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《Geochimica》 1998-06
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Chen Guoneng (Department of Earth Sciences, Zhongshan University, Guangzhou 510275)  
The In-situ,Melting hypothesis relevant to the genesis of granite has revealed the concentration and dispersion trends of the various chemical elements in the endogenic process. The concept of Geochemical Field of the Elements is derived from the point mentioned above and the locations of the elements in the periodic table. Geochemical Field of the Elements, which not only sums up the concentration-dispersion trend of elements in the in-situ melting process, but also unravels the relation between their configuration and distribution in place, exhibits three cross sections, namely the cross section of a granite body and its exocontact zone, of the continental crust and of the globe. Besides, Geochemical Field of the Elements also displays the cyclic process of continental material, and clearly shows that melting within the crust is a key link in the formation and evolution of the continental crust.
【Fund】: 高等学校博士点专项科研基金;;国家教委重点基金
【CateGory Index】: P595
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