Identification of metasomatic components in lithospheric mantle under multiple tectonic regimes: Insights from Early Cretaceous mafic rocks in the northeastern North China Craton

Identification of mantle metasomatic components under multiple tectonic regimes is crucial for reconstructing the subduction history of multiple plates. Representative Early Cretaceous (125–122 Ma) gabbroic diabase from the northeastern North China Craton (NCC), provides a geochemical record to explore the genetic relationship between mantle metasomatic agents and tectonic evolution. Samples from gabbroic diabase exhibit low SiO2 and high MgO contents as well as arc-like trace element patterns, suggesting a sub-continental lithospheric mantle (SCLM) origin. Their inherited zircons and isotope variations indicate the existence of two crustal components with different tectonic affinities that were recycled into the SCLM: Paleo-Asian oceanic crust and Yangtze Craton continental crust. The metasomatic signatures of the two crustal components are previously imprinted on the geochemical compositions of the studied mafic rocks. Subsequently, the melting of the metasomatic SCLM is triggered by the subduction of the Paleo-Pacific Plate. Based on the identification of mantle metasomatic components in this study and previous geological evidence, the spatial extents of the subduction influence of the Paleo-Asian oceanic plate and Yangtze Craton on the SCLM beneath the northeastern NCC are broader than previously considered. These new findings signify a critical role of the mantle metasomatic components that can effectively identify the geological relics of the previous plate subduction. Thus we believe that the former mantle metasomatism and latter mantle melting for mafic rocks suggest two geological implications.