The oceanic island volcanic rocks in the Chiang Mai zone, northern Thailand, were usually covered by Lower Carboniferous and Upper Permian shallow-water carbonate rocks, with the Hawaii rocks and potash trachybasalt being the main rock types. Alkaline series was dominant with sub-alkaline series occurring in few cases. Geochemical characteristics of the rocks were described as follows: the major chemical compositions were characterized by high TiO2, P2O5, and medium K2O. Rare-earth elements were characterized by right-inclined strong LREE-enrichment patterns and the trace element patterns were of the upward-bulging K-Ti enrichment type.