Petrogenesis of Early Permian Intrusive Rocks from Southeastern Inner Mongolia, China: Constraints on the Tectonic Framework of the Southeastern Central Asian Orogenic Belt

Abstract

The Central Asian Orogenic Belt (CAOB) is one of the largest and longest-lasting accretion-type orogens, located to the south of the Siberia Cratonand to the north of the Tarim and North China cratons, east of the Baltica Craton and west of the Pacific