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《Advance in Earth Sciences》 2004-05
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THE MORPHOLOGY OF MELT (AND FLUID) IN INTERGRANULAR PORES OF ROCK UNDER HIGH-TEMPERATURE AND HIGH-PRESSURE AND SOME DEVELOPMENT OF EXPERAMENTAL STUDIES OF THIS BRANCH

HOU Wei, ZHOU Wen-ge, XIE Hong-sen ,LIU Yong-gang (Institute of Geochemistry, Chinese Academy of Sciences,Guiyang 550002,China)  
The morphology of melt (and fluid) in intergranular pores of rock under high-temperature and high-pressure is one of forward branches in modern petrology. In this branch, the morphological features of melt (and fluid) in intergranular pores of rock, interconnectivity, and the relation between melt (or fluid) and mineral crystals around them under high-temperature and high-pressure are studied. Some observational methods of materials science are used in the study of this brach. The interfacial energy theory of physical chemistry is theoretical basis of this branch. The studies of morphology of melt (and fluid) in intergranular pores of mantle rock under high-temperature and high-pressure are very important for partial melting of mantle, asthenosphere, and metasomatism of mantle. In this paper, the theoretical basis, experimental method, and some results of this branch are reviewed.
【Fund】: 国家自然科学基金重大项目"地球内部几个重要界面物质的高温高压物性研究"(编号:10299040);; 中国科学院知识创新工程重要方向项目"同步辐射高压高温实验技术及地幔地核重要矿物的物性研究"(编号:KJCX2 SW No.3)资助
【CateGory Index】: P584
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