To earth ' s hidden chambers pierced i by my wisdom , deep through the earth ' s crust , into the pathway , hidden for ages from the children of men 进入地球靠我的智慧连通隐藏的房间，通过地壳的深处，进入道路，为人类孩子年代隐藏起来的道路。
Lord oxburgh is especially interested in the thermal behaviour of the earths crust , and recently he has turned his attention to climate change , energy and water futures and global development 勋爵对地壳的热能变化尤其感到兴趣，近来更进而研究气候变化能源和水的未来及全球发展。
Such features might result from the rotation movement of the earth crust and exert serious impact on the geotectonic evolution and large scale metallogeny in hunan province and adjacent regions 这种特征可能是地壳的旋转运动所造成，它对湖南及邻区大地构造的演化、大规模成矿作用等具有重大的影响。
Together with the localization of seismicity on faults , this leads to the conclusion that a fraction of the crust is susceptible to rupture , while presently being quiescient 与断层的局部地震活动性一起考虑，可以得出如下结论地壳的一部分，在目前处于静止状态条件，它实际处于一种易受影响导致破裂的敏感状态。
These studies , therefore , suggest that the songsugou peridotite is not a tectonic massif of the upper mantle but a ultramafic magmatic rock body crystallized in deep crust and tectonically emplaced in the upper crust 从而证明了松树沟橄榄岩体并不是上地幔岩石的残片，而是由岩浆在深部地壳环境下结晶而成并以固态构造侵位于地壳的上部。
The tectonic deformation of the plateau , in which fault belts were included , was simulated at the later stage . at the same time , the occurrence , evolution and formation principles of the plateau were all researched 最后，对包含断裂带的高原地壳的构造变形进行了动态仿真，并初步探讨了高原构造应力场的成因、高原的演化及形成机制等问题。
Studies on the metamorphic history of the granulites on a very old platform provide us some important information of the properties , status and forming processes of the lower crust and forming mechanism of the early continent crust 古老地台麻粒岩的变质历史研究可以为我们深入了解下地壳性质，状态及形成过程，探讨早期大陆地壳的形成机制提供重要的信息。
The uplifting is differential according to the stage with crust shortening and thickening and material east - flowing . for this deformation dynamic mechanisms there have been several opinions because of the shortage of information 这种隆升是以分阶段差异隆升为特点，并且伴随有地壳的缩短变厚以及物质东流，但对高原这种形变的动力机制解释历来却有许多观点，其主要原因是研究资料的不足。
Then , media parameters of the crust , boundary function forces of the area and the finite elementary analyses model were reversibly simulated . linking up with the plateau crustal deformation back analyses model , the tectonic deformation was also simulated 该模型属于动力学的物理模型，包含反演地壳的介质参数、反演研究区域的边界作用力与正分析三大部分组成，并以此模型为基础仿真模拟了高原的构造变形。
The characters of velocity ' s distribution within the mid - layer of the middle crust resemble that of the upper crust ' s bottom layer , and the velocity strongly disturbed . the prominent higher velocity anomalies exist below the linbi uplift and the hu - su uplift within this layer 中地壳的中间层速度分的基本特征类似上地壳底部，横向均匀性显著；中地壳下部速横向不均匀性明显，在灵壁隆起和湖苏隆起的下部有显著的高速异常。
