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fault block相关的网络例句

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与 fault block 相关的网络例句 [注:此内容来源于网络,仅供参考]

Fault block of east Shan 6 in Shanjiasi oilfield is a typical super heavy oil reservoir.

单家寺油田单 6东断块是典型的超稠油油藏。

A well was drilled in G388-2 fault block as an application of this technique in Tangjiahe Oilfield and greater amount of oil has been obtained.

然而,大多数情况下用钻井资料编制的是局部构造图,其精度受钡J井小层对比精度的影响,必须在全工区范围

And the later improvement and development direction are pointed out, which will lay a firm foundation for making further improvement on the exploitation effects of Tuo 7 fault block.

并指明了下步改进及发展方向,为进一步提高坨七断块的开发效果奠定坚实基础。

Tracer test data of 76-30 well group of the Guan-104 fault block in Dagang oil field have been analyzed by this model.

以大港油田官104断块76-30井组的示踪剂测试为例进行了分析,由示踪剂产出曲线拟合得到了该井组目前的剩余油饱和度分布。

The G142 fault block was classified 13 minilayers and 4 kinds of flow unit based on the flow unit classification.

基于流动单元划分,将官142 断块划分出13个小层,分为4 类流动单元。

Because the BaMianTai oil field was a fault block hydrocarbon reservoir and the stable yields of the reservoir is a bottleneck problem, the thesis did a lot of works on the meticulous description research, and the fine ...depositional time comparison; the flat distribution graphs and the reservoir sand graphs of depositional microfacies in different time were drafted; the researches on 3D seismics microtectonics and little faults'fine explanation and reservoir types of main layers were completed in the thesis.

本文针对八面台油田是一个复杂的断块油藏的特点和制约油田稳产的瓶颈问题,开展了精细油藏描述研究工作,进行了沉积时间单元精细划分对比;编制了不同时间单元的沉积微相平面分布图、油砂体图;完成了主力油层顶面三维地震的微构造、小断层精细解释以及油藏类型的研究。

It is featured by fractural faults,severe multiple and igneous rocks,thus the technology of fine structural interpretation plays key role in progressive development of little fault block oilfield.

素有&地质家考场&的江苏油田地下情况复杂,断层破碎,火成岩发育,多次波严重,因此,构造精细解释在复杂小断块的滚动开发中起着至关重要重要的作用。

The geological and geophysical data show that in the lower crust of young continental tectonic units may occur pervasive, non-seismic, subhorizontal and ductile flow related to thermal softening. The laminar flow drives fault-block movement of the upper crust, results in the formation of orogenic belts and sedimentary basins, and causes coupling between ductile lower crust and brittle upper crust/mantle.

大量的地质和地球物理资料表明,年轻的大陆构造活动区的下地壳可能因热软化而出现透入性非地震式顺层韧性流动,这种下地壳层流作用驱动大陆上地壳发生地震式脆性断块运动,形成盆山格局,发生圈层耦合。

After crystallization basement was formed in Tai Shan group in the end of Archaean, it suffered long term denudation and deposited to marine and land interbedded formation with stable lithology and thickness. Buried Hill is a large size fold nappe which was uplifted, compressed, folded, denudated and settled in Indosinian period, deposited in Mesozoic formation, then wholly advanced to the west in the late of Yan Shan movement. The force acting on internal structure of buried hill was complicated, and fault block was broken up.

本文通过物探、测井二次解释和钻井等大量资料的研究认为:桩西古潜山在太古代末期泰山群形成结晶基底后,遭受长期剥蚀,在古生代沉积一套岩性、厚度稳定的海陆交互相地层,是一个经印支期抬升、挤压、褶皱、剥蚀、沉降接受中生界地层沉积之后,在燕山运动后期,整体向西推移的大型褶皱推覆体。

Lithologies are mostly sand and carbonate rocks, caps are mud rock, shale and magmatite. Entrap types are anticline, fault block rebuilt by breaking and the screened entrap diapered rock mass. The composition is CO_2, N_2, CH_4, C_2H_6 and He etc. It is magma air source body and its geologic fashions are intrusion and buried volcanic conduit. The relations between gas reservoirs and gas source bodies have three types: magma intrusion-breaking-communicated gas reservoir, magma intrusion-contacted CO_2 reservoir and buried volcanic conduit-contacted gas reservoir. The CO_2 migration in magma intrusion is consisted of fusing and crystallizing phases;it in volcanic conduit is consisted of near-surface effusion and crystallizing phases.The buoyancy of CO_2 in water far more than migration resistance in breaking or chink, CO_2 is easy float upward, the floating can results in differentiation of different density gases and concentration of sealed gas. The gas in sand reservoir firstly migrate into the higher porosity and coefficient of permeability sand, and along with the pressure going up it migrate into the lower. In magma intrusion-breaking-reservoir migration, CO_2 firstly migrate into watered breaking, began gravity differentiation and concentrate, the gas pressure time and again go up, CO_2 migrate into reservoir and concentrate under expansibility as the pressure reach upward a given extend. The CO_2 in reservoir experience four breaking modes: chemistry deposition, dissolution, diffusion and mechanic breaking, the pressure balance can be broken by faulting and the CO_2 will further migrate and form new reservoir.

济阳坳陷已发现的八里泊、阳25、平方王、平南、高青、花17 CO_2气藏主要储集层位有奥陶系、中生界、沙四段、沙三段、沙一段、馆陶组和明化镇组,储集层岩性以砂岩和碳酸盐岩为主,盖层以泥质岩、页岩和岩浆岩为主。;圈闭类型主要为受断裂改造的背斜、断块及刺穿岩体遮挡圈闭。;气体成分主要有CO_2、N_2、CH_4、C_2H_6、He等。;主要气源体为岩浆气源体,气源体的主要地质形式为侵入体和埋藏的火山通道。;气藏和气源体的空间关系有岩浆侵入体一断裂一气藏沟通型、岩浆侵入体-CO_2气储集层接触型和埋藏火山通道-气储集层接触型三种类型。;岩浆侵入体CO_2气运移分为熔融运移阶段和结晶运移阶段,火山通道中CO_2气运移分成近地表喷发阶段和结晶运移阶段。;断裂中,CO_2在水中的浮力远大于运移阻力,CO_2气容易上浮,CO_2在断裂中的易浮性导致不同密度气体的分异和走向上封闭的断裂气体相对富集。;气体在砂岩储集层运移聚集具有选择性,会优先进入孔隙度和渗透率较高的砂岩,随着压力增加,才会进入孔隙度和渗透率较低的砂岩;在岩浆气源体-断裂-储集层空间输导格架下,CO_2气在膨胀力的驱动下,首先进入含水的断裂并重力分异而聚集,气体压力会不断增高,当压力增至一定程度,CO_2气会向高孔隙度、渗透率的储集层运移并聚集。;在岩浆气源体-储集层接触空间输导格架下,CO_2气受膨胀力的驱动直接向储集层运移并聚集。;成藏的CO_2气会经历化学沉淀、溶解、扩散和机械破坏四种破坏方式,会受断裂切割而打破压力平衡,沿断裂进一步运移和聚集成藏。

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呼气,收缩臀部肌肉;拱起身体,尽量抬起头来,右腿伸直朝向天花板(膝微屈,以避免肌肉紧张)。

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