1) the east of Manjiaer region
满东地区
1.
Based on analyses of accumulation material basement,event and mode in the east of Manjiaer region of the Tarim Basin,it has been found out that,besides kerogen source rocks rich in carbonate from Cambrian to Middle-Lower Ordovician,there also exist regenerated hydrocarbon source rocks represented by ancient reservoirs.
塔里木盆地满东地区的成藏物质基础、成藏事件和成藏模式分析表明,该地区除发育寒武系—中下奥陶统高有机质丰度的干酪根型烃源岩外,还发育以古油藏形式为主的"再生烃源",油气藏的形成可分为3个发展阶段:1)中加里东期的古隆起发育、古油气藏形成阶段;2)晚加里东期—印支期的古隆起隆升剥蚀、古油藏破坏并调整阶段;3)晚燕山期—喜山期的上构造层褶皱断裂发育、圈闭形成、以古油藏裂解气充注为主的阶段。
2) the eastern part of Jilin province
东满地区
1.
From 1930 to 1935,the revolutionary struggles were influenced by the first "Left" route, carried out the second "Left" route and the third "Left" route, they make destruction to the Party and the power severely in the eastern part of Jilin province.
从1930年至1935年,东满地区的革命斗争深受党内第一次“左”倾错误路线的影响,贯彻执行党内第二次、第三次“左”倾错误路线,使东满地区各级党组织遭到了严重的破坏,革命力量受到了严重的损失。
3) Manxi area
满西地区
1.
Sedimentary sequence analysis and reservoir evaluation of the Donghe Sandstone of Carboniferous in Manxi area of Tarim Basin;
塔里木盆地满西地区石炭系东河砂岩沉积层序分析与储集层评价
2.
By use of new theory, views and methods of modern Sedimentology and through the analasis of core, well logging and log data of approximately twenty well in Manxi area, six kinds of sedimentary facies such as wave-dominated littoral, tide-dominated littoral,.
本文以层序地层学理论为指导，综合测井、录井资料，将塔里木盆地满西地区石炭系划分为六个层序，并描述了各层序及体系域的特征。
4) West Manjiaer region
满西地区
1.
According to the principle and method of sequence stratigraphy, this paper systematically analyzes the core, well logging and seismic data of Carboniferous of West Manjiaer region in Tarim Basin, the Carboniferous could be divided into seven sequence boundaries, including three sequence boundaries of type Ⅰ and four sequence boundaries of type Ⅱ.
利用层序地层学的原理和方法,综合利用塔里木盆地满西地区石炭系的岩心、测井和地震资料,在研究区石炭系识别出了7个层序边界界面,包括3个Ⅰ型层序边界及4个Ⅱ型层序边界。
5) Madongdong area
马东东地区
1.
Deposition environment, diagenesis and abnormal high pressure are the main factors to control petrophysical properties of deep reservoir in Madongdong area.
马东东地区深部储层物性影响因素分析结果表明 ,沉积环境、成岩作用和异常超压的形成与分布是影响本区深部储层物性的主要因素。
6) East Liaodong area
辽东东地区
1.
A 2-D experiment model was used for modeling oil migration and accumulation in the East Liaodong area.
采用二维物理模型对辽东东地区石油运移和聚集进行了实验研究,结果证实:①断层带的石油运移方式对石油运移路径产生了重要的影响;②3套不整合面在不同充注方式下对石油的输导作用不同,馆陶组下段和东营组之间的不整合面(不整合面1)在2种充注方式下对石油都起到输导作用,东营组与沙河街组之间的不整合面(不整合面2)和沙河街组沙二段与沙河街组沙四段之间的不整合面(不整合面3)仅在幕式充注情况下对石油的运移起到侧向输导作用;③东营组砂体最终能否成藏,取决于砂体与其他输导体的匹配关系,其中与油源断层相沟通且尖灭的砂体最有利于形成岩性油藏。
补充资料：太平洋地区标准会议标准(见太平洋地区标准会议)
太平洋地区标准会议标准(见太平洋地区标准会议)
standards of PASC: see Pacific Area Standards Congress; PASC
Ta iPingyang Diqu Bioozhun Hu呼ib沁幻Zhun太平洋地区标准会议标准(s切md田心sofR巧C)见太平洋地区标准会议。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条