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   tectonic compression 在 石油天然气工业 分类中 的翻译结果: 查询用时:0.801秒
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tectonic compression    
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  构造挤压
    (3) the further increase of excess pressure from the tectonic compression since the Kangcun satge(N 1-2k).
    而康村期 (N1 - 2 k)以来的构造挤压则引起流体压力幅度的进一步增高
短句来源
    Since the decrease of load and temperature in the process of uplifting makes unisostatic compaction and other factors tend to stopping, tectonic compression often becomes the most principal genesis of overpressure in uplifted areas.
    由于抬升过程中负载和温度的降低使得不均衡压实作用等因素趋于停止,构造挤压往往是抬升区超压最主要的成因。
短句来源
    It is summed up that cause of abnormal formation pressure include factors of disequilibrium between compaction and expulsion of water in mudstone, tectonic compression, bearing pressure by high fluid potential, vertically hydrodynamic run-through by fault, etc, and their actions are of distinction respectively among different areas.
    研究区异常压力的成因主要有压实与排水不平衡、构造挤压、高流体势承压、断层对水动力的垂向贯通 ,在不同地区 ,这 4个因素所起的作用大小有所差别。
短句来源
    According to analysis on geological characteristics and geostressed environments of these gas pools, and comparative study between the north zone and south zone, and the pools under halite-gypsum regional cap rocks and the pools above the regional cap rocks, the ultimate origin of overpressure was rapid filling and intense compaction, and strong tectonic compression inside closed system.
    通过对他们的地质特征、分布特点和地应力环境分析 ,及与系统南带各油气田和北带第三系盐—膏质区域盖层之上油田对比研究认为 :在第三系盐—膏质区域盖层之下封闭体系中高速充填—强烈压实和剧烈构造挤压是克拉2等气田孔隙流体超压的根本原因 ;
短句来源
    Abnormal high pressure in reservoirs caused by tectonic compression is coincident with the main period of gas accumulation, and the through_salt overthrusts formed after the main period have provided vertical seals. All these have resulted in coexistence of gas and high pressure and its preservation up to now in many traps.
    构造挤压而形成的储层异常高压与天然气的主要成藏期一致 ,以及成藏期后穿盐断裂的垂向封闭 ,使得该地区许多圈闭中的天然气与异常高压共存并保存至今。
短句来源
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  构造挤压
    (3) the further increase of excess pressure from the tectonic compression since the Kangcun satge(N 1-2k).
    而康村期 (N1 - 2 k)以来的构造挤压则引起流体压力幅度的进一步增高
短句来源
    Since the decrease of load and temperature in the process of uplifting makes unisostatic compaction and other factors tend to stopping, tectonic compression often becomes the most principal genesis of overpressure in uplifted areas.
    由于抬升过程中负载和温度的降低使得不均衡压实作用等因素趋于停止,构造挤压往往是抬升区超压最主要的成因。
短句来源
    It is summed up that cause of abnormal formation pressure include factors of disequilibrium between compaction and expulsion of water in mudstone, tectonic compression, bearing pressure by high fluid potential, vertically hydrodynamic run-through by fault, etc, and their actions are of distinction respectively among different areas.
    研究区异常压力的成因主要有压实与排水不平衡、构造挤压、高流体势承压、断层对水动力的垂向贯通 ,在不同地区 ,这 4个因素所起的作用大小有所差别。
短句来源
    According to analysis on geological characteristics and geostressed environments of these gas pools, and comparative study between the north zone and south zone, and the pools under halite-gypsum regional cap rocks and the pools above the regional cap rocks, the ultimate origin of overpressure was rapid filling and intense compaction, and strong tectonic compression inside closed system.
    通过对他们的地质特征、分布特点和地应力环境分析 ,及与系统南带各油气田和北带第三系盐—膏质区域盖层之上油田对比研究认为 :在第三系盐—膏质区域盖层之下封闭体系中高速充填—强烈压实和剧烈构造挤压是克拉2等气田孔隙流体超压的根本原因 ;
短句来源
    Abnormal high pressure in reservoirs caused by tectonic compression is coincident with the main period of gas accumulation, and the through_salt overthrusts formed after the main period have provided vertical seals. All these have resulted in coexistence of gas and high pressure and its preservation up to now in many traps.
    构造挤压而形成的储层异常高压与天然气的主要成藏期一致 ,以及成藏期后穿盐断裂的垂向封闭 ,使得该地区许多圈闭中的天然气与异常高压共存并保存至今。
短句来源
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  tectonic compression
Most seismic events involve thrusting mechanisms that are consistent with the present stress state of E-W-oriented tectonic compression, but are not consistent with the opening of the deepest ore vein.
      
