1) Dongying Basin
东营盆地
1.
Trace element analysis has been carried out on ostracod shells from the first member of the Shahejie Formation (Oligocene)(SHA 1) in the Dongying Basin, East China.
通过对山东东营盆地早第三纪生油层中介形虫化石壳体进行微量元素分析 ,得出在沙河街组一段中、下亚段沉积时期 ,湖水较浅、盐度高 ,气候干燥 ,古湖泊营养水平低 ;上亚段沉积时期 ,湖水变深、变淡 ,气候凉湿 ,湖水营养化程度增高。
2) Dongying Fault Basin
东营断陷盆地
1.
Effect of formation superpressure system on hydrocarbon migration and accumulation in Dongying Fault Basin;
东营断陷盆地地层流体超压系统与油气运聚成藏
3) Huimin-Dongying Basin
惠民-东营盆地
4) Dongying and Huimin basins
东营、惠民盆地
1.
source rocks, in the Dongying and Huimin basins.
山东东营、惠民盆地的油源断裂,即沟通生油岩与非生油岩的同生断裂发育区,出现了油田水的高含盐度分布带。
5) 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。
6) Jiudong basin
酒东盆地
1.
Through analyses of the biomarker characteristic and its effect on sedimentary setting,water salinity,maturity and parent material,the crude oil from Ying'er sag in Jiudong basin can be classified into the crude from Zhonggou formation in Yingcan-1 Well and the crude from Jiucan-1 Well,Chang-101 Well and Chang-2 Well.
通过原油生物标志物特征及其在追溯沉积环境、水体咸度、成熟度及母源先质等方面的分析,可将酒东盆地营尔凹陷原油分为两类:一类为营参1井中沟组原油;另一类是以酒参1井、长101井和长2井原油为代表的油。
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