地壳变动

构造地震和地壳变动型海啸之间不是因果关系，而是伴生或共生关系。

The tectonic earthquake-faulting tsunami relation is not causality , but juxtaposition .

太平洋月平均水位周期变化和线性升降趋势地壳变动海面升降运动

Periodic variation and linear rise trend of monthly mean value of sea-level in Pacific Ocean

地壳变动海面升降运动第四纪海面升降运动湖面的升降和物源的摆动使辫状三角洲沉积体系中发育夹层。

Eustatic lake level and source change had resulted in intercalation development in braided delta system .

排氢脉冲导致洋壳扩张的增强，而此则与创造出造山带的地壳变动幕相关。

Degassing impulses give rise to the strengthening of oceanic crust spreading which is correlated with phases of diastrophism creating folded orogenic belts .

这些为认识用大地测量方法定量研究现代地壳变动的客观性提供了理论基础。

So the theoretical bases for objective recognizing the recent crustal movements by using the quantitative research of geodetic method are supplied by means of this study .

闽西南&粤东北地区大地构造演化与铜、（伴生）银的成矿作用构造地震和地壳变动型海啸之间不是因果关系，而是伴生或共生关系。

GEOTECTONIC EVOLUTION AND Cu - ( ASSOCIATED ) Ag METALLOGENESIS IN SOUTHWEST FUJIAN AND NORTHEAST GUANGDONG The tectonic earthquake-faulting tsunami relation is not causality , but juxtaposition .

天山山脉形成于古生代晚期古洋盆关闭以后，现今山脉的地貌特征则是新生代晚期地壳变动的产物。

The Tianshan Mountains formed after the closing of the Late Paleozoic oceanic basin and the geomorphological features of the present mountains are the production of Late Cenozoic crustal movement .

地球模拟器是由日本宇宙开发事业团、日本原子能研究所以及海洋科学技术中心共同开发的矢量型超级计算机，用于预测及解析整个地球的大气环流预测、全球变暖预测、地壳变动等。

Earth simulator is a parallel vector super-computer which developed by National Space Development Agency of Japan ( NASDA ) and Japan Atomic Energy Research Institute ( JAERI ) and Japan Agency for Marine-Earth Science and Technology ( JAMSTEC ) .

地震：由于地质断层积聚的压力被释放或由于火山活动引起的地壳的突然变动。

Earthquake : a sudden movement of the earth 's crust caused by the release of stress accumulated along geologic faults or by volcanic activity .

它是地壳从活动阶段向稳定阶段过渡的地壳变动。

Xingcheng movement is a tectonization in the transitional time from the active stage of the earth 's crust to the stable stage .

华北中地壳滑脱面及其活动分区的天然地震研究地壳变动海面升降运动

A Seismic Study on the Detachment Layer in Middle Crust and Its Relation to Subdivision of Active Tectonics in North China