Middle Neoproterozoic (ca. 705–716 Ma) arc to rift transitional magmatism in the northern margin of the Yangtze Block: Constraints from geochemistry, zircon U–Pb geochronology and Hf isotopes

• Published in: Journal of geodynamics Vol. 109; pp. 59 - 74
• Main Authors: Wang, Ruirui, Xu, Zhiqin, Santosh, M., Xu, Xianbing, Deng, Qi, Fu, Xuehai
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.09.2017
• Subjects: Geochemistry and tectonic setting; Neoproterozoic; Slab rollback; South Qinling; Tectonic transition; Zircon geochronology and Lu-Hf isotopes; Zircon geochronology and Lu-Hf isotopes; Tectonic transition; Geochemistry and tectonic setting; Slab rollback; South Qinling; Neoproterozoic
• ISSN: 0264-3707
• DOI: 10.1016/j.jog.2017.07.003

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