Eclogites and ultramafic rocks (peridotites) within biotite gneisses in the eastern part of the Dabie UHP metamorphic terrane.
The original mantle-derived magma, intruded into the lower crust, was contaminated by crustal granulites during magma differentiation.
Located in the southern Dabie Mts.
Ref.:
- Chavagnatz, V., and Jahn, B.M. (1996): Coesite-bearing eclogites from the Bixiling complex, Dabie Mountains, China: Sm-Nd ages, geochemical characteristics and tectonic implications. Chemical Geology 133, 29-51.
- J. Appl. Cryst. 34, 442–453 (2001).
