1) Northern of West Depression,Liaohe Basin
辽河盆地的凹北段
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) 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
4) 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。
5) Xialiaohe basin
下辽河盆地
1.
evolution of stress field in Xialiaohe basin is divided into six stages firstly .
通过对下辽河盆地及邻区的构造形迹特征和应力场资料的研究，阐明了这一地区自侏罗纪以来区域地应力场演化特征，首次将其应力场演化划分为６个期次，并初步探讨了应力场的变化对油气聚集的影响。
6) northern Songliao Basin
松辽盆地北部
1.
Formation mechanism and main controlling factors for lithologic reservoirs in northern Songliao basin;
松辽盆地北部岩性油藏形成机制及主控因素
2.
Characteristics of the Cretaceous supersequences in northern Songliao Basin;
松辽盆地北部白垩纪超层序特征
3.
Characteristics of Sedimentary Facies and Sequence Boundary in Upper Cretaceous Qingshankou-Yaojia Formation of Northern Songliao Basin;
松辽盆地北部上白垩统青山口—姚家组沉积相及层序地层界面特征
补充资料：凹模壁厚及凹模垫板尺寸
型腔壁部投影面积 壁 厚， 毫 米
F， 厘米2 h1 h2 h3 h4 h5
<5 15~20 30~40 <=10 15~20 30~40
>5~10 20~25 40~50 10~15 20~25 40~55
>10~50 20~30 50~60 15~20 20~30 55~65
>50~100 30~35 60~75 20~25 30~40 65~70
>100~200 35~40 75~85 25~30 40~50 70~75
>200 >40 >85 30~35 50~60 >80
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