• 盆地构造活动火山作用可以促进干酪成烃转化。

    Tectonic activities and volcanism in the basin have an influence on hydrocarbon generation of kerogen and its change.

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  • 分析了鄂尔多斯地块南部渭河盆地构造空间分布特征

    The space distribution characteristics of structures from topography and landform of the south part of Ordos block and Weihe basin are analyzed.

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  • 盆地构造沉降沉积过程主要北缘和西张性断层控制

    Tectonic subsidence and sedimentation were primarily controlled by the northern and western basin border faults.

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  • 前者为陆内-环境产物.后者形成陆缘盆地构造环境。

    The former is formed in trench - arc environment ofintracontinental rift, and the latter in marginal basin.

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  • 由此可见,塔里木盆地构造活动枢纽部位碳酸盐岩聚集油气有利地区

    Therefore the structural pivot positions are the favorable areas for petroleum accumulation in the carbonates in Talimu Basin.

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  • 沉积研究油气勘探质量评价、盆地构造演化基础和有力手段。

    The study of sedimentary research is important to petroleum exploration, analysis of reservoir quality and tectonic evolution.

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  • 应用构造分析理论方法辽河盆地构造断裂,进行系统深入研究

    The paper makes a systemic and thorough studies to the structure fracture in Liaohe Basin by using the theory and method of structure analysis.

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  • 新生代盆地构造沉积分布特征表明渤海湾盆地一个、新生代叠合盆地

    The characteristics of structure and depositment in this Mesozoic and Cenozoic time show that Bohai basin is a Mesozoic and Cenozoic composite basin.

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  • 矿化围岩沉积组合反映形成于较深海盆地环境裂谷盆地构造背景。

    Sedimentation combination of the surrounding rocks suggests that they are formed in deep ocean basin environment, which belongs to rift valley basin.

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  • 讨论总结了盆地构造特征及其发育规律为该区油气勘探提供新的认识依据。

    Also discussed are the basin characteristics and its developing law in this paper, thus giving the new idea to its oil and gas exploration.

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  • 耦合模型可以解释盆地构造盆地沉降山脉隆升岩石圈深部构造特征

    This basin and mountain coupling mechanics model may reasonably interpret the features of the basin structures, basin depression, mountain uplift, lithosphere structure and geothermy in this region.

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  • 沉积剥蚀盆地构造演化控制,生油岩系阶段与过程具有多期次的特征。

    Controlled by the deposition and erosion as well as the basin thermal evolution, the hydrocarbon generation was of multi-phases.

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  • 进行了黄县盆地充填沉积地层划分盆地构造演化阶段分析有机结合起来

    The sequence stratigraphic division of basin filling succession in Huangxian faulted basin is conducted, and combined with the analysis of tectonic evolution stages of basin.

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  • 重点研究吐哈盆地构造单元类型构造属性及其构造反转之间关系相关问题

    This paper focuses on such related aspects as the types and attributes of tectonic units, and the relation between the tectonic units and basin inversion of Turpan-Hami Basin.

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  • 通过深化盆地构造沉积条件认识,揭示了上第三系、下第三系和古潜山成藏模式

    The basin structure, sedimentary and reservoir development conditions were investigated. The Neogene, eogene and Paleozoic models for developing reservoirs were refined.

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  • 黔西北地区一个裂谷盆地构造区,盆地内发育铅锌矿床,矿化受断裂地层的联合控制。

    The northwestern Guizhou Province is located in a rift basin with some lead-zinc deposits controlled by the faults and strata.

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  • 盆地构造演化特征影响,盆地铀矿化存在两种类型潜水氧化带型局部性层间氧化带型。

    Features of tectonic evolution resulted in the development of two type uranium mineralizations in the basin, I e. phreatic oxidation and local interlayer oxidation types.

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  • 以北黄海盆地构造几何学运动学特征基础探讨了黄海盆地构造变形样式动力学演化过程

    Based on the structural geometry and kinematics of North Yellow Sea basin, the tectonic deformation style and geodynamic process of North Yellow Sea basin are studied.

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  • 微量元素稀土元素、同位素方面论证了霍田中元古宙大陆边缘裂谷盆地构造环境。

    The studies of microelement, rare earth element and isotope compositions that the Huogeqi polymetallic ore field was formed in rift basin of back arc continental marging during Proterozoic Era.

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  • 通过鹤岗盆地构造特点分析总结倾角构造复杂区块内提高煤炭资源回收的几点实践经验

    In this paper, the experience of improving coal resources recovery in the fields with high inclination Angle and complex structures are summarized on the analysis of Hegang Basin structural features.

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  • 根据新测构造地质剖面资料,指出运动导致右江盆地构造全面褶皱主张误解

    It is confirmed that the theory of the overall folds of the platform cover and the Youjiang basinal synthem of South China caused by the Indosinian movement is a great misunderstanding.

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  • 控制柴达木盆地构造样式规律性主要因素区域构造环境盆地基底性质应力作用方式岩石力学性质等。

    The basic control factors to the regular evolution of the structural style are geo-tectonic environment, basement nature, stress state, physical nature of rocks and stage of tectonic evolution.

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  • 我国南方地洼盆地构造演化流体演化砂岩铜矿成矿作用三者之间具有密切关系,处于个统一的系统之中。

    There is a close relation among tectonic evolution, fluid evolution and formation of sandstonecopper deposits in diwa basins of South China.

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  • 地层是一切地质问题基础,地层的划分直接影响着对盆地构造演化沉积环境甚至盆地油气远景的认识

    The classification of strata has a great effect on the knowledge about structural evolution, sedimentary environment and even evaluation of hydrocarbon potential in a basin.

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  • 盆地构造演化经历了盆地盆地两个阶段,后者又进一步分为陆内裂谷时期、再生前陆盆地时期和盆地消亡时期。

    It has two tectonic evolutionary stages of foreland basin and intracontinental basin that is further divided into three periods of intracontinental rift, newborn foreland basin and dying out basin.

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  • 黄汉纯显强,王长利。1989。柴达木盆地构造演化石油富集规律地质论评,35 (4):314- 323。

    Huang Hanchun, Zhou Xianqiang and Wang Changli. 1989. Tectonic evolution of the Qaidam Basin and the regularity of oil accumulation. Geological Review, 35 (4) : 314-323.

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  • 塔里木盆地构造应力场油气聚集研究是一个涉及构造物理构造地质石油地质等多学科的具有较强理论与应用价值的问题。

    The study on structural stress field and hydrocarbon accumulation of Tarim basin, which dealing with geophysics, tectonics and petroleum geology is very important in theory and application.

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  • 沉积盆地构造演化模拟建立盆地成因地质地球物理模型基础之上,其中包括运动学模型、运动学—流变学模型和动力学模型。

    Tectono thermal modeling is based on the geological geophysical models of basin formation, which include kinematic model, kinematic rheological model and dynamic model.

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  • 目前法国,有超过2万套的公寓温暖的地下水供暖的,这些地下水来自一个叫做巴黎盆地的地质构造,位于巴黎附近

    More than 20,000 apartments in France are now heated by warm underground water drawn from a heat reservoir in a geologic structure near Paris called the Paris Basin.

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  • 目前法国,有超过2万套的公寓温暖的地下水供暖的,这些地下水来自一个叫做巴黎盆地的地质构造,位于巴黎附近

    More than 20,000 apartments in France are now heated by warm underground water drawn from a heat reservoir in a geologic structure near Paris called the Paris Basin.

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