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《Geochimica》 2005-05
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Formation time and magma source of granites in Bengbu uplift: Evidence from LA-ICPMS zircon U-Pb dating and tracing

YANG De-bin1, XU Wen-liang1, PEI Fu-ping1, WANG Qing-hai1, LIU Xiao-ming2 1. College of Earth Sciences, Jilin University, Changchun 130061, China; 2. Key Laboratory of Continental Dynamics, Ministry of Education, Northwest Un iversity, Xi,an 710069, China  
The granites in the Bengbu uplift were dated using LA-ICPMS zirco n U-Pb method to determine their formation time and to trace their magma sources. The results show that the weighted mean 206Pb/238U ages of magmatic zircons fro m the Xilushan and Nüshan granites in the Bengbu uplift are (129.3±4.8) Ma (n= 7) and (130.1±3.2) Ma (n=9), respectively, which indicates that these granites were formed in the beginning of Early Cretaceous. The weighted mean 206Pb/238U a ges of magmatic zircons from the Caoshan monzonitic granite and the Mayishan gra nite are (110.3±2.8) Ma (n=17) and (115.8±3.1) Ma (n=18), respectively, which indicates that they were formed in late period of Early Cretaceous. The petrogra phic characteristics of these granitic intrusives and the occurrence of magmatic zircons with fine-scale oscillatory zoning rims indicate that they were formed by normal crystallization of felsic melts rather than by migmatization. The coe xistence of the Neoproterozoic magmatic inherited zircons, the Indosinian metamo rphic inherited zircons, and the Archean and Paleoproterozoic inherited zircons in the Xilushan and Nüshan granites implies that the magma sources could be inv olved in both the basements of the Yangtze Block (YB) and the North China Block (NCB). And some of them were superimposed by the ultrahigh pressure metamorphism . The occurrence of the YB basement in the lower continental crust of the NCB co uld be resulted from the NWW (or near EW) directed subduction of the YB beneath the NCB along the Tan-Lu fault zone.
【Fund】: 国家自然科学基金(40472033 40133020);; 西北大学大陆动力学教育部重点实验室开放基金~~
【CateGory Index】: P588.121;P597.3
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