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1)  H_2 oil group of Pingdiquan formation
平地泉组H_2油组
2)  Pingdiquan Formation
平地泉组
1.
Based on the observation and study of a large number of cores and thin sections by cathodoluminescence and SEM, this paper expounds in detail the mechanism of the main diagenesis and its action mode and analyzes the diagenesis sequences and porosity evolution of the Permian Pingdiquan Formation in WucaiwanShishugou region of the eastern Junggar Basin.
通过对岩心、薄片、铸体薄片、扫描电镜等多种资料的综合研究,详细阐述了准噶尔盆地东部五彩湾-石树沟地区二叠系平地泉组储层主要成岩作用的形成机理和作用方式,分析了成岩序次和孔隙演化。
2.
Associated with the study of lighter hydrocarbon constituent, carbon isotope, biomarker and inclusions, adopted the technique of oil source correlation on whole oil samples, it can be confirmed that the hydrocarbon source of viscous crude in Permian, in the east slope of Jimusaer depression, is Pingdiquan Formation mudstone; Carboniferous oil comes from Carboniferous source rock.
本论文根据轻烃、碳同位素、生物标志化合物等资料,运用全烃地球化学油源对比方法进行油源对比,得出吉木萨尔凹陷东斜坡区二叠系的稠油来自平地泉组泥岩,石炭系的稀油来自石炭系本身源岩;同时,根据地化资料研究了原油的成因,认为二叠系稠油是生物降解和成熟度较低共同作用的结果,石炭系的稀油存在轻组分散失现象;最后,综合构造、沉积、烃源岩和油藏地球化学资料,分析了吉木萨尔凹陷原油的成藏机制和模式。
3)  histamine H_2
组胺H_2
4)  Quantou Formation
泉头组地层
1.
Research on Ultra-low Permeability Quantou Formation and Oilfield Development
特低渗透泉头组地层与油田开发研究
5)  H_2/H_∞mixedcontrol
H_2/H_∞组合控制
6)  Baikouquan Formation
百口泉组
1.
The flow units in the alluvial fan reservoir of Baikouquan Formation in Bai-21 wellblock of Baikouquan Oilfield,Zhungeer Basin are divided into 4 kinds of E,G,F and P based on core and well-logging data.
以准噶尔盆地百口泉油田百21井区百口泉组冲积扇相储层为例,利用岩心、测井资料开展流动单元研究,在储层细分对比的基础上,采用定性与定量相结合的方法将研究区流动单元分为E,G,F,P等4种类型。
2.
The Baikouquan formation (T1b) of Triassic in Wuerhe oilfield can be divided into one long-stage semi-cycle (LSC), three mid-stage cycles (MSC) and seven short-stage cycles (SSC) which are in correspondence with the sandbody development period, that is, each period sandbody developed in each SSC correspondingly.
将乌尔禾油田下三叠统百口泉组(T1b)划分为1个长期基准面上升半旋回(LSC)、3个中期旋回(MSC)、7个短期旋回(SSC)。
补充资料:平地
1.平坦的地面。 2.平整地面。 3.犹言突然;平白无故。 4.平稳地;稳当地。
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