[1]Walshe J L. A six-component chlorite solid solution model and the systems[J]. Economical Geology,1986, 81: 681-703.
[2]Essene E J. The current status of thermobarometry in metamorphic rocks[J].American Mineralogist,1989, 74: 1-44. 
[3]Hoish T D. A muscovite-biotite geothermometer[J]. American Mineralogist,1989, 74: 565-572.
[4]Mancktelow N S, Pennacchioni G. The influence of grain boundary fluids on the microstructure of quartz-feldspar mylonites[J]. Journal of Structural Geology, 2004, 26: 47-69.
[5]Passchier C W, Trouw R A J. Micro-tectonics[M]. Springer-verlag Berlin Heidelberg,1996:36-45.
[6]Stipp M, Stünitz H, Heilbronner R, et al. The eastern Tonale fault zone: A  natural laboratory' for crystal plastic deformation of quartz over a temperature range from 250 to 700℃[J]. Journal of Structural Geology,2002, 24:1 861-1 884.
[7]Sibson R H. Fault rock distribution and structure within the Alpine fault zone: A preliminary account[J]. Bulletin of the Royal Society of New Zealand,1999, 18:55-66.
[8]Van D. Orientation analysis of localized shear deformation in quartz fibres at the brittle-ductile transition[J]. Tectonophysics,1999, 303: 83-107.
[9]Hirth G, Tullis J. Dislocation creep regimes in quartz aggregates[J]. Journal of Structural Geology,1992,14:145-159.
[10]Neil S Mancktelow. The influence of grain boundary fluids on the microstructure of Quartz-feldspar Mylonites[J]. Journal of Structural Geology,2004,26: 47-69.
[11]White S H. Geological significance of recovery and recrystallization processes in quartz[J]. Tectonophysics,1977, 39: 143-170.
[12]Drury M R,Urai J L. Deformation-related recrystallization processes[J]. Tectonophysics,1990, 172:235-253.
[13]Schofield D L, Dlemos R S. Relationship between syn-tectonic granite fabric and regional P-T-t-d paths: An example from the Gander-Aralon boundary of NE Newfounelland[J]. Journal of Structural Geology,1998, 30:459-471.
[14]Lister G S, Dornsiepen U F. Fabric transitions in the Saxony granulite terrain[J]. Journal of Structural Geology,1982, 41: 81-92.
[15]Law R D. Crystallographic fabrics: A selective review of their applications to research in structural geology[C]//Knipe R J, Rutter E H, eds. Deformation Mechanisms, Rheology and Tectonics. Geological Society Special Publication, 1990, 54: 335-352. 
[16]Bouchez J L. Plastic deformation of quartzites at low temperatures in an area of natural strain gradient[J]. Tectonophysics, 1997, 39: 25-50.
[17]Mainprice D, Bouchez J L, Blumendeld P. Domiant c-slip in naturally deformed quartz: Implications for dramatic plastic softening at high temperature[J]. Geology, 1986, 14: 819-822.
[18]Tullis J, Yund R A. Transition from cataclastic flow to dislocation creep of feldspar: Mechanisms and microstructures[J]. Geology, 1987, 15:606-609.
[19]Pryer L L. Microstructures in feldspars from a major crustal thrust zone: The Grenville Front, Ontario, Canada[J]. Journal of Structural Geology, 1993, 15: 21-36.
[20]Borges F S, White S H. Microstructural and chemical studies of sheared anorthosites, Roneval, South Harris[J]. Journal of Structural Geology, 1980, 2: 237-280.
[21]Gapais D. Shear structures within deformed granites: Mechanical and thermal indications[J]. Geology, 1989, 17:1 144-1 147.
[22]Gates A E, Glover L. Alleghanian tectono-thermal evolution of the dextral transcurrent hylas zone, Virginia Piedmont, USA[J]. Journal of Structural Geology, 1989, 11:407-419.
[23]Tullis J, Yund R A. Diffusion creep in feldspar aggregates: Experimental evidence[J]. Journal of Structural Geology, 1991, 13: 987-1 000.
[24]Vidal J L, Debat P, Soula J C. Ddformation and dynamic recrystallization of K-feldspar augen in orthogneiss from montagne Noire, Occitania, Southern France[J]. Lithos,1980, 13: 247-255.
