摘要
Flow units are the most elementary constituents of basaltic lava strata, and the zonation of pores and fractures determines the capability and distribution of basaltic reservoirs. Both outcrop and borehole information are used to build the geologic model of basaltic lava flow units, indicating that each unit is composed of three parts such as the upper vesicular zone, the central massive zone and the lower vesicular zone from top to bottom. Three electro-facies including alteration zone, vesicular zone and massive zone were identified by combining the natural gamma log (GR), acoustic log (DT), density log (RHOB), electrical resistivity (LLD) and neutron log (NPHI). Natural gamma-ray spectral logging (K, Th and U) were also utilized to distinguish intervals with abnormal high gamma values.