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characteristics of evolution
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  演化特征
    Based on the researches of kinematic analogue in the Qintong depression, initial model and boundary conditions of simulation of structural stress evolution have been cnstructed appropriately. Taken ST365 profile as an example,the characteristics of evolution and the figures of stress σ_x,σ_y and τ_(xy)at all stages have been given by applying nonlinear theory and plastic flow theory to the study in this region,their geological significance of petroleum and natural gas has been explored .
    本文以溱潼凹陷地质演化的运动学研究为基础,合理地建立构造应力演化研究的初始模型和边界条件,运用非线性理论和塑性流动理论,以中部剖面ST365为例,模拟了各期次应力σ_x、σ_y和τ_(xy)的演化特征和图解,并对其油气地质意义进行了初步探讨。
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    Based on an investgation of regional geoenvironmental setting,this paper deals with the basic features and the spatial variations of the oil-field water of Minghuazhen Formation in the study area and describes the stages and characteristics of evolution in the process of geological history. It is pointed out that the modern evolutionary pattern of oil_field water chemistry follows the direction of concentrated salinization and normal metamorphism.
    在论述地质环境背景的基础上 ,揭示了研究区上第三系明化镇组油田水化学的基本特征和空间分布规律 ,重溯其在地质历史过程中形成演化的阶段和特点 ,论证了油田水现代化学是遵循浓缩盐化、正向变质作用方向演变形成的。
短句来源
    Deformation mechanism is attributed to plastic rheology and ductile shear at middle-deep levels in the crust,experiencing characteristics of evolution during multiphase and stages.
    变形机制属地壳中深层次塑性流变和韧性剪切,经历了多期多阶段演变等特征。
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  characteristics of evolution
Furthermore, the characteristics of evolution for the disturbances of different modes in the hypersonic sharp cone boundary layer were discussed.
      
Changes in the quantitative characteristics of evolution of the phase variables (maximum Lyapunov exponent and Hausdorff dimension) are also studied as a function of the external field.
      


Studying stress evolution is a key link of basin simulation. The distribution of stress at each stage decided the migratory direction of petroleum and natural gas. Based on the researches of kinematic analogue in the Qintong depression, initial model and boundary conditions of simulation of structural stress evolution have been cnstructed appropriately. Taken ST365 profile as an example,the characteristics of evolution and the figures of stress σ_x,σ_y and τ_(xy)at all stages have been given by applying...

Studying stress evolution is a key link of basin simulation. The distribution of stress at each stage decided the migratory direction of petroleum and natural gas. Based on the researches of kinematic analogue in the Qintong depression, initial model and boundary conditions of simulation of structural stress evolution have been cnstructed appropriately. Taken ST365 profile as an example,the characteristics of evolution and the figures of stress σ_x,σ_y and τ_(xy)at all stages have been given by applying nonlinear theory and plastic flow theory to the study in this region,their geological significance of petroleum and natural gas has been explored .

构造应力演化研究是盆地模拟的重要环节,各期次构造应力分布情况决定了油气的运移方向。本文以溱潼凹陷地质演化的运动学研究为基础,合理地建立构造应力演化研究的初始模型和边界条件,运用非线性理论和塑性流动理论,以中部剖面ST365为例,模拟了各期次应力σ_x、σ_y和τ_(xy)的演化特征和图解,并对其油气地质意义进行了初步探讨。

Based on an investgation of regional geoenvironmental setting,this paper deals with the basic features and the spatial variations of the oil-field water of Minghuazhen Formation in the study area and describes the stages and characteristics of evolution in the process of geological history. It is pointed out that the modern evolutionary pattern of oil_field water chemistry follows the direction of concentrated salinization and normal metamorphism.

在论述地质环境背景的基础上 ,揭示了研究区上第三系明化镇组油田水化学的基本特征和空间分布规律 ,重溯其在地质历史过程中形成演化的阶段和特点 ,论证了油田水现代化学是遵循浓缩盐化、正向变质作用方向演变形成的。

Of ductile shear belts,deformation fabric considerably developed in Yiwu,Xingjiang Province and sequence evolution occur apparently,there exist transformation of thrust shear and ductile-brittle deformation,the deformation period is in early Variscan previous to late Permian.Its age of forming is earlier than magma eruption in the area of researching.Deformation mechanism is attributed to plastic rheology and ductile shear at middle-deep levels in the crust,experiencing characteristics of evolution during...

Of ductile shear belts,deformation fabric considerably developed in Yiwu,Xingjiang Province and sequence evolution occur apparently,there exist transformation of thrust shear and ductile-brittle deformation,the deformation period is in early Variscan previous to late Permian.Its age of forming is earlier than magma eruption in the area of researching.Deformation mechanism is attributed to plastic rheology and ductile shear at middle-deep levels in the crust,experiencing characteristics of evolution during multiphase and stages.This shear zone dominates the ore-forming belts,mineralized zones and orebody attitudes in the region.A primitive treatment of metallogensis and regularities in distribution is made for the chief minerals as mesothermal-epithermal gold-silver-copper,ore-forming course is generally judged to the late Paleozoic with geologic events occurred frequently and mineralization bear multiphase and multi origins.

新疆伊吾韧性剪切带变形组构较发育,序列演化明显,存在逆冲剪切和韧—脆性变形转换,变形时代为华力西早期,早于晚二叠世。其形成时代应早于研究区岩浆侵入活动时期。变形机制属地壳中深层次塑性流变和韧性剪切,经历了多期多阶段演变等特征。该剪切带控制了该区的成矿带、矿化带、矿体的产状。对中—低温热液金银铜等主要矿产的成矿作用和分布规律作了初步探讨,粗略判断成矿过程大概是在地质事件多发的晚古生代,并且成矿具多期性和多源性。

 
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