[1]Wei Guanyi(卫管一), Shi Shaoqing(石绍清), Mao Yanshi(茅燕石), et al. Precambrian Structure and Metamorphism in the Himalayan Region[M]. Chengdu: Chengdu Science and Technology University Press,1989(in Chinese). [2]Liu Guohui(刘国惠), Jin Chengwei(金成伟), Wang Fubao(王富宝), et al. Tibet Metamorphic and Igneous Rocks[M]. Beijing: Geological Press, 1990(in Chinese). [3]Liu Yuping (刘宇平), Chen Zhiliang(陈智梁). The PT path evidence in the metamorphic rocks of the NS structure in the Himalayas[J]. Tethys Geology(特提斯地质), 1994,18: 52-60(in Chinese). [4]Chen Bingwei(陈炳蔚), Ren Liudong(任留东), Wang Yanbin(王彦斌).Tectonics and deformation feature of the Tibet-Qinghai Plateau and its adjacent region[A]. In:Xiao Xuchang(肖序常), Li Tingdong(李廷栋), eds. Tectonic Evolution and Uplift of Qinghai-Xizang (Tibet) Plateau[C]. Guangzhou: Guangdong Science and Technology Press, 2000.83-122(in Chinese). [5]Wu Chunming(吴春明), Geng Yuansheng(耿元生). Some research advances on detailed metamorphic process in the last five years[J].Advances in Earth Science(地球科学进展), 2001, 16(6): 785-794(in Chinese). [6]Ren Liudong(任留东), Chen Bingwei(陈炳蔚). The metamorphism and granitic features of the north Himalayas and their comparison with that of the high Himalayan belt[J]. Geology Bulletin(地质通报), 2002,21: 397-404(in Chinese). [7]McLellan E L. Sequential formation of subsolidus and anatectic migmatites in response to thermal evolution, eastern Scotland[J]. Journal of Geology, 1989, 97:165-182. [8]He Yixing(贺义兴), Ma Rui(马瑞), Yao Jie(姚杰), et al. The microdomain mineral textures of anatexis in the sillimanite-K-feldspar leptynite of the Fuping group at Pingshan county, Hebei Province[J]. Geological Review(地质论评), 2001, 47: 82-87(in Chinese). [9]Kerrick Derrill M. Reviews in Mineralogy[A]. In: Paul H Ribbe, ed. The Al2SiO5 Polymormphs[C]. Mineralogical Society of America, 1990. [10]Argles T W,Platt J P. Stepped fibres in sillimanite-bearing veins: Valid shear-sense indicators in high grade rocks? [J]. Journal of Structural Geology, 1999, 21:153-159. [11]McLellan E L. Metamorphic reactions in the kyanite and sillimanite zones of the Barrovian type area[J]. Journal of Petrology, 1985, 26:789-818. [12]Wells P R A. P-T conditions in the Moines of the Central Highlands Scotland[J]. Journal of Geological Society of London, 1979, 136: 663-671. [13]Ahmad R, Wilson C J L. Microstuctural relationships of sillimanite and fibrolite at Broken Hill, Australia[J]. Lithos, 1982, 15: 49-58. [14]Vernon R H, Flood R H, D'Arcy. Sillimanite and andalusite produced by base-cation leaching and contact metamorphism of felsic igneous rocks[J]. Journal of Metamorphic Geology, 1987, 5: 439-450. [15]Wintsch R P, Andrews M SDeformation induced growth of sillimanite: “Stress” minerals revisited[J]. Journal of Geology, 1988, 96: 143-161. [16]Nabelek P I. Quartz-sillimanite leucosomes in high-grade schists, Black Hills, South Dakota, a perspective on the mobility of Al in high grade metamorphic rocks[J]. Geology, 1997, 25: 995-998. [17]McLelland J, Morrison J, Selleck B, et al. Hydrothermal alteration of late- to post-tectonic Lyon Mountain Granitic Gneiss, Adirondack Mountains, New York: Origin of quartz-sillimanite segregations, quartz-albite lithologies, and associated Kiruna-type low-Ti Fe-oxide deposits[J]. Journal of Metamorphic Geology, 2002, 20 (1):175-190. [18]Anderson G M, Pascal M L, Rao J. Aluminum speciation in metamorphic fluids[A]. In: Helgeson H C ed. Chemical Transport in Metasomatic Processes[C]. Boston: Reidel, 1988. 297-321. [19]Morgan G B, London D. Experimental reactions of amphibole with boron-bearing aqueous fluids at 200 MPa: Implications for tourmaline stability and partial melting in mafic rocks[J].Contributions to Mineralogy and Petrology, 1989,102: 281-297. |