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《Geological Science and Technology Information》 2003-03
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ADVANCES IN STUDY ON THE INTERACTION BETWEEN MAFIC AND FELSIC MAGMAS IN OROGENIC SUITES

MA Changqian(Faculty of Earth Sciences, China University of Geosciences, Wuhan Hubei 430074, China)  
Progress made thanks to the great number of the geochemical and magmadynamical studies over the last twenty years has allowed important insights into interaction between mafic and felsic melts, subject of Eurogranites 2002 held on September 1421,2002 in central Italy. The present review addresses the interaction relationship between mafic and felsic magmas, and the role of mafic melts in generation of voluminous granitic magmas, combining with the discussion of prefield meeting workshop, and field excursion of Eurogranites 2002. In granitoid batholiths,there are not only granites sensu stricto, but also many mafic rocks (e.g., gabbro and diorite). In general, the mafic rocks may be mantlederived parental magmas, end members in magma mixing and fractionationassimilation processes, material from lower crustal source regions, and/or heat sources that drive partial melting of the overlying continental crust. Such study of the relationship between mafic and felsic magmas can provide valuable constraints on the relative role of crustal recycling and new mantle additions to the continental crust during orogenic processes.
【Fund】: 国家自然科学基金资助项目(49972022);; 高等学校博士点基金资助项目(20010491018);; 中国地质调查局项目"中国花岗岩重大地质问题研究"(200113900018)
【CateGory Index】: P588.14
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