Hl. Mei et al., The first discovery of eclogite and Palaeoproterozoic granitoids in the Beishan area, northwestern Gansu Province, China, CHIN SCI B, 44(4), 1999, pp. 356-361
The eclogite, discovered in Liuyuan, occurs as lenticular enclave within gr
anitic gneiss. It has typical features of eclogite in petrology and mineral
ogy. The eclogite provides an important window to reconstruct the tectonic
border of the Tarim block. The granitoids, located in Baihu area, yield U-P
b zircon ages of 1 660-2 000 Ma (Palaeoproterozoic), which implies an early
Precambrian basement in the area.