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《Geology in China》 2015-01
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The emplacement epoch, petrogenesis and geological significance of Gabuzha granodiorite at the southern edge of Qiangtang, Tibet

QIN Chuan;LI Zhi-wu;ZHU Li-dong;ZHANG Yu-xiu;YANG Wen-guang;HUANG Rui;Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology;Key Laboratory of Computational Geodynamics, CAS;College of Earth Science,University of Chinese Academy of Sciences;  
The Gabuzha granodiorite in Gerze area intruded into the Jurassic Sewa Formation at the southern edge of the southern Qiangtang terrane, and can be used to constrain the evolution of Bangong Co-Nujiang River suture zone. LA-ICP MS zircon U-Pb dating yielded a weighted mean age of(143.8 ± 0.5) Ma, suggesting that the Gabuzha granodiorite formed during late Jurassic to early Cretaceous. The Gabuzha granodiorite is metaluminous I- type granite and belongs to high- K calc- alkaline series. Its REE model is characterized by enrichment of light REE, and Eu shows weak negative anomaly. Large ion lithophile elements are obviously enriched in Rb, Ba, K, Th and U. High field strength elements Nb, Ta, P and Ti show strong depletion. The results show that the magma source of Gabuzha granodiorite might have been derived from mixture of continental crust materials, subducting sediments and mantle- derived wedge, and experienced a certain degree of separation and crystallization as well. The Gabuzha granodiorite formed in an island arc environment related to northward subduction of the Bangong Co-Nujiang River Meso-Tethys Ocean beneath the Qiangtang terrane.
【Fund】: 中国地质调查项目(1212011086065);; 国家自然科学基金项目(40802048 41472209 41002055);; 高等学校博士学科点专项科研基金(20125122110010)联合资助
【CateGory Index】: P588.121;P597.3
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