平地泉 meaning in Chinese
land spring
pingdiquan
Examples
- The study of diagenesis and its stages let us think that the pingdiquan formation belongs to period " a " of early diagenesis
成岩作用及阶段研究认为二叠系平地泉组属早成岩“ a ”期。 - 3 ) the pingdiquan formation mainly are the deposition of lake and fan - delta , fan - delta developing in the background of the lake facies sedimentary
平地泉组以湖，扇三角洲相沉积为主，扇三角洲的生长是在湖相的背景下进行的。 - Applicating all kinds of new theories , this research has undergoed die mesningful exploration of the sequence , sedimentary facies , reservoir properties and the evolution of pores of the pingdiquan formation of permian . and the syudying effects can direct our work in fact well
研究应用了各种新理论，对二叠系平地泉组的层序、沉积相，储层和孔隙及其演化进行了有意义的探索，而且有效地指导了勘探工作。 - Directed by the advance theories of sequence stratigraphy , reservoir beds sedimentology , seismic stratigraphy and petro - geology , measured by exactitude seismic procession , analysis of seismic facies , analysis of single well lithfacies and sedimentary facies , study of macro and micro character of reservoir and diagenesis , this paper study comprehensively the stratigraphy sequence , the type and distributiong of sedimentary facies , reservoir properties , the diagenesis and the evolution of pores of the 2nd and 3rd parts of pingdiquan formation of permian in wucaiwan - shishugou region in jungan basin . we can optimum seek favourable target area and apply the study results on oil field production in order to solve the difficult questions . we mainly achieve several views as follows : l ) establish the sedimential sequence framework of permian formation in studying area and delimint the jiangjunmiao formation of middle dyas series as lowstand system tract , the lower of the second part to the third part of pingdiquan formation of middle dyas series as transgressive system tract , the upper of the second part to the first part of pingdiquan formation as highstand system tract
以层序地层学、储层沉积学、地震地层学、石油地质学的先进理论为指导，以地震资料精细目标处理、地震相分析、单井岩相分析、沉积相分析、宏观和微观储层特征分析及成岩作用研究为手段，对准噶尔盆地东部五彩湾? ?石树沟地区二叠系平地泉组二、三段的地层层序、沉积相类型及展布、储层物性特征、成岩作用及孔隙演化进行综合研究，优选出有利勘探区带，并将研究结果应用到生产中，解决生产中的难题，主要取得了以下几点认识：建立了工区内二叠系沉积层序框架，把中二叠统将军庙组地层划为低水位体系域，中二叠统平地泉组二段下部三段地层为水进体系域，二段上部一段地层为高水位体系域。 - 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 . meanwhile , the causes of oil formation are investigated based on datum of reservior geochemistry : viscous crude of permian is the result of biodegradation and low maturity working together , and that lighter hydrocarbon constituent of carboniferous oil is missing . at last , the mode and mechanism of the oil pool formation are analysed in the study area according to the structure phylogeny , sedimentary history , and data of reservior geochemistry
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。