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The absolute majority of tectonists base their constructions on the model of an unmovable Earth.

绝大部分构造学家的学说是建筑在不运动的地球模型上的。

By comprehensively using the theories and methods of coal-gas geology, coal petrology, tectonophysics and earth dynamics.

本文综合运用瓦斯地质学、煤岩学、构造物理学和地球动力学的理论和方法。

The Altai Paleozoic orogenic belt of Xinjiang Autonomous Rejoin is geologically wellknown both domestic and abroad by the intensive development of low-pressure metamorphism and granitic magmatism. Within pelitic metamorphic rocks, even though sillimanite is well developed and the low-pressure minerals like andalusite and cordeirite etc. are quite common, the assemblage of garnet and staurolite is more important.

中文题名阿尔泰海西造山带中-低压递增变质作用特征及其地球动力学副题名外文题名 Features and geodynamics of the low-to mid-pressure progressive metamorphism in the Altai hercynian orogenic belt 论文作者郑常青导师卢良兆徐学纯教授学科专业矿物学、岩石学、矿床学研究领域\研究方向变质地质学学位级别博士学位授予单位吉林大学学位授予日期2001 论文页码总数132页关键词阿尔泰造山带造山带构造地质馆藏号BSLW /2003 /P542 /1 新疆阿尔泰古生代造山带以低压变质及花岗质岩浆作用广泛发育闻名国内外,泥质变质岩系中矽线石较发育,红柱石和堇青石等低压特征矿物相当常见,但是,石榴石—十字石的组合更普遍。

A good many mico-landblock of the early Neoproterozoic-Cambrian volcanic rock that distribute in the Tianshan orogenic belt and on its both sides, and the Carboniferous-Permian volcanic rocks that widely distribute in the Tianshan and adjacent regions are selected for subject investigating in this paper. Renewing the ocean-land format and ocean-land conversion process of Tianshan orogenic belt in the Paleozoic is the masterstroke for this paper. On the basis of detailed field investigation, many subjects, such asregional lithology、geochemistry、structural geology、volcanic sedimentology geology、sotope geochronology and synthesis analysis study of geophysics data, are adopted as instrumentality in the paper, this study lays emphasis on the formation, evolution and dynamics of early Neoproterozoic-Cambrian and Carboniferous-Permian volcanic rock in the Tianshan and its adjacent regions to find out Carboniferous-Permian volcanic rock property, eruptive sequence, time and space distribution characteristics, to resume and reconstruct evolution process of Carboniferous-Permian volcanic rock, and to explore connection of magmatism process and lithosphere stretching action of neopaleozoic ocean-land transformation in the Tianshan region.

本文选择分布于天山及其两侧的诸多微陆块上新元古代—早寒武世火山岩和天山地区广泛发育的石炭纪—早二叠世火山岩为研究对象,以恢复重建天山造山带古生代洋陆格局和洋陆转换过程为主线,在详细的野外工作基础上,综合运用区域岩石学、地球化学、构造地质学、火山沉积学、同位素地质年代学、区域地球物理资料综合分析研究等多学科手段,重点研究天山及其邻区新元代—早寒武世和石炭—二迭纪火山岩系的形成演化及其动力学,查明天山石炭纪火山岩系的性质、喷发序列、时空分布特点,恢复重建其形成演化过程,探索天山地区晚古生代洋陆转换过程中火山岩浆作用与岩石圈拉伸作用的关系。

Coding;Communication;Communication systems;Communication technology;Components;Data;Data description;Data processing;Data processing system;Data records;Data representation;Data transfer;Definition;Definitions;Earth's surface;Encoding;Geodesy;Geographic information;Geographical;Geography;Geology;Geomatics;Geotechnics;Information;Information exchange;Information processing;Information technology;Schemes;Topology

中文标题地质信息。数据描述。传输中文主题词信息技术;信息;数据处理;地质的;信息交流;地球表面;地质信息管理;地质信息;定义;图表;数据处理系统;大地构造学;地质学;拓扑学;数据传送;信息处理;数据记录;通信系统;元部件;地理学;数据表示;传播技术;传播学;数据;编码;编码;数据描述;大地测量学

