
深度在3,000—6,000米之间的海底盆地,除海岭和海沟外,底部平缓。海盆面积占海洋总面积的70%以上。
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