1 Brodie K H, Rutter E. On the relationship between deformation and metamorphism with special reference to the behaviour of basic rocks. In: Thompson A B, Rubie D C, eds. Metamorphic Reactions: Kinematics, Textures, and Deformation. Berlin: Springer, 1985. 138-179
[2]
2 Barruol G, Kern H. Seismic anisotropy and shear-wave splitting in low-crustal and upper-mantle rocks from the Ivrea Zone—Experimental and calculated data. Phys Earth Planet Inter, 1996, 95: 175-194？？
[3]
3 Drury M R, Ural J. Deformation-related recrystallization processes. Tectonophysics, 1990, 172: 235-253？？
[4]
4 Stünitz H. Transition from fracturing to viscous flow in a naturally deformed metagabbro. In: Boland J N, Fitz Gerald J D, eds. Defects and Processes in the Solid State: Geoscience Applications. Amsterdam: Elsevier, 1993. 121-150
[5]
5 Berger A, Stünitz H. Deformation mechanisms and reaction of hornblende: Examples from the Bergell tonalite (Central Alps). Tectonophysics, 1996, 257: 149-174？？
[6]
6 De Meer S, Drury M R, De Bresser J H P, et al. Deformation Mechanisms, Rheology and Tectonics: Current Issues and New Developments in Deformation Mechanisms, Rheology and Tectonics. London: Geol Soc Spec Publ, 2002. 200
[7]
7 Kitamura K. Constraint of lattice-preferred orientation (LPO) on Vp anisotropy of amphibole-rich rocks. Geophys J Int, 2006, 165: 1058-1065？？
[8]
8 Díaz Azpiroz M, Lloyd G E, Fernández C. Development of lattice preferred orientation in clinoamphiboles deformed under low-pressure metamorphic conditions—A SEM/EBSD study of metabasites from the Aracena metamorphic belt (SW Spain). J Struct Geol, 2007, 29: 629-645.？？
[9]
9 Tatham D J, Lloyd G E, Butler R W H. Amphibole and lower crustal seismic properties. Earth Planet Sci Lett, 2008, 267: 118-128？？
[10]
10 Tullis J. Deformation of feldspars. In: Ribbe P H, ed. Reviews in Mineralogy—Feldspar Mineralogy. Mineral Soc Amer, 1983, 2: 297-323
[11]
11 Passchier W C, Trouw R A J. Microtectonics. Berlin: Springer, 2005. 60-61
[12]
12 Imon R, Okudaira T, Fujimoto A. Dissolution and precipitation processes in deformed amphibolites: An example from the ductile shear zone of the Ryoke metamorphic belt, SW Japan. J Metamorph Geol, 2002, 20: 297-308？？
[13]
13 Imon R, Okudaira T, Kanagawa K. Development of shape- and lattice-preferred orientations of amphibole grains during initial cataclastic deformation and subsequent deformation by dissolution-precipitation creep in amphibolites from the Ryoke metamorphic belt, SW Japan. J Struct Geol, 2004, 26: 793-805？？
[14]
14 Rooney T P, Riecker R E, Gavasci A T. Hornblende deformation features. Geology, 1975, 3: 364-366？？
[15]
15 Morrison-Smith D J. Transmission electron microscopy of experimentally deformed hornblende. Am Mineral, 1976, 61: 272-280
[16]
16 Dollinger G, Blacic J D. Deformation mechanisms in experimentally and naturally deformed amphiboles. Earth Planet Sci Lett, 1975, 26: 409-416？？
[17]
17 Biermann C. (100) deformation twins in naturally deformed amphiboles. Nature, 1981, 292: 821-823？？
[18]
18 Hacker B, Christie J M. Brittle/ductile and plastic/cataclastic transition in experimentally deformed and metamorphosed amphibolite. In: Duba A G, Durham W B, Handie J W, et al, eds. The Brittle-Ductile Transition in Rocks. AGU Geophys Monogr Ser, 1990, 56: 127-148？？
23 王凯怡, 郝杰, Wilde S A, 等. 山西五台山-恒山地区晚太古-早元古代若干关键地质问题的再认识: 颗粒锆石离子探针质谱年龄提出的地质制约. 地质科学, 2000, 35: 175-184
[24]
24 Wield S A. SHRIMP U-Pb zircon ages of the Wutai Complex. In: Kr？ner A, Zhao G C, et al, eds. A Late Archaean to Paleoproterozoic Lower to Upper Crustal Section in the Hengshan-Wutaishan Area of North China. Guidebook for Penrose Conference Field Trip. Beijing:Chinese Academy of Sciences, 2002. 32-34
26 Kaibysheva O A, Pshenichniuka A I, Astanin V V. Superplasticity resulting from cooperative grain boundary sliding. Acta Mater, 1998, 46: 4911-4916？？
[27]
27 Zelin M G, Krasilnikov N A, Valiev R Z, et al. On the microstructural aspects of the nonhomogeneity of superplastic deformation at the level of grain groups. Acta Mater, 1994, 42: 119-126？？
[28]