Thus, in general, the slip pattern on faults as a whole agrees with the sense of tectonic compression in this region.
      
But the magnitude of slip resulting from the tectonic compression is much larger than that due to the block rotation.
      
(3) Between the slips caused by regional compression and block rotation, there is a possibility that the sense of slip caused by rigid body rotation in two adjacent blocks is opposite to the slip caused by the tectonic compression.
      
Geophysical applications that can be approximated by undrained conditions (fast loading) include seismicity, tidal and barometric loading, and tectonic compression.
      
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The Cenozoic sedimentary basin of Taiwan Strait is composed of Xiapeng, Wuquyu, Xinzhu ,and Taiwan depressions. By analysis and correlation of seismic stratigraphic characteristics in the west part with Cenozoic strata in the east part of the strait, and combining with fault structures, magma-tism, tectonic characteristics of the basin, etc., it is suggested that the tectonic evolution of the basin has undergone crustal extension (pregnant period)at the end of Mesozoic, first extended rifting(in-fant period)...

The Cenozoic sedimentary basin of Taiwan Strait is composed of Xiapeng, Wuquyu, Xinzhu ,and Taiwan depressions. By analysis and correlation of seismic stratigraphic characteristics in the west part with Cenozoic strata in the east part of the strait, and combining with fault structures, magma-tism, tectonic characteristics of the basin, etc., it is suggested that the tectonic evolution of the basin has undergone crustal extension (pregnant period)at the end of Mesozoic, first extended rifting(in-fant period) in Late Cretaceous-Paleocene, tectonic subsidence (teenage period)in early Eocene, second extended rifting (youth period)in late Eocene-Oligocene, cooling subsidence (adult period) in early-middle Miocene, tectonic compression (old period) in late Miocene-early Pliocene, contrac-tion-uplft (dying period) in late Pliocene-Quaternary. Among the evolution cycles of the basin, pregnant period-youth period is a tectonic continental rifting stage, adult period is a tectonic rejust-ment stage, and old period-dying period is a stage of complete shortened and closed-uplift of Taiwan Depression. Taiwan Depression is a typical example for a continental margin rift from generation to dying.

台湾海峡新生代沉积盆地由厦澎、乌丘屿、新竹和台湾等坳陷组成。通过对海峡西部的地震地层特征和东部的新生代地层的分析和对比,结合沉积盆地的断裂构造、岩浆活动以及大地构造特征,认为该盆地的构造演化经历了中生代末地壳拉伸(孕育期)、晚白垩世—古新世张裂(幼年期)、始新世早期沉降(少年期)、始新世后期—渐新世再次张裂(青年期)、中新世早—中期冷却沉降(壮年期)、晚中新世—上新世早期挤压—收缩(老年期)、上新世后期—第四纪收缩—隆起(消亡期)。其中,孕育期—青年期为陆缘裂谷阶段,壮年期为构造调整阶段,老年期—消亡期为全面收缩及台湾坳陷封闭隆起阶段。台湾坳陷是陆缘裂谷从产生到衰亡的典型实例。

The formation of coal measure-derived oil & ggs fields in NW China is the product of the assemblage in spatial and temporal domains of certain tectonic conditions,sedimentology and the accumulation of oil-prone organic materials as well as the effective expulsion of oil & gas from the coal measures.The study made by this paper shows that the following.conditionsare necessary for the formation of coal measure-derived oil & gas fields in Jurassic sequence of NW China The Jurassic original basin,which was occupied...

