ObjectivernThe formation ages of global magmatic sulfide Ni-Cu deposits are from Archean to Mesozoic,the Neoarchean and Neoproterozoic are the two peaks.In Chin
ObjectivernLate Paleozoic supra-subduction zone (SSZ)-type ophiolites and intra-oceanic arc igneous petrotectonic assemblages are developed in the Erenhot—Hege
ObjectivernDiabase sills with baddeleyite/zircon U-Pb ages of ~1.32 Ga have been found in many areas of the North China Craton (NCC) (Peng,2015).Some researchers