湖南省地壳经历了漫长的地质演化过程，造就了各种岩石类型。
Hunan provincial crust goes through the long geological evolution process and forms many kinds of rocks.
海森博士认为，考虑矿物的进化特性是确定行星的地质演化时间的有效手段。
Dr Hazen argues that considering minerals in evolutionary terms is a powerful way to help identify how far a planet has developed geologically.
开合运动是地球运动的基本形式，开合构造是地质演化的基本构造。
Opening-closing is a basic form of the Earth's movement and opening-closing tectonics is a basic tectonics in geological evolution.
对研究孟家屯岩组，以及泰山岩群和整个鲁西的地质演化历史有重要的意义。
These results are significant in studying the Mengjiatun Formation, Taishan Group, and the geological evolution of western Shandong.
通过对具体地区的实际模拟，总结出了煤层气地质演化史数值模拟研究的方法。
By the actual simulation of the concrete region, summarizes the investigative method of simulation in the geological evolution history of coal bed gas.
根据前人成果，建立了煤层气地质演化史模型并以此为基础研制了计算机模拟系统。
According to the result of past researched, the author of this article established the geological evolution history model of coal bed gas and computer simulation system on this base.
对盆地深部未知区进行模拟计算，查明了未知区山西组主煤层煤层气地质演化史特征。
Simulation calculation of deep buried and unknown area was conducted and CBM geologic evolution process in the area was founded out.
运用数值模拟方法对河东煤田柳林矿区主煤层煤层气地质演化史进行了定量模拟研究。
The paper has quantitatively studied the evolution history of coalbed methane (CBM) of main coal seams in Liulin Mining Area of Hedong Coalfield by using numerical simulation method.
从地质演化和成矿动力学角度，长江中下游成矿带在我国、甚至世界上具有鲜明的特色。
In view of geological evolution and metallogenic dynamics, the MiddleLower Yangtze metallogenic belt has its own distinguishing features in China, even in the world.
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.
正确归并和界定地质事件群在研究区域地质演化特征或进行大区域间的地质对比时具有十分重要意义。
It is of great significance to define geological events and merge them into an event group in the research on regional geological evolution and geological correlation between large regions.
西昆仑以其强烈的构造变形、频繁的岩浆活动、漫长的地质演化历史及特殊的大地构造环境而具有得天独厚的成矿地质条件。
Magmation was frequent, tectonic deformation was violent, the history of geological evolvement was long and geological condition of producing mineral was good in West Kunlun.
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.
现在，地质证据和恒星演化模型之间这种明显的矛盾被称为“微弱年轻太阳悖论”。
Now, this apparent contradiction between geologic evidence and the stellar evolution model became known as the faint young Sun paradox.
这对研究西昆仑山早前寒武纪陆壳增生及构造演化提供了重要的地质资料。
This study supplies new geological data for research of the early Precambrian crust growth and tectonic evolution of Western Kunlun.
早古生代花岗岩的确认对该区地质构造演化研究具有重要意义。
The identification of the Early Caledonian granites is of important significance in studying the geological tectonic evolution of the area.
结果研究总结得出了世界主要国家砂岩型铀矿的地质特征、主要的产铀盆地模式及其演化。
Results Show the geology feature, main metallogenic models and its evolution connections of sand-stone type uranium deposit in all the world.
地球化学省是区域岩石圈演化过程中形成的，是具有共同成因的、一定规模的地质单元的地球化学表现。
The geochemical province, formed in the course of regional lithospheric evolution, is characterized by geological units with common origin and certain sizes.
孔雀河斜坡由于受多次构造运动作用，石油地质条件都受到构造演化的影响。
Because of several tectonic moments, the petroleum geologic conditions in Kongquehe slope are effected by tectonic evolution.
含油气系统中的流体地质作用贯穿于烃类生成、运移、聚集及后期演化的各个阶段。
Geological function of fluid occurred at the various stages of generation, migration, accumulation and later evolution of hydrocarbon in the petroleum system.
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.
青藏高原新生代以来的持续性、阶段性隆升是地球演化过程中重要的地质和环境事件。
The continuous and periodic uplift of the Qinghai-Tibet Plateau since the Cenozoic is an important geological and environmental event during the evolution of the Earth.
利用盆地模拟技术模拟烃源岩各地质时期的热演化阶段。
It USES basin simulation technique to simulate the heat evolution stages of various geologic period of hydrocarbon source rock.
简要阐述菱形地块地质构造演化及成矿作用特征。
In this paper, we briefly describe the characteristics of its geological tectonic evolution and metallogenesis.
本文讨论了能动断层概念的演化，提出了针对我国地震地质环境与条件的能动断层识别标志。
The paper discusses the evolution of the capable fault concept and points out the identification marks of capable faults in accordance with the seismic environment and condition in China.
大型矿集区的形成，是在地质历史演化进程中，多矿种大矿量超常聚集的结果。
The formation of large ore concentated are results from the anomalous concentration of multi mineral resources and large amount of ore materials during the process of geologic evolution history.
作者提出了一个变质地质体在一次变质—变形旋回中构造演化的理想模式。
According to this analysis, an ideal model of geological evolution in a metamorphic -deformation cycle is suggested.
唐古拉山地区广泛出露早新生代陆相地层，较好地记录了青藏高原北部新生代地质构造演化与古环境变迁的过程。
The Cenozoic fluvial strata, exposed widely in the Tanggula Mountains, detaily recorded the information of the uplift of the northern Tibet Plateau and the paleoenvironmental evolution.
异常区的空间分布演化与震中、地质构造和地热等有密切关系。
The variation of the spatial distribution of the anomaly region is closely related to the epicenter, geological structure and geothermal activity.
异常区的空间分布演化与震中、地质构造和地热等有密切关系。
The variation of the spatial distribution of the anomaly region is closely related to the epicenter, geological structure and geothermal activity.
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