摘要
Granitoid rocks are widely distributed in Motianling Area and Yanbaoshan Area in northern Guangxi.According to rock geochemistry,these granitoid rocks are characterized by relatively enriched in Si、K and poor in Na、Ca、Ba、Sr、Eu,and have higher LREE.These rocks belong to alkaline——calcium-alkaline granites,and have high fractional crystallization.Based on the analysis of their petrogenesis,it is concluded that the granitoid rocks are formed at the collision between the Cathaysia block and the Yangtze block or between the Yangtze block and a certain island arc block,and are postorogenic granites.