Petrogenesis of Early Cretaceous mafic dikes in southeastern Jiaolai basin, Jiaodong Peninsula, China

Mafic dikes of mainly Early Cretaceous age (130-110 Ma) are widely developed on the Jiaodong Peninsula, China. Previous studies of the dikes, which have focused mainly on occurrences in the Jiaobei uplift and in the Sulu orogenic belt, have thoroughly examined their petrogenesis and geodynamic setting. This study identified four previously unknown mafic dikes (dolerite and lamprophyre) in southeastern Jiaolai basin (near Haiyang city), Jiaodong Peninsula. Detailed geochemical and geochronological analyses were conducted to determine the petrogenesis of the dikes and to infer their geodynamic setting. Zircon U-Pb dating by laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) indicates that the dikes were emplaced at similar to 126 Ma. The dikes are characterized by low SiO2 contents (44.3-52.3 wt.%), high contents of MgO (7.28-10.13 wt.%), Cr (267-652 ppm), and Ni (93-335 ppm), and high Mg-# values (63-73); they are enriched in large ion lithophile elements (LILEs; Ba, K, and Sr), depleted in high field strength elements (HFSEs; Nb, Ta, P, and Ti), and are characterized by high (Sr-87/Sr-86)(i) isotope ratios (0.707226-0.708222), low epsilon(Nd)(t) values (-12.3 to -13.6), and zircon epsilon(Hf)(t) values (-15.6 to -23.6). These features suggest that the dikes were derived from enriched subcontinent lithospheric mantle (SCLM). The wide range of Rb/Sr (0.04-0.18) and Ba/Rb (5-34) ratios, and the low and limited range of Dy/Yb (1.93-2.52) and K/Yb (5.71-11.99) ratios of the dikes indicate that the magmas originated from a low degree of partial melting of an amphibole-and phlogopitebearing lherzolite in the spinel-garnet transition zone. The parental magma might have experienced fractionation of olivine and clinopyroxene during its ascent without significant crustal contamination. Evident depletion of Nb-Ta and Zr-Hf, low and limited range of Th/Yb ratios, elevated Ba/La ratios, constant chondritic Zr/Hf ratios, and a large range of Hf/Sm ratios further indicate that the mantle sources of the dikes were altered by carbonate-related metasomatism from subducted slab-derived fluids, which were most likely related to subduction of the Palaeo-Pacific plate during the Mesozoic. The mafic dikes in the southeastern Jiaolai basin resemble the arc-like mafic dikes in the Jiaobei terrain and the Sulu orogenic belt, and possibly indicate lithospheric thinning induced by slab rollback of the Palaeo-Pacific plate.