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impounding water reservoir相关的网络例句

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As is low porosity and low permeability gas reservoir in Daniudi Gasfield and the influence of the drilling and geologic conditions on it, the total hydrocarbon values in wellsite gas logging could not accurately reflect reservoir gas bearing properties, and the interpretation and evaluation accuracy was decreased.

大牛地气田为低孔、低渗油气藏,由于钻井与地质条件等因素的影响,现场录井随钻全烃值不能准确反映储集层的含气性,降低了解释评价的准确性。

Through fully digested available information and predecessor's cognition, using whisht and dynamic data acquisitied from each stage, making a refined known and interpretation for single reservoir sand, construct, collector, sediment etc in the oilfield. By dint of numerical reservoir simulation and producting history fitting for verification and adjustion.

通过现代沉积类比,在对取心井、大量电测资料和沉积微相研究的基础上,认为五2西克下组属于扇三角洲沉积体系,纵、横向上相变快,造成储层非均质性强。S_7~(42)为扇三角洲上分流平原亚相沉积;S_7~(41)为扇三角洲下分流平原亚相沉积;S_7~3扇三角洲内前缘亚相沉积;S_7~2、S_7~1均为扇三角洲外前缘亚相沉积。

In view of multi-types, complicated structure, and strong aeolotropism of reservoir of buried hill, we use kinds of forecasting techniques for reservoir together to solve these problems in our research.

针对潜山储层储集空间类型多、结构复杂,非均质性极强的这种特性,本次研究采用了多种储层预测技术联合攻关的方法。

Ta' He oil field is situated in desert of the Tarimensis basin, because it is impact by multiphase play and aeolotropism of reservoir development, the reservoir category, genesis and distribution law is very complicatedly.

塔河油田位于塔里木盆地北部的戈壁沙漠中,受多期成藏及储集层发育非均质性的影响,使塔河油田奥陶系油藏类型、油藏分布规律、油藏的成因都极其复杂。

This study takes the reservoir of the Kela 2 gas field of the Tariam basin, the western China, as an example for understanding the relationship between the porosity and permeability and autogenetic minerals and textures of the clastic rocks on the vertical depth scale. The secondary pores are essential reservoir space in this gas field, moreover, their origin is closely related to dissolution of the frame grain of plagioclase and the cements of calcite.

本文以克拉2气田储层为研究对象,探讨了该区纵向深度上孔隙度、渗透率与矿物组合、结构上的变化,发现次生孔隙是本区储层的重要储集空间,并且与长石骨架颗粒和方解石胶结物的溶蚀密切相关。

In order to know physical properties of Eogene reservoir origin type in Gudong area clearly,the physical properties of the main reservoir origin types were studied in detail including sandbodies of braided-river delta, meandering-river delta, shallow lake and bathyal lake.

为详细了解孤东地区古近系储层成因类型的物性特征,分别对其主要的储层成因类型———辫状河三角洲砂体、曲流河三角洲砂体、浅湖砂体和半深湖砂体的物性做了详细研究。

In order to know physical properties of Eogene reservoir origin type in Gudong area clearly,the physical properties of the main reservoir origin type s were studied in detail including sandbodies of braided-river delta, meandering-river delta, shallow lake and bathyal lake.

为详细了解孤东地区古近系储层成因类型的物性特征,分别对其主要的储层成因类型———辫状河三角洲砂体、曲流河三角洲砂体、浅湖砂体和半深湖砂体的物性做了详细研究。

But for complex type reservoir or lesser wells in the work area,reservoir changes between wells exist biggish indetermination.

但对于复杂类型储层或井点较少的工区,井间储层变化存在较大的不确定性。

By means of core observation and log analysis of reservoir, it is recognized that widely distributed Tazhong uplift is formed from the late of Middle Ordovician to the early of Late Ordovician (from Llandeilo in Early Caradoc). The buried hill paleo-karst reservoir developed in the carbonate rocks of the mid-upper section of Yingshan formation of Lower Ordovician and covered by Lianglitag formation of Upper Ordovician is dominated by lithology of granular limestone, micritic limestone and algal elastic limestone interlayered with dolomite of open to semi-restricted platform fades.

通过岩心观察、测井储集层分析等手段,识别出塔中凸起区广泛分布形成于中奥陶世晚期-晚奥陶世早期(兰代洛世-卡拉道克世早期)、发育于下奥陶统鹰山组中上部碳酸盐岩中且被上奥陶统良里塔格组覆盖的古潜山岩溶储集层,其原岩主要为开阔-半局限台地相颗粒灰岩、泥晶灰岩、藻灰岩夹白云岩。

The chief controlling factors to available reservoir are paleo-karst morphology in Llandeilo to Early Caradoc and multi-stage faulting and karstificatio. Its evolution of reservoir chiefly suffered the reconstruction of diagenesis such as epidiagenetic karstifiration uncovered for over 10 Ma in Llandeilo to Early Caradoc and 3-stage burial karstification since Late Ordovician to Devonian, Permian to Triassic and Tertiary.

有效储集层主控因素是兰代洛世-卡拉道克世早期的岩溶古地貌及多期断裂岩溶作用,其储集空间演化主要经历了兰代洛世-卡拉道克世早期长达10×10^6a以上的暴露淡水岩溶及3期(晚奥陶世-泥盆纪、二叠纪-三叠纪、古近-新近纪以来)埋藏岩溶等建设性成岩作用的改造。

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