在制定油气开发方案前，必须建立一个完整的构造演化、沉积作用、成岩作用的综合模式，进而预测有利构造沉积成岩相带。
So, before a development scheme of oil and gas is formulated, a synthetic model on structural evolution, sedimentation, and diagenesis should be set up to predict the favourable zones.
俯冲带和地球系统演化过程中的动力学及物质循环。
And dynamics and mass circulation in subduction zones and Earth system evolution.
上述理论阐明不了大陆岩石圈、大陆造山带的组成，结构与演化，也与当代的基础理论不尽吻合。
This theory could not explain the composition, structure and evolution of continental lithosphere and continental orogenic belt, and also is not in line with modern scientific theory.
最后讨论了本区高压变质带的成因演化。
At last, evolution of high pressure metamorphic belt is discussed.
本文从分析区域构造背景入手，详细探讨了该带前第三系构造体系特征及其形成和演化过程。
This paper discusses in detail the pre-Tertiary tectonic system and its evolutionary process based on regional background analysis.
根据构造演化剖面的分析结果，确定了高邮凹陷南部断阶带。
The south terrace in Gaoyou sag is presented, according to the analysis of the structural evolution section.
韧性剪切带变形变质作用及演化阶段是确定金矿化能否形成的重要因素。
The evolution and deformation and metamorphism of ductile shear zone takes an important role in the formation of gold mineralization.
这一结果与粤西-海南成矿带的成矿时代特征及特提斯构造演化特点相吻合。
This is identical with the characteristics of west Guangdong Hainan gold metallogenic belt and the evolution of Tethys tectonics.
这些剪切带阵列经历了长期的演化历史，具正向的、反向的、螺旋形或旋回式的流变学演化轨迹。
The shear zone arrays in Tongbai - Dabie orogenic belt experienced a long history of evolution, showing the normal, inverse and screw -type or cyclic rheological evolutional paths .
这些转换断层系统对中国大陆东、南缘含油气盆地和边缘构造带的形成和地质演化起着重要的作用。
These transform fault series play an important role in the formation and the geological evolution of the Southeastern China continental margin basins and the tectonic-structural zones.
指出，现今大量的地球化学资料证实，烃类在很大程度上是由天然的CO、CO2、H2在全球无机合成带的地质演化过程中形成的。
It is approved from a great number of geochemical data that hydrocarbons could be formed from co, CO2 and H2 in global inorganic synthetic zones by geologic evolution process to a great extent.
盆地形成演化受特提斯构造带地球动力学控制。
Its formation and evolution was controlled by the dynamics of the Tethys tectonic belt.
吉林中部烟筒山地区的硅质岩带是研究古亚洲洋构造演化的一个关键地区。
The siliceous rock zone in Yantong mountain area, central Jilin Province, is the key region for studying the paleo-Asian ocean tectonic evolution.
本文利用测井、钻井和C、O同位素等资料，研究了核二段各砂组沉积时期的沉积环境、相带分布、砂体展布以及沉积演化规律。
Sedimentary environment and its evolution, distribution of sedimentary facies and sand bodies are discussed on the base of the data of log, drilling and c, o isotope.
在中生代，该盆地的形成与演化受特提斯构造带的控制。
In Mesozoic era, the formation and evolution of the Mesozoic Lanping Simao basin were controlled by the Tethys tectonic zone.
俯冲带变质脱水作用对俯冲带的流体形成、岩浆起源和演化起着重要的控制作用。
Metamorphic dehydration in subduction zones plays a significant role in the genesis of slab-derived fluids and the generation and evolution of arc magmas.
盘山系统形成演化过程中造山带和沉积盆地之间一切相互作用的总和即为盆山间的耦合关系。
The coupling relationships between sedimentary basins and orogenic belts refer to all of their interactions in their formation and evolution.
测年结果为研究东昆仑造山带的演化历史提供了重要的年代学资料。
The dating results provide important data for the evolutionary history of the East Kunlun orogenic belt.
利用正演模拟方法，分析了主要断裂带的发育演化。
The evolution of major fault zones is analysed with the forward modelling method.
该项研究对冲断带烃源岩的演化过程分析和烃类相态分布的控制因素分析具有实际指导意义。
The study is of practical significance for analyzing the evolutionary process of source rocks in thrust belts and the control factors of phase distribution of hydrocarbons.
通过对区内标志岩层组合的系统追索，所确定的构造变形特征，对正确认识该造山带的形成演化具有重要地质意义。
Thedetermined structural deformation features through systematic tracing the marker bed in the area are geologically significant to correctly recognizing the formation and evolution of the orogen.
经地震剖面解释及构造演化分析，该区主要断裂带是油气运移的良好通道，且不存在油气的严重漏失。
Seismic section interpretation and structural evolution analysis reveal that the main fractured zones are good hydrocarbon migration pathways and no serious leakage of hydrocarbons exists.
并对组成喜马拉雅造山带各种主要沉积盆地进行了构造沉降分析，研究盆地演化动力机制；
The tectonic subsidence analysis and dynamic mechanism of the basin evolution are processed in the main sedimentary basins across this belt.
最后，讨论了该断裂带的形成与演化。
The formation and evolution of the fault is discussed as well.
重点论述了风化带内煤层开采的覆岩破坏移动演化特征；
The characteristics of damage, movement, evolution in mining coal bed in weathered zone were discussed mainly.
造山带区域构造演化与大规模成矿作用是同一大陆动力学过程的不同表现。
The regional tectonic evolution and extensive mineralization in orogenic belts are different expressions of the same continental dynamic process.
这些火成岩组合有规律地分布在构造走廊域内，是揭示东昆仑造山带构造演化的关键所在。
These igneous assemblages are regularly distributed in the corridor and seem to be the key to revealing the tectonic evolution of the East Kunlun orogenic belt.
抽拉—逆冲岩片构造是杨志华等在研究秦岭造山带过程中提出的一种关于大陆造山带形成与演化的全新构造观。
The draw thrust sheet tectonics is a new viewpoint put forward by Yang Zhihua during his study on development and evolution of the Qinling orogenic belt.
论述了川西甘孜—理塘断裂带构造演化与金矿床成矿作用的关系，总结了区内金矿化的特征和金矿床类型。
The tectonic evolution of Garze Litang fracture zone, the characteristics of gold mineralization and types of gold deposit as well as their relationship in west Sichuan are expounded in this paper.
论述了川西甘孜—理塘断裂带构造演化与金矿床成矿作用的关系，总结了区内金矿化的特征和金矿床类型。
The tectonic evolution of Garze Litang fracture zone, the characteristics of gold mineralization and types of gold deposit as well as their relationship in west Sichuan are expounded in this paper.
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