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《Geochimica》 2006-01
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Geochemistry of aluminous A-type granites along Darabut tectonic belt in West Junggar, Xinjiang

SU Yu-ping1,2, TANG Hong-feng1, HOU Guang-shun1,2 and LIU Cong-qiang11. Laboratory for Study of the Earth's Interior and Geofluids, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China; 2. Graduate School of Chinese Academy of Sciences, Beijing 100049, China  
There are several batholiths mainly composed of alkali feldspar granites, including Miaoergou, Akebasitao, Karamay, and Hongshan plutons, outcropped along Darabut tectonic belt in West Junggar, Xinjiang. The results of studies on petrology and elemental geochemistry show that all these alkali feldspar granites are typically aluminous A-type granites, which are characterized by high 100 00×Ga/Al ratios. From the results of zircon U-Pb dating by LA-ICPMS, they were emplaced at about 300 Ma, being contemporary with alkaline granites in East Junggar. The alkali feldspar granites studied belong to A2 on petrogenetic type, and should be formed in a post-collisional tensional environment. εNd(t) values of these granites are high, ranging from +6.42 to +7.46, but many geological and geochemical characteristics demonstrate that these rocks were not directly derived from a depleted mantle, but most likely formed by fractional crystallization of granodioritic magmas which were produced by partial melting of a juvenile crust which mainly consists of oceanic crust and arc complex.
【Fund】: 中国科学院西部之光项目(2002年度);; 国家重点基础研究发展计划项目(2001CB409805)
【CateGory Index】: P588.121;P597.3
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