摘要
Ar-Ar dating for whole rock from the Qinglongtai diabase returns a plateau age of 35.5±1.7 Ma, which is in good accordance with their isochronal age within the uncertainty. It shows that the diabase has intruded in the Paleogene Shahejie period.Geo-chemically, these diabases have low SiO2, high Na2O+K2O and TiO2 contents, with intensive differentiation between light REE and height REE, slight Eu positive anomaly, and generally enrich in large iron lithophile elements (LILE, such as Sr and Ba) and high field strength elements (HFSE, such Nb and Ta), and can be comparable to those typical ocean island basalts (OIB).