supported by China Ministry of Science and Technology ("973" Project) (2012CB4166006);the National Natural Science Foundation of China (41210003)
Recently, more attention has been paid to Precambrian magma events and crustal growth of the North China Craton(NCC), accompanying with controversy in activity stages and dynamic mechanism. In this study, we report th...
This work was supported by the NationalNatural Sciences Foundation of China; the Science and Technology of Commission of China.
Zircon U-Pb ages have been determined for basement gneisses in the Bayan Obo REE-Fe-Nb deposit. On the U-Pb concordia diagram data of three samples yield up-per intercept ages of 1948-1917 Ma. Thus, these basement gne...
This work was supported by the National Natural Science Foundation of China (Grant No. 49872072) ; the Postdoctoral Foundation of China, as well as U.S. National Science Foundation (Grant No. EAR-9903012).
A zircon U-Pb age of (916±16) Ma is measured for grantoid gneisses from the Yagan-Onch Hayrhan metamorphic core complex and represents the crystallization age of the grantoid magma. This age provides evidence for the...
This work was sup- ported by the National Natural Science Foundation of China (Grant No.49972029) ; the Ministry of Science and Technology of China (Grant No. G1999075501).
The mineral inclusions in zircon from gneisses in ultra-high pressure (UHP) zone of the Dabie Mountains were identified by using a laser Raman microspectrometer. Coesite occurs as inclusions in zircons from all types ...
Adakite is an igneous rock generated by the partial melting of subducting ocean slab in an island arc setting. Meanwhile, residuals of the slab-melting are transformed to eclogite or garnet-amphibolite during a slab s...
The mineral inclusions in accessory minerals of the country gneisses have been studied in order to interpret relation between eclogites and their country gneissic rocks. Omphacite inclusions have been identified in ti...
A detailed mapping work has revealed that the studied Santunying area, which is about 500 km^2, is dominantly composed of three granulite facies plutonic gneisses, Santunying gneiss, Xiaoguanzhuang gneiss, both Q-dior...