作者: Ruirui Wang , Zhiqin Xu , M. Santosh , Xianbing Xu , Qi Deng
DOI: 10.1016/J.JOG.2017.07.003
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摘要: Abstract The South Qinling Belt in Central China is an important window to investigate the Neoproterozoic tectono-magmatic processes along northern margin of Yangtze Block. Here we present whole-rock geochemistry, zircon U-Pb geochronology and Lu-Hf isotopes a suite Middle intrusion from Wudang Uplift Qinling. Zircon LA-ICP-MS ages reveal that these rocks were formed at ca. 705–716 Ma. Geochemical features indicate felsic magmatic are I-type granitoids, belong calcic- calc-alkaline series, display marked negative Nb, Ta Ti anomalies. Moreover, enrichment light rare earth elements (LREEs) large ion lithophile (LILEs), combined with depletion heavy (HREEs) support have affinity typical arc Andean-type active continental margins. REE patterns highly moderately fractionated, (La/Yb) N = 5.13–8.10 meta-granites, 2.32–2.35 granodiorite. granitoids wide range e Hf (t) values (−29.91 14.76) two-stage model (696–3482 Ma). We suggest Ma sourced different degrees magma mixing between partial melting overlying mantle wedge triggered by hydrous fluids released subducted materials crustal melting. hybrid magmas emplaced shallow crust accompanied assimilation fractional crystallization (AFC). Both isotopic geochemical data arc. These as well contemporary A-type granite may mark transitional tectonic regime rifting, probably related slab rollback during oceanic subduction beneath