摘要
There are abundant mafic dykes that intruded the Mesoproterozoic Ebian Group in Jinkouhe area of western Sichuan Province. Their precise emplacement time is significant for revising the time of the Ebian Group and studying the Precambrian tectonic setting of the western margin of Yangtze Craton. One of the diabase dykes from Jiadanqiao Formation of Ebian Group was dated by SHRIMP zircon U-Pb dating. The result shows that the zircons are of typical mafic magmatic origin with clear and wide internal growth zoning and high Th/U ratios, and the weighted mean 206Pb/238U age is(813.4±8.2) Ma (MSWD=0.56). This result represents the emplacement time of the diabase dykes, and also constrains the minimum age of Jiadanqiao Formation in Ebian Group.