构造变动

  • 网络tectonic disturbance;diastrophism
构造变动构造变动
  1. SQ2层序由于构造变动频繁,加上后期剥蚀严重,导致聚煤作用逐渐减弱。

    As for SQ2 sequence , due to frequent changes in structure and subsequent strong denudation , the coal accumulation was gradually weakened .

  2. 叠合盆地构造变动破坏烃量研究方法探讨

    Study on Destroyed Hydrocarbon Amount by Tectonic Event in Superimposed Basins

  3. 多旋回构造变动区的油气系统

    The petroleum system in the region of polycyclic tectonic movement

  4. 构造变动比较强烈地区的油气勘探远景预测

    Prediction of hydrocarbon exploration potential in stronger structural dislocation area

  5. 中国大陆岩石圈最新构造变动与地震灾害

    Late Quaternary tectonic deformation and earthquake hazard in continental China

  6. 临清坳陷东部构造变动特征及控制作用

    Tectonic variation characteristics and controlling function in the eastern part of the Linqing depression

  7. 地球构造变动对土壤分带格局和古气候事件的影响

    Influence of tectonic activities on the regional distribution of soils and on paleoclimatic events

  8. 构造变动对油气藏保存的影响

    The structural event influence on preserving hydrocarbon pools

  9. 济阳坳陷构造变动破坏烃量反演模拟

    Inversion modeling of the hydrocarbon amount destroyed by tectonic event in the Jiyang Depression

  10. 简单剪切&中国东南地区活动构造变动机制讨论

    A simple SHEAR-DISCUSSING on the fluctuation mechanism of active structures in southeast area of China

  11. 某些构造变动与流体运移关系分析

    Relationship of Tectonic Moves and Fluid Migration

  12. 构造变动和地震与块体活动及区域构造应力场变化密切相关。

    Tectonic deformation and earthquakes have close relationship to the evolution of regional tectonic strain field .

  13. 油气藏保存条件是构造变动比较强烈地区油气勘探的关键。

    The reservoir preservation conditions are the key of the hydrocarbon exploration in stronger structural dislocation area .

  14. 地下流体及流体力普遍存在且对构造变动产生影响。

    The subsurface fluid and fluid force produced by subsurface fluid universally exist and have influence on tectonism .

  15. 鄂尔多斯盆地以稳定著称,构造变动微弱,地层平缓,盆地内部褶皱、断裂不甚发育。

    Ordos Basin has been well known of stability , with the weakly tectonic movement , gentle stratum .

  16. 塔里木盆地台盆区构造变动与油气聚散关系

    A discussion on the relationship between tectonization and hydrocarbon accumulation and dissipation in the platform-basin transitional area of Tarim basin

  17. 研究表明,构造变动破坏烃量主要有三种形式:剥离区域盖层、切断区域盖层的连续性和破坏圈闭的有效容积。

    The removal of the regional cap rock , the destruction of the regional cap rock continuity and the effective volume of traps .

  18. 研究中采用了易于获得的两个地质参数,即剥蚀率和地层变形程度作为定量化指标,拟合出构造变动强度的定量化公式。

    The two parameters of denudation rate and stratum deformation degree can be used to fit the quantitative characterization formula of tectonic movement intensity .

  19. 主要矿体均受含锰岩系、后期构造变动、风化作用的控制,矿体呈似层状、透镜状。

    The main orebodies are controlled by the manganese-bearing rock series , post-stage tectonic events and weathering and show the form of stratoid and lenticular .

  20. 文中提供的实例表明,采用构造变动与油气公布相关分析法,是提高该带油气勘探效率的有效方法。

    It is illustrated that the correlation analysis of structural evolution to hydrocarbon occurrence is an effective method for raising hydrocarbon exploration efficiency in this structural belt .

  21. 该带在形成过程中经历了块断抬斜、重力滑动、反拖牵引、盐岩拱升等多种形式的构造变动。

    The central uplift belt underwent a series of structural evolution : fault block tilting , gravity slumping , inverse drag , rock salt uplifting and so on .

  22. 惠州凹陷是个十分复杂的凹陷,经历了多次的构造变动,总体为张性盆地的背景下,断层表现出张性或张扭性的特征,具有多期活动的特点。

    Huizhou Depression is a very complicated depression , in the background of extensional stress basins , after lots of structural actives , characteristics of faults is extensional and transtension .

  23. 无论是从生产勘探开发还是科学研究的角度,都有必要对盆地中新生代的构造变动与后期改造进行综合研究。

    Whether in exploitation or in scientific study , it is necessary for us to study on tectonic evolvement and late reformation of the Basin in Mesozoic and Cenozoic period .

  24. 沾化凹陷东部是济阳坳陷构造变动最为复杂的地区之一,同时也是胜利油田油气资源最为丰富的地区之一。

    Eastern Zhanhua sag is one of the most complicated tectonism areas in Jiyang depression , and it is also one of the most hydrocarbon proliferous areas in Shengli oilfield .

  25. 结论对于构造变动强烈、烃源岩层位多、热演化历程复杂的叠合盆地,其油气藏类型复杂,油气勘探的难度增大。

    Conclusion The types of reservoir are complex , and the exploration of petroleum is every difficult in the basin of strong structural movement , multi-layer source rocks , complex thermal history .

  26. 焉耆盆地经历了复杂构造变动及地层遭到强烈的剥蚀,这制约了对盆地发生、发展、衰退和消亡等过程的认识。

    Yanqi basin was underwent complex structure change and strata were eroded strongly which restrict the cognition of the basin , such as generation , development , decline and disappear , et al .

  27. 上第三系油气藏属于次生油气藏,它们主要是由于上新世以后因构造变动导致下第三系油气藏调整和破坏,油气发生向上再运移而聚集形成的。

    And that in the upper Tertiary reservoirs are of secondary oil / gas reservoirs , accumulated through upward remigration of hydrocarbons from the adjustment and damage of the lower Tertiary reservoirs , due to post Pliocene tectonic movements .

  28. 构造变动过程中的快速隆升异常区和与之相伴生的高梯度变形带、以及显著地断层活动异常,是较强地震孕育的标志,地震往往发生在具有较高应变积累的区域附近;

    The abnormally quick uplifting region and its associated high-gradient deformation zone as well as obvious abnormality of fault activity are symbols of strong earthquakes , and earthquakes commonly take place in and near the region with high strain accumulation .

  29. 本区构造变动划分为三个大的阶段,即:前中生代褶皱基底的形成和稳定古陆发育阶段、中生代古陆裂解阶段、新生代块断活动及整体沉降阶段。

    The tectonism in this area can be divided into three phases , that is the folded basement formation and stable ancient land in Pre-Mesozoic , ancient land cracking phase in Mesozoic , the faulted activity and subsidence phase in Cenozoic .

  30. 这些地质事件的发生和构造变动,与周邻各构造域,特别是中国东、西部(含青藏高原)重大构造运动的复合、叠加及其与时彼此消长变化密切相关;

    The happening of these geological events and structural fluctuation are closely related with the compound , superimpose , change with time and strong-weak of major structural movement of peripheral structural domain especially that of the east and west of China .