地壳的

This tendency is well correlated to the geotectonic features and the structure of the crust and upper mantle, and approximately coincident to the features of other geophysical field in this region.

并提出该区尤其是郯庐带的某些地段可能有上地幔物质上涌，引起地壳深部产生很大的温度差异和密度差异，造成热应力的高度集中。

This is an A_1 type granitoid belt, slightly predominated by mantle components. Their source regions are probably mainly the lithospheric mantle and lower crust, which had been metasomatized and enriched so that they could bear OIB characters in trace elements.

这是一个以地幔物质略占优势的A1亚型花岗质杂岩带，其源区物质可能主要是经过交代和富集的具有OIB型微量元素特征的岩石圈地幔和下地壳。

Based on the previous geological work, a large number of granitoid samples are carried on the Sm-Nd isotopic analysis. The results show that the εNd values of these granitoids occurred in Beishan Mountain area range from-16. 39 to +10. 89, some of which are characterized by the positive εNd value. It suggests that the crustal growth existed during Phanozoic in Beishan Mountain area, just like other regions in the CAOB.

本文在以往工作基础上，通过大量的Nd同位素分析，发现北山地区花岗岩类的εNd值变化于-16.39～+7.85，不少花岗岩类具正εNd值，说明本区与中亚造山带上其他地区一样，在显生宙存在大规模的地壳生长。

We divide the evolution of becoming rocks into four periods: early region's metamorphic process and mixed lithifaction,sedimentation and becoming rocks process in middle and late Proterozonic Era and in the Paleozonic Era,trasformation process of burial hill layers in earth shell'uplift period in the Mesozonic Era, and transformation process to burial hill in the Cenozonic Era.

将储层的成岩演化划分为四个阶段：即早期区域变质作用和混合岩化作用、中晚元古代和古生代沉积成岩作用、中生代地壳抬升阶段潜山地层的改造作用和新生代断裂对潜山的改造作用。

Huge quantities of ground water deposited in the limestone flow from south to north and are blocked by the magmatic rocks.

由于在济南的地面下，存在着许多地壳裂痕，大量的地下水在压力的作用下流出地面。

The Daping mine is a ductile shear zone controlled mesothermal deposit, which was formed by rapid decompression and subsequent boiling and deposition.

结合其它证据，作者认为该矿的成矿流体主体为深源的壳幔混合流体，而不是地壳浅部的大气降水、岩浆水或其混合流体。

In terms of physical-chemical conditions of ore deposits and nano-theories and nano-effects, in connection with themodynamics discussion on Au migrational mode, this paper first time points out that Au is migrated chiefly in the form of nano-particle natural gold in ore-bearing fluid.

3根据金成矿的物理化学条件计算，引进纳米理论和纳米效应，联系Au迁移形式的热力学讨论，首次提出本区金矿成矿流体中Au主要以纳米微粒自然金形式迁移，但在地壳中的物理化学条件下可能部分呈金-硅配合物和金-硫配合物形式在一定范围内迁移

This paper discusses the detection of postglacial rebound by using data from space geodetic measurement of VLBI, and using measured site velocities and length rates of baselines to detect the vertical and horizontal postglacial rebound respectively.

本文利用甚长基线干涉测量技术提供的实测站速度和地球物理模型ICE_4G提供的数据，采用实测站速度法和基线长度变化率法分别检测了冰期后地壳回弹的垂直运动和水平运动。

The Taihu Lake is situated in the centre of the dish-like lowlying land south of the Changjiang River, which was resulted from the two dynamic factors, the long-term ground depression at a rate of 0.4 mm/a, calculated from the archaeological data, and the rise of the postglacial sea level that was responsible for the formation of the high coastal plain on the east margin of the dish-like low-lying land.

本文从沉积学、地层学、地貌学、考古学和历史地理学角度，综合分析了太湖的成因和演变。认为地壳沉降与海面上升是构成江南碟形洼地的内外动力，为太湖的形成奠定了基础。全新世海侵最盛时，太湖海湾水深潮急、泻湖、滨海沼泽围绕海湾分布。随南部湾口沙嘴封堵，海湾趋于消失，陆地扩大，遗址增多。3700a来，海面回升，湖面逐渐扩展，形成现代太湖。

Silicons are the most in the earth's crust, silicon oxidize the silicon form and exist by two more, is rich in two high-temperature karst which oxidize the silicon, under the function of the pressure, and soak trunks outside gradually inside, there is a crystallization course, it is the silication course.

地壳中硅是最多的，硅多以二氧化硅形式存在，富含二氧化硅的高温岩溶，在压力的作用下，从外及内逐渐浸润树干，并有个结晶过程，便是硅化过程。

The basic concept of FOP can be summarized as to further optimize effective prescription according to the standard of curative effects and with the aid of modern science and technology and theories of traditional Chinese medicine.

其基本内涵可概括为：以确有疗效的中药复方为研究对象，以现代科学技术和传统中医药理论为技术支持，以该复方所治病证的药效响应为评价标准，以优化重组疗效更优的新复方为研究目的。

Ever since our world has been a world, native forests have been indiscriminately exploited by man.

自从我们的世界一直是世界原生森林被任意剥削人。