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facies相关的网络例句

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与 facies 相关的网络例句 [注:此内容来源于网络,仅供参考]

At western segment of Altyn Tagh tectonic belt, The eclogites and khondalite series were recognized in Altyn Group (Early Proterozoic?) Which had been thought prviously that it consists of high greenschist facies and lower amphibolitic facies metamorphic rocks. They crop out at the northern slope and southern slope of Altyn Tagh Mountains respectively.

在阿尔金构造带西段,在原认为主要由高绿片岩相—低角闪岩相的阿尔金群中,发现有榴辉岩及麻粒岩相的孔兹岩系,它们分别分布在阿尔金山的北坡和南坡。

The tectonic rocks along the fault zone are composed of cataclastic rocks and mylonites formed in higher, middle and lower temperature. Respectively, both of structural features and rocks have the features of multiple phase's of deformation. The deformation features of main minerals in the high temperature mylonites show that: the quartz has the form of long single crystal and the fabric feature of point maximum near X axis; the feldspar has the form of recrystallization assemblage, They present a high amphibolite-granulite facies with temperature >600℃ and depth >20km. The deformation features of mylonites formed in middle temperature show that: the quartz has the form of polycrystal banding and the fabric feature of point maximum near Y axis and small circle girdle with Y rotational axis; the feldspar has the form of a coremantle structure, They reflect a high greenschist-lower amphibolite facies with temperature from 400℃ to 600℃ and depth from 15km to 20km.

其中,高温糜棱岩主要矿物变形特征组合为:石英为长矩状或长条状单晶、组构为近X轴的点极密,长石为几乎完全重结晶的集合体,形成温度>600℃,相当于高角闪岩—麻粒岩相,形成深度>20km;中温糜棱岩主要矿物变形特征组合为:石英为多晶条带、组构为近Y轴点极密和以Y轴为旋转轴的小圆环带,长石发育核幔结构,形成温度为400~600℃,相当于高绿片岩—低角闪岩相,形成深度为15~20km;低温糜棱岩主要矿物变形特征组合为:石英发育核幔结构、组构特征为近Z轴点极密,长石以碎裂为主,形成温度<400℃,相当于中低绿片岩相,形成深度为8~12km;碎裂岩则主要代表了地表浅层的变形。

By means of analysis on the feature of four types of diagenetic facies, the idea that distribution of diagenetic facies belt playing control action at oil and gas enrichment is proposed, which provides scientific foundation for the further exploration.

对所划分出的4类成岩相特点的分析,提出了成岩相带展布对油气富集具控制作用的观点,为油区进一步勘探提供了科学依据。

The determination of hydrochemical facies type is a tool to control groundwater from pollution any deviation from background water facies can be related to pollution.

水化学类型的确定是研究地下水污染的有效方法,当某一地区的地下水化学含量与环境背景值相差较大时,即可以看作地下水受到了某种程度的污染。

According to the principle of isochronic facies controlled modelling, this paper systematically studied the high-resolution sequence stratigraphy, the microfacies research, the structure modelling, the facies modelling, the parameter modelling, the upscaling, and the flow simulation, and probed the new idea and new flow chart of stochastic modelling in terrestrial reservoirs.

本着等时相控建模的原则,本文开展高分辨率层序地层学-微相研究-构造建模-相建模-参数建模-网格粗化序列研究,探讨陆相储层随机建模的新思路和新流程,并总结密井网区地质规律以指导类似地区的油气开发。

These dilatation veins are the ultramafic—mafic intrusive sheets in early stage, which occurred the strong boudinages and the shearing rotation forming θ、Φ、δtype porphyroclasts generally, as the series different size deformation zones; the features of the leucocratic felsic veins in middle stage; the pink granitoid veins in later stage, show a gneisses evolution process from the deep tectonic facies to the middle tectonic facies.

这些扩张脉体,早期阶段为超镁铁质—镁铁质侵入岩席,受后期构造改造岩席发生强烈石香肠化或受剪切发生旋转,呈θ、Φ、δ碎斑系,总体构成一系列规模不等的变形带;中期阶段以发育淡色长英质脉体为特征;晚期阶段为肉红色花岗质脉体,反映出片麻岩由深构造相向中浅构造相变化的过程。

So the seismic facies analysis method was used to classify the seismic facies of the igneous rock. The result shows that the igneous rock is characterized by slabby, bow, mushroom and moundy in profiles.

在英买力地区,火成岩与碳酸盐岩为共生状态,两种地层的速度十分接近,用常规速度分析方法难以将它们区分。

Based on seismic section explanation of thousands of kilometers, the authors selected 4 seismic parameters (frequency, swing, continuity and inner reflect configuration), adopted multiple nomenclative principle of seismic facies of "figure+configuration+swing+frequency+continuity" and generalized 10 seismic and 5 sedimentary facies for the northern sag of South Yellow Sea Basin.

在数千公里地震剖面解释基础上,选用频率、振幅、连续性及内部反射结构等4个地震参数,采用&构形+结构+振幅+频率+连续性&的地震相复合命名原则,总结出南黄海盆地北部坳陷白垩系近10种地震相单元,5种沈积相类型。

The zircon mineralogy and chronology of the eclogite show that a lot of primary inclusions of omphacite,phengite,garnet,bariosite etc.occur in the zircons,so the zircon should be formed during eclogite facies metamorphism.SHRIMP dating for zircons suggests the age of eclogite facies metamorphism range from 230 to 243Ma.

锆石矿物学和SHRIMP年代学研究表明,榴辉岩锆石中含有大量的绿辉石、多硅白云母、石榴子石、冻蓝闪石等矿物原生包裹体,锆石为榴辉岩相变质作用过程中从形成的变质锆石,锆石SHRIMP U—Pb年龄在230~243Ma之间,代表榴辉岩相变质作用的时代。

Analysis on mineral characteristics (percent of shingly fragment, maturation index and heavy mineral coefficient of stability) and depositional environment in Mesozoic remanet strata show that provenance located in the north of Yanqi basin, clast were moved from north to south in Mesozoic, and the sedimentary environment in northern basin were braided stream facies while shallow lacustrine stream facies in southern basin.

通过对焉耆盆地现今残留中生代地层中的岩矿特征(碎屑含砾百分比、成熟度指数和重矿物稳定系数)及沉积环境分析,焉耆盆地中生代物源区位于盆地北部,碎屑由北至南搬运;盆地北部为辫状河相沉积环境,南部为浅湖相沉积环境。

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