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热演化的
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  thermal evolution
     Based on the consideration of coupling of the rotational and thermal evolution, I research two kinds of heating mechanisms induced by the spin-down of the star: crust deconfinement heating and r-mode dissipation heating.
     在此背景下,本文又基于综合旋转演化与热演化的考虑,重点研究了两类由旋转导致的加热机制(外壳相变加热和r模耗散加热)对正常态和色超导态奇异星热演化的贡献。
短句来源
     METHOD OF NUMERICAL SIMULATION ON TECTONICALLY THERMAL EVOLUTION
     构造热演化的数值模拟方法
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     Four hierarchies of overpressure retardation on the thermal evolution of organic matter and hydrocarbon generation were recognized. ①All aspects of OM maturation were retarded by overpressure.
     识别出超压抑制有机质热演化和生烃作用的4个层次:①超压抑制了有机质热演化的各个方面,包括不同干酪根组分的热降解(生烃作用)和烃类的热演化;
短句来源
     The restraining effect of abnormal pore fluid pressures on organic matter thermal evolution is conditioned,and that of overpressure on organic matter evolution is evident under the circumstances of early developed overpressures,high original organic matter abundance and organic matter high thermal evolution retained products,which is related to the closeness of pressure system.
     异常孔隙流体压力对有机质热演化的抑制作用是有条件的 ,在超压早期发育、高原始有机质丰度和高有机质热演化产物滞留的情况下超压对有机质的演化具有明显的抑制作用 ,并且其具体表现和压力系统的封闭性有关。
短句来源
     Controlled by the deposition and erosion as well as the basin thermal evolution, the hydrocarbon generation was of multi-phases.
     受沉积剥蚀及盆地构造—热演化的控制,生油岩系的生烃阶段与过程具有多期次的特征。
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  “热演化的”译为未确定词的双语例句
     Fission track evidence for the tectonic-thermal history of the Hefei basin
     合肥盆地构造热演化的裂变径迹证据
短句来源
     e. stage Ⅰ and stage Ⅱ, which by 0. 60% ~0.65% Ro,and moreover, the difference of maturity in different tectonic units was showed.
     (4)苏北盆地有机质热演化阶段划分为阶段Ⅰ和阶段Ⅱ,其界线出现在Ro0.60%~0.65%,并揭示出不同构造单元有机质热演化的不均衡性。
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     The Relationship between Methyl Phenanthrene Ratios and the Evolution of Organic Matter
     甲基菲比值与有机质热演化的关系
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     The free radical concentration (Ng) of kerogen is a valid index to study thermal maturation of organic matter and paleotemperature of sedimentary basin.
     干酪根自由基浓度是研究有机质热演化的有效指标之一.也是研究沉积盆地古地温的热参数之一。
短句来源
     ④Overpressure had no detectable effect on All aspects of OM maturation.
     ④超压对有机质热演化的各个方面均未产生可识别的影响。
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  相似匹配句对
     METHOD OF NUMERICAL SIMULATION ON TECTONICALLY THERMAL EVOLUTION
     构造演化的数值模拟方法
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     Modelling of microstructural evolution of aluminium alloy during thermomechanical processing
     铝合金变形组织演化的模拟
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     HOT
     报!
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     Why Chinese?
     汉语
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     The Logic about Evolution of Institution
     制度演化的逻辑
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  thermal evolution
Thermal evolution of a fan submitted to high temperature in a confined environment
      
The present work describes a complete numerical study of the thermal evolution carried out for a ventilation fan.
      
The effect exerted by the anion of Pb and Zn salts on the thermal evolution of the structure of polymetallosiloxanes formed by base-catalyzed (NH4OH) hydrolytic polycondensation of ethyl silicate with zinc(II) or lead(II) salts was studied.
      
The boundary conditions for calculating the thermal evolution of the early Earth are refined by simultaneously analyzing the sizes of impact thermal anomalies and the model size distributions of projectiles (the mass spectrum of planetesimals).
      
The chemical and thermal evolution of the baryon component in the gravitational field of low-mass primordial dark-matter halos during their virialization is studied.
      
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Characteristics of thermal evolution with in creasing depth of organic matter in different sedimentary basins of Meso-Cenozoicage in China are reviewed on the basis of analytical data of soluble saturated hydrocarbons, asphaltenes and insoluble kerogen etc. from source rocks. Six stages are proposed for the whole process of evolution, and the structural changes of organic matter for each stage are studied with data obtained form analysis of elements, infrared spectrum, chromatogram, chromatogram-mass spectrogram...

Characteristics of thermal evolution with in creasing depth of organic matter in different sedimentary basins of Meso-Cenozoicage in China are reviewed on the basis of analytical data of soluble saturated hydrocarbons, asphaltenes and insoluble kerogen etc. from source rocks. Six stages are proposed for the whole process of evolution, and the structural changes of organic matter for each stage are studied with data obtained form analysis of elements, infrared spectrum, chromatogram, chromatogram-mass spectrogram and paramagnetie resonanceetc., leading to the further inquiry of the mechanism and process of oil and gas generation,

本文根据生油岩中可溶有机质饱和烃及其重组分——沥青质和不溶有机质干酪报等资料,深入研究了我国中、新生代不同类型沉积盆地有机质随埋深的热演化特征,在此基础上提出了有机质及原油热演化过程六个阶段的划分。通过有机元素、红外、色谱、色谱-质谱联用、顺磁等资料,研究了各热演化阶段有机质的结构组成变化,进一步探索了油气的生成机理和过程。

Taking into account of the three factors of kerogen types(T), temperature

本文提出的定量评价生油岩的TTT法,同时考虑了生油母质类型(T)、有机质成熟的温度(T)和时间(T)三个因素;它采用生油岩中不同类型干酪根在不同热演化阶片上的裂解烃产率、有机碳、氯仿沥青A和总烃等四个参数,可以直接计算生油岩的生烃量和排烃量.本文结合松辽盆地的实际资料,对青一段生油岩的生烃量、排烃量进行了计算,其结果与烃类垂向分布及有机质成熟史相吻合.

