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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]

The sedimentation is the foundation, affecting the basic pattern of the reservoir,and the sedimentary facies zones beneficial to the formation and evolution of the reservoir includes platform edge bank facies, introplatform point beach facies and acclivity sedimentary facies, etc.; the diagenesis is the key factor, determining the pattern and scope of the final distribution of the reservoir and being of great influence on reservoir structure, and the diagenesis of promoting the formation of storage rooms is mainly the dissolution occurred during hypergene stage and burial stage;and the tectonism is the condition of influencing the connectivity among various reservoir bodies and among the storage rooms within a single reservoir body.

该套储层是在4亿年左右的地质历史中,由沉积、成岩和构造作用相互影响而形成的最终成果:其中沉积作用是基础,影响着储层的基本形态,有利于储层形成与演化的沉积相为台地边缘滩、台内点滩和上斜坡等沉积相带;成岩作用是关键,决定了储层的最终分布形态和范围,对储层结构的影响至关重要,促进储集空间形成的成岩作用主要有表生期和埋藏期的溶解作用;构造作用是条件,影响着各储集体之间以及单一储集体内部储集空间的连通情况。

They are Neogondolella facies, transitional facies, Hindeodus facies and HindeodusIsarcicella facies. Analysis of conodont geochemistry is a better way for studying paleoecology.

依三种生态类型在上述六种沉积相中的分布,划分了四个牙形石相,即:Neogondolella相,过渡相,Hindeodus相和Hindeodus-Isarcicella相。

According to the characters of organic maceral, organic type, biomarker,it can be divided to five types of sedimentary facies: unrest restricted sea graptolite facies, alluvial restricted sea, carbonate mesa algal deposit facies, mud mesa algal deposit facies and deep water shelf algal deposit facies.

根据烃源岩有机显微组分、有机质类型、生物标志物及成烃能力等特征划分出五类沉积有机相,即动荡局限海笔石相、滞流局限海笔石相、碳酸盐台地藻积相、泥质台地藻积相和深水陆棚藻积相。

Based on the special geological traits of the fourth member of the Shahejie Formation of Block Tuo-123 in Dongying Depression, in combination with the sequence identification and comparison of the seismic section, five typical seismic facieses were summarized, including sub-parallel sheeted seismic facies, hummocky onlap fill seismic facies, lens seismic facies, wedge seismic facies and blank seismic facies, and their traits and distribution range were analysed.

针对东营凹陷坨123断块沙四段的具体地质背景,在对地震剖面层序划分和追踪对比的基础上,总结出5种典型的地震相:亚平行席状地震相、丘形上超充填地震相、透镜状地震相、楔形杂乱地震相和空白地震相,并分析了其主要特征及展布范围。

Igneous rocks of Jiyang depression show typical reflecting features on seismic profile. Tabular reflection seismic facies, arc reflection seismic facies and hummocky or mushroom reflection seismic facies are the three main facies.

济阳坳陷火成岩在地震剖面上呈现典型的反射特征,其反射地震相主要有板状反射地震相、弧状反射地震相、丘状或蘑菇状反射地震相等三种。

Riganpeicuo formation developed marine effusive facies, delta facies, carbonate platform facies and shelf facies, which suggest the paleography of South Qiangtang Basin in late Triassic experienced the process of rifting, sea level rising continuously, and then developing carbonate platform and shelf facies.

日干配错组发育有水下火山喷溢相、三角洲相、碳酸盐岩台地和陆棚相,反映盆地由早期的裂陷火山喷发—盆地基底沉降,海平面不断上升形成台地相至陆棚相的古地理面貌。

This study shows that there are 4 kinds of volcanic facies in deep volcanics in north Songliao Basin: eruptive facies, overflow facies, volcanic vent facies and volcanic sedimentary facies. There are 4 volcanic eruption cycles: Huoshiling period, Shahezi period, Yingchengzi period and Quantou period. There are 4 structural evolution stages: north-south accumulation, west-east subduction, uplift mantle and thin crust, alternative open and close. There are 4 kinds of pool-forming patterns:(1) pattern with the migration along the unconformity and fault to the near crater;(2) pattern with the migration along unconformity and fault to the rift margin;(3) pattern with the migration along unconformity, fault and fracture to the source rock;(4) pattern with the migration of the deep gas along the deep and large fault to the volcanic trap.

