Early Cretaceous high-Mg diorites in the Yanji area, northeastern China: Petrogenesis and tectonic implications

Abstract

Mesozoic granitic rocks are widely distributed in northeast (NE) China. However, high-Mg dioritic rocks are considerably rare. Here, we report a newly recognized high-Mg diorite (the Xintun diorite) in the Yanji area, NE China, to constrain its origin and implications for the tectonic evolution of eastern Asian continental margin. Zircon U–Pb dating yields a crystallization age of 128±1Ma for the Xintun diorite. The diorites are characterized by high MgO (4.4–6.6wt.%), Cr (119–239ppm), Ba (419–514ppm) and Sr (649–747ppm) contents and Mg# values (59–64), but low FeOtotal/MgO ratios (1.2–1.4), with geochemical features similar to those of sanukitic high-Mg andesites (HMAs). They show moderate radiogenic Sr (ISr=0.7047–0.7050) and Nd (εNd=0.3–1.1), with high La/Sm ratios, which are indicative of contributions from sediment components. The mineral assemblage of euhedral hornblende, magnetite and titanite, implies a water-rich and oxidized signature for their primitive magmas. These features suggest that the Xintun high-Mg diorites were probably formed via partial melting of the subducting sediments and subsequent interaction of mantle peridotites with both melts and aqueous fluids. Geochemical modeling reveals that hornblende-dominated fractional crystallization under water-sufficient conditions enabled the evolved magmas to acquire adakitic signatures. We believe that the Paleo-Pacific subduction beneath eastern Asian continental margin caused large-scale back-arc extension of NE China in the Early Cretaceous, and, consequently, induced the asthenospheric flow toward the mantle wedge, reheating subducting sediments enough to cause melting. Therefore, the occurrence of the Xintun high-Mg diorites signifies the onset of extensive back-arc extension of eastern Asian continental margin at ca. 128Ma.