SHRIMP Age and Geochemistry of the Bikou Volcanic Terrane: Implications for Neoproterozoic Tectonics on the Northern Margin of the Yangtze Craton

Abstract

Abstract The Bikou volcanic terrane is predominated by subalkaline tholeiitic lavas. Rock samples display lower initial ratios of Sr and Nd, 0.701248–0.704413 and 0.511080–0.512341 respectively. 207 Pb and 208 Pb are significantly enriched in the lavas. Most samples have positive ε Nd , which indicates that the magma was derived from EM‐type mantle source, while a few samples with negative ε Nd indicate that there was contamination in the magma evolution. Magma differentiation is demonstrated by variations of LREE and LILE from depletion to enrichment. Additionally, normalized REE patterns and trace elements showed that lavas from the Bikou volcanic terrane have similar characteristics to those of basalts in arc settings caused by subduction and collision. Analyses showed that the Bikou volcanic terrane is a volcanic arc. New evidence proved that the Hengdan Group, north of the Bikou arc, is a turbidite terrane filling a forearc basin. Consequently, the Bikou volcanic terrane and the Hengdan turbidite terrane construct an arc‐basin system. New SHRIMP ages showed that this arc‐basin system developed on the northern margin of the Yangtze craton in the Neoproterozoic (846–776 Ma), and this arc‐basin system is in agreement with the tectonic processes of Rodinia in the Neoproterzoic.