28 Schmid S M. Microfabric studies as indicators of deformation mechanisms and flow laws operative in mountain building. In: Hsu K J, ed. Mountain Building Processes. London: Academic Press, 1982. 95-110
[29]
29 Rutter E H, Casey M, Burlini L. Preferred crystallographic orientation development during the plastic and superplastic flow of calcite rocks. J Struct Geol, 1994, 16: 1431-1446？？
[30]
30 Boullier A M, Guéguen Y. Peridotite mylonite produced by superplastic flow. In: Snoke A, Tullis J, Todd V R, eds. Fault Related Rocks—A Photographic Atlas. New Jersey: Princeton University Press, 1998. 514-515
[31]
31 Hoshikuma A. Grain growth and superplasticity: Their implication to earth science. J Geol Soc JP, 1996, 102: 232-239？？
[32]
32 靳是琴, 李鸿超. 成因矿物学概论. 长春: 吉林大学出版社, 1986. 221-222
[33]
33 Holland T, Blundy J. Non-ideal interactions in calcic amphiboles and their bearing on amphibole-plagioclase thermometry. Contrib Mineral Petrol, 1994, 116: 433-447？？
[34]
34 Anderson L A, Smith D R. The effects of temperature and fO2 on the Al-in-hornblende barometer. Am Mineral, 1995, 80: 549-559
[35]
35 Gifkins R C. Grain boundary sliding and its accommodation during creep and superplasticity. Metall Mater Trans, 1976, 7A: 1225-1232？？
[36]
36 White J C, White S H. On the structure of grain boundaries in tectonics. Tectonophysics, 1981, 78: 613-628？？
[37]
37 Behrmann J H, Mainprice D. Deformation mechanisms in a high-temperature quartz feldspar mylonite: Evidence for superplastic flow in the lower continental crust. Tectonophysics, 1987, 140: 297-305？？
[38]
38 Tullis J, Dell’Angelo L, Yund R A. Ductile shear zones from brittle precursors in feldspathic rocks: The role of dynamic recrystallization. In: Hobbs B E, Heard H C, eds. Mineral and Rock Deformation: Laboratory Studies. AGU Geophys Monogr Ser, 1990, 56: 67-81？？
[39]
39 Flervoet T F, White S H. Quartz deformation in a very fine grained quartzo-feldspathic mylonite: A lack of evidence for dominant grain boundary sliding deformation. J Struct Geol, 1995, 17: 1095-1109？？
[40]
40 Fliervoet T F, White S H, Drury M R. Evidence for dominant grain-boundary sliding deformation in greenschist- and amphi-bolite-grade polymineralic ultramylonites from the Redbank Defor Maed Zone, Central Australia. J Struct Geol, 1997, 19: 1495-1520？？
[41]
41 Hanmer S. Matrix mosaics, brittle deformation, and elongate porphyroclasts: Granulite facies microstructures in the Striding-Athabasca mylonite zone, western Canada. J Struct Geol, 2000, 22: 947-967？？
[42]
42 Brodie K H. Retrogressive mylonitic metabasic fault rocks. In: Snoke A, Tullis J, Todd V R, eds. Fault Related Rocks—A Photographic Atlas. New Jersey: Princeton University Press, 1998. 402-403
[43]
43 Poirier J P. Creep of Crystals: High-Temperature Deformation Processes in Metals, Ceramics and Minerals. Cambridge: Cambridge University Press, 1985. 276
[44]
44 胡玲. 显微构造地质学概论. 北京: 地质出版社, 1998. 46-47
[45]
45 Vauchez A. Ribbon texture and deformation mechanisms of quartz in a mylonitized granite of Great Kabylia (Algeria). Tectonophysics, 1980, 67: 1-12？？
[46]
46 Behrmann J H. Crystal plasticity and superplasticity in quartzite: A natural example. Tectonophysics, 1985, 115: 101-129？？
[47]
47 Behrmann J H, Mainprice D. Deformation mechanisms in a high-temperature quartz-feldspar mylonite: Evidence for superplastic flow in the lower continental crust. Tectonophysics, 1987, 140: 297-305？？
[48]
48 Behrmann J H. Microstructure and fabric transition in calcite tectonics from the Sierra Alhamilla (Spain). Geol Rundsch, 1983, 72: 605-618？？
[49]
49 Allison I, Barnett R L, Kerrich R. Superplasitic flow and changes in crystal chemistry of feldspar. Tectonophysics, 1979, 53: T41-T46？？
[50]
50 Kleinschrodt R. Competing crystal-plastic and grain size sensitive deformation mechanisms in a peridotite from the Finero Complex (Ivrea Zone, NW-Italy). In: Bunge H J, Siegesmund S, Skrotzki W, et al, eds. Textures of Geological Materials. Oberured: DGM Infor- mationsgesellschaft-Verlag, 1994. 201-219
[51]
51 Ashby M F, Verrall R A. Diffusion-accommodated flow and superplasticity. Acta Metall, 1973, 21: 149-163？？