The formation of coal measure-derived oil & ggs fields in NW China is the product of the assemblage in spatial and temporal domains of certain tectonic conditions,sedimentology and the accumulation of oil-prone organic materials as well as the effective expulsion of oil & gas from the coal measures.The study made by this paper shows that the following.conditionsare necessary for the formation of coal measure-derived oil & gas fields in Jurassic sequence of NW China The Jurassic original basin,which was occupied by lake water or low-positional swamp during the most Jurassic time,should exist,so that the complete association of source rock,reservoir and caprock was well developed;The original depositional environment was characterized with low and gentle depression and humid climate which are favorable for the development of low-positional marshland and lake where the oil-prone organic materials were accumulated with large volume;The sequent basin should occur on the Jurassic original basin which is necessary to keep the coal measure source rocks in the condition of progressive mat uration,and certain degree of tectonic compression taking place soon after the maturation of source rocks can provide the driving force for the effective expulsion of oil & gas from the coal measures.Coal measure-derived oil & gas fields is horizontally distributed along the inner side of lake strandline depositing with source-rock and vertically occured above or below the thresh old of maturity.Owing to the sharp variation of lithology and facies in coal measures,the lithological and composite types of oil & gas pools play a big role in the petroleum accumula tions of coal measure sequence.

煤系油气田的形成是一定的构造、沉积与生烃母质富集、成熟与油气有效排出等因素在时空间配置组合而形成的产物。西北地区侏罗系煤系油气田形成必不可少的条件是:①侏罗系原盆地应存在,发育有完整的生储盖组合;②原始沉积环境呈低缓洼地,并具备潮湿气候,有利于近湖低位沼泽与大量易生烃母质的发育和堆积;③后续盆地要继承发展,以保持源岩递进性受热并熟化;④源岩成熟后的构造挤压是油气有效排驱的主要动力。煤系油气田在平面上沿着与源岩同期的湖岸线内侧分布,位于有油源断层切割,收缩量适中,破坏较弱的区带。剖面上则集中于生烃门限上下。其中构造-岩性与岩性型油气藏占有重要比例。

WT5BZ]Based on the particularity of stratigraphic structure for the salt mud interbeds of the Wuyang Continental Salt lake Basin,the authors discussed the genetic mechanism of anomalous fluid pressure in the basin starting with its destributive characteristics combined with the burial history and thermal evolutionary history of the basin.The calculated results of pressure reveal that the anomalous fluid pressure in the salt lake basin can be classified into shallow,middle and deep three sets of pressure ...

WT5BZ]Based on the particularity of stratigraphic structure for the salt mud interbeds of the Wuyang Continental Salt lake Basin,the authors discussed the genetic mechanism of anomalous fluid pressure in the basin starting with its destributive characteristics combined with the burial history and thermal evolutionary history of the basin.The calculated results of pressure reveal that the anomalous fluid pressure in the salt lake basin can be classified into shallow,middle and deep three sets of pressure sealing systems,that is the gradational and transitional moderately anomalous high pressure system in shallow beds,the mutiple sets of low degree anomalous high pressure system in middle salt mud interdeveloping members and the abrupt high degree anomalous pressure system in deep beds.The formation of anomalous pressure is mainly related to the undercompaction that the fluid in nonpenetrative beds cannot drain off due to non isostatic compaction result from rapid subsidence.It also has something to do with hydrothermal pressure enhancement,organic matter converting into hydrocarbon,tectonic compression,etc.

本文针对舞阳陆相盐湖盆地盐泥互层的地层结构特殊性 ,从盆地内异常流体压力分布特征出发 ,结合盆地埋藏史和热演化史 ,分析探讨其形成机理。压力计算结果表明盐湖盆地内异常流体压力可分为浅、中、深 3套压力封闭体系 :浅层为渐变过渡中等异常高压体系 ;中间盐泥间互发育段为多套低异常高压体系 ;深部为突变高异常压力体系。异常压力的形成主要与快速沉降造成不均衡压实引起的非渗透性岩层中流体不能排泄出的欠压实作用有关 ,还与水热增压、有机物转化成烃及构造挤压等有关

 
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