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Through studies of P|T|t paths and decompressive retrograde metamorphic textures of metamorphic rocks in the East Qinling|Dabieshan region, the authors determined the Mesozoic crust rapid uplifting age, and then inferred that in the East Qinling|Dabieshan region lithosphere delamination occurred from T-3 to J-1. The Yanshanian granites produced by delamination are developed well in the East Qinling|Dabieshan region. But due to the Gondwana plate effect, magmatism in the region caused by delamination lagged until J-3 when the northern Tibet terrane and the Eurasian plate completely amalgamated. Additionally, due to western Pacific plate subducting underneath the Eurasian plate, in the East Qinling|Dabieshan region the stress state was transformed from compression to extension. So in the region from J-3 to K-2 magmatism was most intensive, and liberalization was also relatively strong. Geophysical data reflect that in the East Qinling|Dabieshan region the asthenosphere rose to the shallow level, the Moho is flat with no mountain root, and the crustal thickness is less than 40 km on average. These features agree with those of collisional orogenes in which delamination has occurred. Through contrasting differences in surface and interior depth between east and west Qinling we believe that delamination proceeded from east to west.
Through studies of P | T | t paths and decompressive retrograde metamorphic textures of metamorphic rocks in the East Qinling | Dabieshan region, the authors determined the Mesozoic crust rapid uplifting age, and then inferred that in the East Qinling | Dabieshan region lithosphere delamination occurred from T - 3 to J - 1. The Yanshanian granites produced by delamination were developed in the East Qinling | Dabieshan region. But due to the Gondwana plate effect, magmatism in the region caused by delamination lagged until J - 3 when the northern Tibet terrane and the Eurasian plate completely amalgamated. Additionally, due to western Pacific plate subducting underneath the Eurasian plate, in the East Qinling | Dabieshan region the stress state was transformed from compression to extension. So in the region from J - 3 to K - 2 magmatism was most intensive, and liberalization was also relatively strong. Geophysical data reflect that in the East Qinling | Dabieshan region the asthenos phere rose to the shallow level, the Moho is flat with no mountain root, and the crustal thickness is less than 40 km on average. These features agree with those of collisional orogenes in which delamination has occurred. Through contrasting differences in surface and interior depth between east and west Qinling we believe that delamination proceeded from east to west.