Cretaceous A-type volcanic–intrusive rocks and simultaneous mafic rocks along the Gan-Hang Tectonic Belt, Southeast China: petrogenesis and implications for the transition of crust–mantle interaction

Jurassic and Cretaceous (Yanshannian) tectonics, magmatism and metallogenesis in South China: preface

“…Mid-Late Cretaceous igneous activity on Hainan Island suggests that subduction of the E-W trend Neo-Tethys plate was the main cause (Sun et al 2018). Cretaceous A-type volcanic-intrusive rocks and contemporaneous mafic rocks along the Gan-Hang Tectonic Belt have been studied to illustrate their petrogenesis and implications for crust-mantle interactions (Wang et al 2018b).…”