研究认为,松辽盆地北部深层火山岩主要存在四种火山岩相:即爆发相、溢流相、火山通道相、火山沉积相,划分为四个火山喷发旋回:即火石岭期、沙河子期、营城子期、泉头期,经历了四个构造演化过程:即南北夹攻、东西俯冲、幔隆壳薄、开合交替,具有四种成藏模式:即沿不整合面和断层运移至近火山口处火山岩圈闭聚集成藏模式、沿不整合面和断层砂岩疏导层运移至断陷边部火山岩圈闭聚集成藏模式、沿不整合面及断层、裂缝运移至源岩区内凹中隆火山岩圈闭聚集成藏模式、深部无机成因天然气沿深大断裂运移至火山岩圈闭聚集成藏模式。

The eclogites at western segment of Altyn Tagh tectonic belt occur as lens or boundins within quratz-feldspathic gniesses characterized by amphibolite-facies parageneses. It mainly experienced the prograde amphibolite-facies stage (P=6.06-8.70kb, t=615-690℃),peak eclogite-facies stage (P>15kb,T=700-850℃), granulitic facies stage (P=11-14kb,T=750℃) and ampbiolite-facies stage (P=6.3-9.5kb,T=619-738℃) during decompression.

阿尔金构造带西段的榴辉岩呈透镜状产于长英质片麻岩中,它主要经历了进变质的角闪岩相(P=6.04-8.70Kb,T=615-690℃)、峰期的榴辉岩相(P>15Kb,T=700-850℃)及减压过程中的麻粒岩相(P=11-14Kb,T=750℃)及角闪岩相(P=6.3-9.5,T=619-738℃)的变质作用,构成一个顺时针的PT轨迹。

Namely, with respect to Changxing Formation in the region of interest, the most favorable facies belt is reef-shoal dolomite facies, the more favorable facies belt is restricted platform facies-platform evaporate facies; the most favorable microfacies belt is subordinate organisms and sparry grain dolomite microfacies, the more favorable microfacies belt is non-lamina dolomite mudstone microfacies.

因此长兴组最有利储集相带是礁滩云岩相带,较有利相带是局限台地-台地蒸发岩相带;最有利微相类型是生物粘结云岩微相和亮晶颗粒云岩微相,较有利的微相类型是非纹层纯云泥岩微相。

The coesite-diamond-bearing eclogite distributed in the northern part of the UHPM belt suffered three stages of metamorphism. The first stage is the Ep amphibolite facies metamorphism, which is represented by the paragenesis of phe+Qtz+Cro/Bar Bar+Ep+Ab occurred as inclusions in Grt and Omp; The second stage is the peak metamorphism of eclogite facies with mineral assembledge of Grt+Omp+Coe±Dia±Ky±Zo±Phe+Rt. The P -T condition is 800±50℃,≥28Kb; The third stage is the amphibolite facies retrograded metamorphism from the peak one, which can be divided intothe early amphibolite facies stage with the mineral assembledge of Amp+ Pl+Di+Qtz±Ep+Ilm/Ttn and the late greenschist facies one with the mineral assembledge of Ep+Chl+Bi+Tr+Ab.

分布于超高压变质带北侧的柯石英榴辉岩经历了3个阶段的变质作用:(1)早期绿帘—角闪岩相阶段,以出现在石榴石和绿辉石中的包体矿物多硅白云母、石英、冰蓝闪石或青铝闪石、钠长石等为代表;(2)峰期柯石英榴辉岩相阶段,其矿物组合为Grt+Omp+Ky+Phe±Zo+Coe±Dia+Rt,其变质温度压力为800±50℃,≥28Kb;(3)退化变质作用阶段,早期为角闪岩相,以Amp+Pl+Di±Ep+Qtz+Tit等退变矿物组合为代表;晚期为绿片岩相,以绿帘石、绿泥石、黑云母、透闪石及钠长石等矿物为代表。

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