In Maling oilfield and its vicinity,the process of pore evolution in Yan-10sandstones of Jurassic during diagenesis is discussed in this paper.The mainconclusion proposed are as follows:1)The pore evolution is in fact a process of gradual substitution of secondarypores for the primary ones;2)The decrease of porosity in quartz arenites is mainly due to the precipitationof authigenic minerals in the sandstone pores during diagenesis;while the de-crease of porosity in arenites with more flexible component is mainly...

In Maling oilfield and its vicinity,the process of pore evolution in Yan-10sandstones of Jurassic during diagenesis is discussed in this paper.The mainconclusion proposed are as follows:1)The pore evolution is in fact a process of gradual substitution of secondarypores for the primary ones;2)The decrease of porosity in quartz arenites is mainly due to the precipitationof authigenic minerals in the sandstone pores during diagenesis;while the de-crease of porosity in arenites with more flexible component is mainly caused by compaction during diagenesis;3)The secondary solution pore mainly developed after its diagenetic stage bydissolution and kaolinization in arenite which is abundant in feldspar.This pro-cess is likely to be related to the decarboxylation of organic matter in interbeddedcoal seams and carbonaceous shales by thermalizatin;4)The clastic constituents of sandstone controlled by source materal distinctlyaffect the development of pores.Therefore,the primary and secondary pores insandstones favourable can be predicted on the basis of finding out the sourcematerial of sediments;5)Diagenesis obviously affects on the texture and the uniformity of pores insandstones.

本文论述了鄂尔多斯盆地南部的主力油层(侏罗纪延安统延_(10)砂层组)在成岩过程中的孔隙演化史。作者认为:1.成岩作用改造砂层(岩)的过程,也是改造砂层(岩)中孔隙的过程,砂层(岩)中孔隙的演化史是原生孔隙不断消失和次生孔隙不断形成和消失的过程。2.石英砂屑岩(Quartz arenite)的孔隙度降低,主要是成岩期自生矿物在砂岩孔隙中的沉淀作用造成的;含柔性碎屑组分多的砂屑岩,其孔隙度的降低主要是成岩期的压实作用造成的。3.砂岩中碎屑矿物和自生矿物在成岩期的溶解作用,能产生可观的次生溶孔。本区延(?)砂层组中的次生溶孔主要发育在富含长石的砂屑岩中。此外,还有受力破碎产生的裂隙孔和某些砂岩组分脱水产生的收缩孔等次生孔隙。4.延_(10)砂层组中的次生溶孔,形成于沉积物已固结成岩的阶段。紧邻延(?)砂层组之上的煤系地层和其下的三叠纪延长统泥质岩中有机质,在埋藏成岩热演化过程中所产生的二氧化碳,使地层水的 PH 值降低成为酸性水,这些水进入砂岩中,使其中的长石被溶蚀和高岭土化,从而产生了次生溶孔。5.受沉积物源控制的砂岩碎屑组分,对砂岩原生粒间孔隙的保存和次生孔隙的发育有明显的控制作用。可以在查明沉积物源的基础上...

本文论述了鄂尔多斯盆地南部的主力油层(侏罗纪延安统延_(10)砂层组)在成岩过程中的孔隙演化史。作者认为:1.成岩作用改造砂层(岩)的过程,也是改造砂层(岩)中孔隙的过程,砂层(岩)中孔隙的演化史是原生孔隙不断消失和次生孔隙不断形成和消失的过程。2.石英砂屑岩(Quartz arenite)的孔隙度降低,主要是成岩期自生矿物在砂岩孔隙中的沉淀作用造成的;含柔性碎屑组分多的砂屑岩,其孔隙度的降低主要是成岩期的压实作用造成的。3.砂岩中碎屑矿物和自生矿物在成岩期的溶解作用,能产生可观的次生溶孔。本区延(?)砂层组中的次生溶孔主要发育在富含长石的砂屑岩中。此外,还有受力破碎产生的裂隙孔和某些砂岩组分脱水产生的收缩孔等次生孔隙。4.延_(10)砂层组中的次生溶孔,形成于沉积物已固结成岩的阶段。紧邻延(?)砂层组之上的煤系地层和其下的三叠纪延长统泥质岩中有机质,在埋藏成岩热演化过程中所产生的二氧化碳,使地层水的 PH 值降低成为酸性水,这些水进入砂岩中,使其中的长石被溶蚀和高岭土化,从而产生了次生溶孔。5.受沉积物源控制的砂岩碎屑组分,对砂岩原生粒间孔隙的保存和次生孔隙的发育有明显的控制作用。可以在查明沉积物源的基础上,预测砂岩原生孔隙和次生孔隙的有利分布区.6.本区延_(10)砂层组的某些孔?

 
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