Some Aspects of Crystal Growth of Minerals

机译：矿物晶体生长的某些方面

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Minerals, as natural crystals, are major constituents of the Earth. Present day geophysical models accept a crystalline state of the earth-forming condensed matter everywhere except in the outermost envelope of the Fe-rich nucleus of our planet. If rocks of the continental crust are known for long to be mostly crystalline, those from the oceanic crust are also now known to be so from submarine exploration and deep-sea drilling projects. As a whole the earth's crust, dominated by silicate minerals, exhibits a rigid behaviour down to the Moho discontinuity (some 8-10 km under sea floor, some 30 to 70 km under the continents).

机译：矿物质，作为天然晶体，是地球的主要成分。当今的地球物理模型在除地球富铁原子核最外层之外的任何地方都接受地球形成的凝结物质的结晶状态。如果长期以来人们都知道大陆壳的岩石大部分是晶体，那么现在从海底勘探和深海钻探项目中也知道来自海洋壳的岩石。总体而言，以硅酸盐矿物为主的地壳在莫霍面不连续性（海床以下约8-10公里，大陆下约30至70公里）下表现出刚性行为。

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来源
《Theoretical and technological aspects of crystal growth》|1998年|269-290|共22页
会议地点 Rimini(IT);Rimini(IT)
作者
A. Baronnet;
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作者单位

CRMC2-CNRS, Campus Luminy, Case 913, F-13288-Marseilles Cedex 9, France;

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会议组织
原文格式 PDF
正文语种 eng
中图分类晶体生长;
关键词
minerals; crystal growth; mechanisms; electron microscopy;

机译：矿物质晶体生长机制；电子显微镜;

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Some Aspects of Crystal Growth of Minerals

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