[1] Bell T H,Johnson S E. Porphyroblast inclusion trails: the key to orogenesis. Journal of Metamorphic Geology, 1989,7(3): 279-310. [2] Schulz B. Prograde-retrograde PTt-deformation path of Austroalpine micaschists during Variscan continental collision(Eastern Alps). Journal of Metamorphic Geology, 1990, 8(6):629-643. [3] Brown M. PTt evolution of orogenic belts and thecauses of regional metamorphism. Journal of the Geological Society,1993,150(2): 227-241. [4] Bell T H, Johnson S E. Shear sense: a new approach that resolves conflicts between criteria in metamorphic rocks.Journal of Metamorphic Geology, 1992, 10(1): 99-124. [5] Bell T H. Foliation development and refraction in metamorphic rocks: reactivation of earlier foliations and decrenulation due to shifting patterns of deformation partitioning. Journal of Metamorphic Geology, 1986, 4(4): 421-44. [6] Bell T H,Rubenach M J.Sequential porphyroblast growth and crenulation cleavage development during progressive deformation. Tectonophysics, 1983, 92(1-3): 171-194. [7] Bell T H, Fleming P D, Rubenach M J. Porphyroblast nucleation, growth and dissolution in regional metamorphic rocks as a function of deformation partitioning during foliation development. Journal of Metamorphic Geology,1986,4(1):37-67. [8] Bell T H, Johnson S E, Davis B, et al. Porphyroblast inclusion-trail orientation data: eppure non son girate. Journal of Metamorphic Geology, 1992,10(3): 295-307. [9] Gray N H, Busa M D. The three-dimensional geometry of simulated porphyroblasts inclusion trails:inert-marker,viscous-flow models. Journal of Metamorphic Geology, 1994, 12(5): 575-587. [10] Vernon R H. Porphyroblast-matrix microstructural relationships:recent apporoaches and problems.In:Daly J S,Cliff R A, Yardley B W D, eds. Evolution of Metamorphic Belts. Geological Society Special Publication, 1989, 43:83-102. [11] Bard J P. Microtextures of igneous and metamorphic rocks. Dordrecht/Boston/Lancaster,D.Reidel Publishing Company, 1987. 70-107. [12] Passchier C W, Trouw R A, Zwart H J, et al. Porphyroblast rotation: eppur si muove? Journal of Metamorphic Geology, 1992, 10(3): 283-294. [13] Bell T H, J oh nson S E. R otat ion of relat ively large rigid ob jects during ductil e def ormat ion : W ell est ab lish ed fact or int uit ive prejudice? A u st ralian J ournal of Ear th S ciences, 1990, 37( 4) : 441-446. [14] Aerden D G A M. Prophyroblast non-rotation during crustal extension on the Variscan Lys-Caillaouas Massif. Pyrenees. Journal of Structural Geology,1995, 17(5): 709-725. [15] Mancktelow N S, Visser P. The rotation of porphyroblasts around a single fold. Lukmanier Pass. Central Alps: reply.Journal of Structural Geology, 1993,15(3): 1369-1372. [16] Hayward N. Microstructural analysis of the classical spiral garnet porphyroblasts of south-east Vormont: evidence fornon-rotation. Journal of Metarnorphic Geology, 1992, 10(4): 567-587. [17] Bell T H,Forde A. On the significance of foliation patterns preserved around folds by mineral overgrowth.Tectono-physics, 1995, 246(3): 171-181. [18] Williams M L. Sigmoidal inclusion trails. punctuated fabric development, and interactions between metamorphism and deformation. Journal of Metamorphic Geology, 1994, 12(1): 1-21. [19] Bell T H, Hayward N. Episodic metamorphic reactions during orogenesis: the control of deformation partitioning on reactions sites and reaction duration. Journal of Metamorphic Geology, 1991, 9(5): 619-640. [20] Hayward N. Determination of early fold axis orientations within multiply deformed rocks using porphyroblasts.Tectonophysics, 1990, 179(3-4): 353-369. [21] Bjornerud M, Zhang H. A menu-driven Macintosh program for simulating shear-sense indicator development. Geological Society of America. Abstracts with Programs,1992,24:A184. [22] Cashman K V, Ferry J M. Crystal size distribution (CSD) in rocks and kinetics and dynamics of crystallization: Ⅲ Metamorphic crystawzation. Contributions to Mineralogy and Petrology, 1988, 99(4): 401-415. [23] Ridley J. Modeling of the relations between reaction enthalpy and the buffering of reaction progress in metamor-phism. Mineralogical Magazine, 1986, 50(3): 375-384. [24] Barker A J. In terpretation of porphyroblast inclusion trails: limitations imposed by growth kinetics and strain rates. Journal of Metamorphic Geology, 1994, 12(6): 681-694. [25] 庄育勋. 中国阿尔泰造山带热动力时空演化和造山过程. 长春: 吉林科学技术出版社, 1994. 184-185. [26] 王惠初. 变斑晶多期生长与区域多期变形的关系. 国外前寒武纪地质, 1995, 1:53-60. [27] Zwart H J. On the determination of polymetamorphic mineral as sociations and its application to the Bosostarea (Central Pyrenees). Geologische Rundschau, 1962, 52(1):28-65. [28] Masuda T, Mizuno N. Deflection of pure shear viscous flow around a rigid spherical body. Journal of Structural Geology, 1995, 17(11): 1615-1620. [29] Busa M D,Gray N H.Rotated staurolite porphyroblasts in the Littleton schistat Bolton,Connecticut,USA.Journal of Metamorphic Geology, 1992, 10(5): 627-636. [30] Bell T H, Brothers R N. Development of P-T prograde and P-retrograde, T-prograde isogrdic surfaces during blueschist to eclogite regional deformation/metamorphism in New caleclonia, as in dicated by progressively developed porphyroblast microstructures. Journal of Metamorphic Geology, 1985, 3(1): 59-78. |