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《ACTA SCICENTIARUM NATURALUM UNIVERSITIS PEKINESIS》 1994-02
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Isotope and REE Geochemical Characteristics of CrustEvolntion in the Paleozoic Orogenic Belt ofBeishan Region, Gansn Province

MU Zhiguo, LIU Chi, HUANC Baoling, HOU Guiting,(Departinent ol Ceology, Peking University)ZUO Cuochao, LIU Chunyan, FENG Yongzhong(Cansu Bureau of Ceology & Mineral and Resources)  
O, Sr, Nd and Pb isotope composition and ratio of the rocks collected from 12intrusive massesof Beishan region in Gansu province have been determined. Their agesare from Pro-Caledonian to indoChina period. In addition, REE content of 40 igneousrocks including above 12 intrusive masses were analyzed. The isotopic variability issystematic resulted from each isotope variation of different tectonic period with lessmature getting more and more mature as well as with from lower mature to highermature of crust. If we thought that it was normal evolution of isotope with getting upof crust maturity, then it would appear reverse isotope evolution while the crust matu-rity was getting down, and 'random' or 'diverse' isotope evolution would occur whilethe superlative maturity of crust was coming also. The two tectonics units, belong tothe Tarim plate and to Kazakhstan Plate, respectively, have different characteristics ofisotope variation. They have similar different characteristics of REE distribution also.
【Fund】: 国家自然科学基金
【CateGory Index】: P597
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