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.
地球介质的黏度是地球动力学研究中的重要参数。
The viscous properties of Earth media are very important in geodynamics.
盆地热历史类型受其地球动力学背景及构造演化史控制。
The thermal history type of basin is controlled by its dynamic background of the earth and structural evolution.
固体地球动力学研究应向流体地球动力学进行概念转变。
We need to change the concept of solid geodynamics to liquid one.
一般都认为造山带和盆地形成于不同的地球动力学环境。
It has been generally considered that orogenic belts and basins are formed by different geodynamic mechanisms.
青藏高原的地球动力学研究是一个复杂而饶有兴趣的问题。
The geodynamics of the plateau is one of the most interesting problems for the earth scientists.
板块俯冲碰撞理论曾是花岗岩构造动力学、地球动力学研究的主线。
Subduction and collision theory of Plate tectonics is a basement of the study of granite tectonic dyna mics and geodynamics.
论述了一个旨在统一板块构造学说和地幔柱学说的地球动力学理论。
In this paper, the author advocates a new dynamical theory of the Earth, attempting to unify plate tectonics and plume theories.
岩石热破裂在工程上应用广泛，并且是地球动力学基础研究对象之一。
Rock thermal fracturing has great application prospect and is one of the basic research objects of geodynamics.
文章扼要阐述了幔源铀成矿的地球动力学背景，评述了热点铀成矿理论。
The geodynamic regime of mantle-derived uranium metallogenesis and theory of hotspot uranium metallogenesis are briefly discussed.
刚体地球章动序列和非刚体地球章动的转换函数都和地球动力学扁率有关。
A rigid Earth nutation series and a non rigid Earth transfer function both are associated with the Earth dynamical flattening.
未来流水下切研究要在流水动力学和地球动力学两方面探索更多的科学问题。
The research of fluvial incision in the future will explore more scientific problems concerning both fluvial dynamics and geodynamics.
本文论述了上地幔各向异性的参数描述和主要证据，以及与地球动力学的关系。
The elastic parameters, their main evidences and relevance to the earth's dynamics of the anisotropy of the upper mantle are discussed in this paper.
分析了中国大陆东部地区和东海海域地球物理场、大地构造、地球动力学特征。
This paper analysed characters of geophysical fields, tectonics and geodynamics of eastern of Chinese continent and east China Sea region.
近年来，应用地球动力学研究镁铁质-超镁铁质岩石演化取得了一些重要进展。
Recently, several important progresses have been made in the geodynamics concerning the evolution of mafic and ultramafic rocks.
结果表明，地震活动时空分布的多重分形特征与不同地球动力学环境关系密切。
The results show that the multifractal characteristics of GSRE are closely related to the geodynamic environment.
探讨了地球动力学扁率值对刚体地球章动振幅和非刚体地球章动转换函数的影响。
In this paper, the effects of the value of the Earth dynamical flattening on rigid Earth nutation amplitudes and the transfer function of non-rigid Earth nutation are discussed.
双高压变质带的确立对解决华北-扬子板块边界地球动力学演化问题具有重要意义。
The establishment of the paired high-pressure belts is of major significance for solving the problem of the geodynamic evolution of the boundary of the North China and Yangtze plates.
表明，在研究许多地球动力学问题时，扣除海水密度变化引起的海面高变化至关重要。
The result shows that it is more important to separate sea level height variation caused by seawater density change in the study of Earth dynamic problem.
本文系统地介绍了GPS应用于精密测地和天文地球动力学的基本模式、原理和误差。
In this paper, the basic models, principle and error sources of GPS applied to precise geodesy and astro-geodynamics are introduced systematically.
也就是说，燕山运动是东亚构造体制转变的产物，其出现有着深刻的地球动力学背景。
That is, the Yanshan Movement is the result of the conversion of tectonic regimes in East Asia, which has profound global geodynamic Settings.
就旋转的地球模型和不运动的地球的模型而言，其地球动力学规律存在着本质的区别。
The laws of geodynamics differ essentially from the models of the unmovable or rotating Earth.
这些结果将为地球动力学研究提供新的定量资料，对于震源层析成像研究等有实际意义。
These results will give new quantitative data for geodynamics and has practical meaning for seismic source tomography research.
在地质历史上，适于前陆盆地发育的地球动力学环境，在时间和空间上均是相当有限的。
The geodynamic environment in which foreland basin is developed is rather limited both temporally and spatially in the geological history.
对这三种地球动力学效应的研究将有助于从另一角度了解地球内部的结构及其运动形态。
It's favorable to find out the earth's internal structure and the earth's movement from the study of these effects.
地震学、地球动力学研究倾向于全地幔对流模型；地球化学研究则支持分层地幔对流。
Seismological and geodynamical evidences supported whole mantle convection model, while geochemical ones supported layered convection model.
这些海潮模型的相互比较为研究海洋的精细结构、海潮的动力学、地球动力学提供了依据。
The comparison of the different ocean tide models should provide a base to the study of ocean structure, ocean tide dynamics and geodynamics.
这些初步成果说明同位素填图与化学地球动力学在造山带研究中是具有重要前景的技术途径。
Theseachievements indicate that isotopic mapping and chemical geodynamics are significant and perspective approaches to researches on orogenic belts.
通过比较，可以看出，海水质量变化可以部分解释1998年以来地球动力学扁率的异常变化。
The result suggests that the oceanic mass redistribution can partly explain the abnormal variation of the Earth's oblateness from 1998.
虽然大多数结果提供了地球动力学的背景，但就其分辨率而言还不足于进行有效的大陆动力学研究。
Though most results present the background of geodynamics, their resolutions are not enough for the effective study of the continental geodynamics.
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