[25]Olsen T S, Kohlstedt D L. Natural deformation and recrystallization of some intermediate plagioclase feldspars[J]. Tectonophysics, 1985, 111: 107-131.
[26]Hay R S, Evans B. Chemically induced grain boundary migration in calcite: Temperature dependence, phenomenology, and possible applications to geologic systems[J]. Contributions to Mineralogy and Petrology, 1987, 97: 77-87.
[27]Rosenberg C L. Deformation and recrystallization of plagioclase along a temperature Gradient: An example from the Bergell tonalite[J]. Journal of Structural Geology, 2003, 25: 389-408.
[28]Yund R A, Tullis J. Compositional changes of minerals associated with dynamic recrystallization[J]. Contributions to Mineralogy and Petrology, 1991, 97: 346-355.
[29]Lafrance B, John Barbara E, Frost B R. Ultra high-temperature and subsolidus shear zones: Examples from the Poe Mountain anorthosite, Wyoming[J]. Journal of Structural Geology, 1998, 20: 945-955.
[30]Anderson D J, Lindsley D H, Dabidson P M. QUILF: A Pascal program to assess equilibria among Fe-Mg-Mn-Ti oxides, pyroxenes, olivine, and quartz[J]. Computers and Geosciences,1993, 19: 1 333-1 350.
[31]Altenberger U. Ductile deformation of K-feldspar in dry eclogite facies shear zones in the Bergen Arcs, Norway[J]. Tectonophysics, 2000, 320: 107-121. 
[32]Ferrill D A, Morris A P, Evans M A,et al. Calcite twin morphology: A low-temperature deformation geothermometer[J]. Journal of Structural Geology, 2004,26:1 521-1 529.
[33]Zhu Guang, Xie Chenglong, Wang Yongsheng, et al. Characteristics of the Tan-Lu high-Pressure strike-slip ductile shear zone and its ⁴⁰Ar/³⁹Ar dating[J]. Acta Petrologica Sinica, 2005, 21(6): 1 687-1 702.
[34]Wang Yongsheng, Zhu Guang, Chen Wen, et al. Thermochronologic information from the Tan-Lu fault zone and its relationship with the exhumation of the Dabie Mountains[J]. Geochimica, 2005, 34(3): 193-214. [王勇生, 朱光, 陈文,等. 郯庐断裂带热年代学信息及其与大别造山带折返的关系[J]. 地球化学, 2005, 34(3): 193-214.]
[35]McDougall I, Harrison T M. Geochronology and Thermochonology by the ⁴⁰Ar /³⁹Ar Method[M]. New York: Oxford University Press, 1998.
[36]Dodson M H. Closure temperature in cooling geochronological and petrological systems[J]. Contributions to Mineralogy and Petrology, 1973, 40(30): 259-174.
[37]Harrison T M. Diffusion of ⁴⁰Ar in hornblende[J]. Contributions to Mineralogy and Petrology, 1981, 78: 324-331.
[38]Reddy S M, Kelley S P, Magennis L. A microstructural and argon laserprobe study of shear zone development at the western margin of the Nanga Parbat-Haramosh Massif, western Himalaya[J]. Contributions to Mineralogy and Petrology, 1997, 128: 16-29.
[39]Zhu Guang, Niu Manlan, Liu Guosheng, et al. ⁴⁰Ar/³⁹Ar Dating for the strike-slip movement on the Feidong Part of the Tan-Lu Fault belt[J]. Acta Geologica Sinica,2005, 79(3):303-316. [朱光, 牛漫兰, 刘国生,等.郯庐断裂带肥东段走滑运动的⁴⁰Ar/³⁹Ar 法定年[J]. 地质学报, 2005, 79(3):303-316.]
[40]Zhu Guang, Wang Yongsheng, Liu Guosheng, et al. ⁴⁰Ar/³⁹Ar dating of strike-slip motion on the Tan-Lu fault zone，East China[J]. Journal of Structural Geology, 2005, 27（8）:1 379-1 398.
[41]Zhu Guang, Wang Daoxuan, Liu Guosheng,et al. Extensional activities along the Tan-Lu fault zone and its geodynamic setting[J]. Scientia Geologica Sinica,2001, 36(3):269-278. [朱光, 王道轩, 刘国生,等. 郯庐断裂带的伸展活动及其动力学背景[J]. 地质科学, 2001, 36(3):269-278.]