摘要
Studying the Mesozoic volcanic rocks widely exposed in Lhasa block can better understand the geological evolution of the Tethys and construction of the whole Tibet Plateau. In present study, major, trace element compositions and isotopic results of Qushenla Formation in north Lhasa block have been reported. The volcanic rocks from Qushenla Formation mainly consist of medium-K calc-alkaline series, including basalt, basalt-andesite and andesite. In the spider diagram, they show the character of enrichment of LILE (Rb, Ba, Th, U) and depletion of HFSE (Nb, Ta, Ti), similar to those of an island arc volcanic rock.