The 127 Ma gold mineralization in the Wulong deposit, Liaodong Peninsula, China: Constraints from molybdenite Re-Os, monazite U-Th-Pb, and zircon U-Pb geochronology

•The geochronological framework of the Wulong orefield has been reconstructed.•Zircon U-Pb geochronology delineates the two main magmatic events in the Wulong orefield.•Molybdenite Re-Os and monazite U-Th-Pb geochronology record the Wulong gold mineralization occurred at 127 Ma.•The Wulong gold mineralization is contemporaneous with the Early Cretaceous magmatism, related to lithospheric thinning under the northeastern North China Craton.