Tempo-Spatial Features Of The Tarim Lip

The study of the tempo -spatial features of the Tarim Large Igneous Province (Tarim LIP) can provide some good evidence of the limits of one of the world's Large Igneous Provinces (LIPs). The results of some recent research on the tempo -spatial features of the Tarim LIP will be addressed in this study. Through the systematical and detailed study of the spatial distribution and the precise dating and contact relationships between the main rock units in the Tarim LIP and the host rocks, the distribution of the Tarim LIP reaches over 2.5x 105 km2, which is a Permian LIP in NW China. The temporal order of the Tarim LIP can be considered continental flood basaltic lavas in the Kupukuziman and Kaipaizileike formations (292-285 Ma) in the early stage, and layered mafic ultramafic complex, very rich magnesium ultramafic dike, mica -olivine pyroxenite breccia pipe, diabase dike, quartz syenite and bimodal dike (284-274 Ma) in the late stage.