Communication;Communication systems;Communication technology;Components;Data;Data description;Data management;Data processing;Data processing system;Data records;Data representation;Data transfer;Definition;Definitions;Earth's surface;Encoding;Geodesy;Geographic information;Geographical;Geography;Geology;Geomatics;Geotechnics;Information;Information exchange;Information processing;Information technology;Metadata;Metafile;Quality;Quality assurance;Schemes;Specification;Topology

中文标题地质信息。数据描述。元数据中文主题词大地测量学;数据描述;编码;数据;传播学;传播技术;数据管理;数据处理;数据表示;地理学;元部件;通信系统;元数据;数据记录;信息处理;数据传送;拓扑学;地质学;大地构造学;数据处理系统;图表;定义;规范;地质信息;地球表面;地质信息管理;元文件;信息交流;地质的;信息;信息技术

In order to solve the important and basic problem of the petrogenesis of "Tiantangzhai migmatitic granite" in the core of Dabie orogenic belt, the detailed 1∶50000 regional geological surveying and the big scale dissection of important region (metamorphic rocks, granites and structure), were operated in about 900km〓 area near Tiantangzhai peak. On the bases of the petrology, mineral chemistry, geochemistry of rare earth element and microelement, isotope geochemistry and chronology, physicochemistry, magmatic dynamics, geodynamics, diagenetic simulation, and regional geophysical data, the theory of cooling age and historical geochemistry and the viewpoint of tectonic evolution are applied to study the petrogenesis of Yanshan epoch granites of this region. On the bases of above studies, the process of tectonomagmatic dynamics after indo-Chinese epoch in Dabie orogenic belt is discussed. The important conclusions are gotten

本文针对大别造山带核部&天堂寨混合花岗岩&成因这一重大基础地质问题,在天堂寨一带近900km〓的面积上进行了详细的1∶5万区域地质调查和大比例尺重点区解剖,通过对区内燕山期花岗岩进行岩石学、矿物化学、稀土微量元素地球化学、同位素地球化学和年代学、物理化学、岩浆动力学、地球动力学和成岩计算机模拟等研究的基础上,结合区域地球物理学资料,应用冷却年龄、历史地球化学理论和构造演化观,阐明区内燕山期花岗岩成因,并以此为基础进一步讨论了大别造山带自印支期以来的构造—岩浆动力学过程,取得了如下的重要认识

This site has been created by Mike Strickler, a geologist affiliated to the University of Oregon, USA. It features answers to many commonly asked questions in the areas of the physical Earth; minerals; rocks; internal processes; global tectonics; geological time; surface processes and astronomy.

该站点是由美国俄勒冈州大学地质学家Mike Strickler创建的,它回答了有关地球科学的一些常见问题,包括:地球物理学、矿物学、岩石学、地球内部构造、全球构造运动、地质年代、地表过程和天文学等。

In this dissertation, sedimentology, historical geology, structural geology, geophysics, structural dynamics/geometric, plate structure etc were combined properly. Taking Jiyang depression as studying object, fault distribution of different periods was analyzed, and thus discussing their structural dynamics. Using tectonic subsidence history modeling and denudating relationship between hanging wall and foot wall in Mesozoic faults, fault activity characteristics were discussed.

本论文将沉积学、地史学、构造地质学、地球物理、构造几何学和运动学、板块构造等多学科有机的结合,以济阳坳陷为研究对象,采用各时期断裂分期配套,分析了不同构造运动时期济阳坳陷断层展布,进行构造运动学讨论;利用构造沉降史模拟与中生代断层上下盘剥蚀关系的恢复,探讨了中生代断裂活动的特征。

After detail field inspecting, combined with the deep indoor research result, the author regarded that those deposits, which districted in West Kunlun Mountain Region , are belong to Mississippi Valley Type Lead-Zinc deposits.

本文运用区域成矿学理论从沉积建造、岩浆活动、构造演化以及区域地球物理场和地球化学场特征等方面系统地阐述了西昆仑地区(特别是奥依塔格—库尔良晚古生代裂陷盆地)的成矿地质条件。

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I didn't watch TV last night, because it .

昨晚我没有看电视,因为电视机坏了。

Since this year, in a lot of villages of Beijing, TV of elevator liquid crystal was removed.

今年以来,在北京的很多小区里,电梯液晶电视被撤了下来。

I'm running my simile to an extreme.

我比喻得过头了。