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1)  Eastern uplift of Liaohe basin
辽河盆地东部凸起
2)  Eastern Depression of the Liaohe Basin
辽河盆地东部凹陷
1.
Based on heat flow measurements and vitrinite reflectance ( R o) data, the geothermal history of Eastern Depression of the Liaohe Basin was reconstructed, which indicated that the Eastern Depression was characterized by lower present day heat flow varying between 47~70 mW/m 2, and that the depression experienced a much higher heat flow (66~82 mW/m 2) period from 43 Ma to about 25 Ma ago.
根据辽河盆地东部凹陷大地热流测量和镜质体反射率数据 ,恢复了该区的热历史 ,结果表明 :东部凹陷热流呈现古热流高现今热流低的变化特征 ,沙河街组三段沉积期到东营组沉积期 (距今 43~ 2 5Ma)盆地热流为 66~ 82mW m2 ,现今热流值为 47~ 70mW m2 。
3)  Liaodongwan-Xialiaohe basin
辽东湾-下辽河盆地
1.
Liaodongwan-Xialiaohe basin is a Cenozoic plate interior rifting basin.
辽东湾-下辽河盆地是一个富含油气的新生代裂陷盆地。
4)  The East Rise of Liaodong Bay Depression
辽东湾坳陷东部凸起
1.
The East Rise of Liaodong Bay Depression might come into be.
本文应用大量地震测线的构造几何学特征分析,结合构造物理模拟试验,认为辽东湾坳陷东部凸起是在先期存在的低凸起的基础上,在渐新世东营组沉积期因营口—潍坊断裂带的右行走滑形成的。
5)  Liaohe Basin
辽河盆地
1.
Characters of coal classification and coal rank distribution in third member of Shahejie Formation in eastern depression of Liaohe basin;
辽河盆地东部凹陷沙三段煤种和煤级分布特征
2.
Lithologic identification and reservoir division of Xing-Ma Archean group buried hill in Liaohe basin;
辽河盆地兴马太古界潜山的岩性识别与储层划分
3.
Research on hydrocarbon abundance conditions in nearshore sublacustrine fan in Western sag of Liaohe Basin——take Rehetai Formation in Xing-Bei area as an example;
辽河盆地西部凹陷近岸湖底扇油气富集条件研究—以兴北地区热河台油层为例
6)  the Liaohe Basin
辽河盆地
1.
Oil-oil meticulous correlation research shows that there exist both immature and mature oils in Oulituozi area of the Liaohe Basin,and the maturity level of these oils is generally lower than those in the other areas of the East Sag.
油—油精细对比揭示辽河盆地欧利坨子地区低熟油和成熟油共存,与东部凹陷其它地区原油相比总体上成熟度较低。
2.
According to analysis of formation water and crude oil at the west Jinganpu of Damintun Sag in the Liaohe Basin,type NaHCO_3 formation water on the top of the burial hills in the studied area is dominative,type CaCl_2 appear in local area.
对辽河盆地大民屯凹陷静安堡西侧低潜山带地层水化学性质特征分析表明,潜山顶部地层水是以NaHCO3水型为主,局部出现CaCl2水型,反映了潜山顶部总体上具有一定的自由交替水动力条件的开放性环境,而局部出现封闭性环境;这种局部性的封闭环境主要是由于封堵性断层及上覆欠压实泥岩的封堵造成的。
补充资料:帘线凸起
分子式:
CAS号:

性质:又称胎里凹凸,帘线凸起,胎里沟痕等。指胎里表面局部高低不平的现象。  胎里帘线起褶  wrinkled cords in tyre cavity  又称胎里帘线叠褶,帘线褶棱,胎里出褶等。指胎里帘线局部起褶棱的现象。

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