2Caddick M J,Konopasek J,Thompson A B. Preservation of garnet growth zoning and the duration of prograde metamorphism-J3. Journal of Petrology, 2010,51 : 2 327-2 347.
3Mernagh T P, Liu L G. Pressure dependence of Raman spectra from the garnet end-members Pyrope,Grossularite and Almandite[J']. Jou- canl of Raman Spectroscopy, 1990,21 : 305-309.
4Zheng Y-F,Fu B,Gong B, et al. Stable isotope geochemistry of ul-trahigh pressure metamorphic rocks from the Dabie-Sulu Orogen in Chi- na;implications for geodynamics and fluid regime[J]. Earth Science Reviews,2003,62:105-161.
5Henderson R R. Determing chemical composition of the silicate garnets using Raman spectroscopy[D]. America, University of Arizona. 2009,1-13.
6Chaplin T,Price G D,Ross P N. Computer simulation of the infrared and Raman activity of pyrope garnet, and assignment of calculated modes to specific atomic motions[J]. American Mineralogist, 1998,83:841-847.
7Gillet P, Fiquet G, Malezieux J M, et al. High-pressure and high-temperature Raman spectroscopy of end-member garnet: pyrope,grossu- lar and andradite[J]. European Journal of Mineralogy, 1992,4 : 651-664.
8Zheng Y F,Fu B, Li Y L, et al. Oxygen and hydrogen isotope geochemistry of ultraigh-pressure eclogites from the Dabie Mountains and the Sulu terrane[J]. Earth and Planetary Science Letters, 1998,155 (1-2) : 113-129.
