[1] Green H W II. Metastable growth of coesite in high strained quartz[J]. J G R, 1972,77(14):2 478-2 482. [2] Smith D C. Coesite in clinopyroxene in the caledonides and its implications for geodynamics[J]. Nature,1984,310(23):641-644. [3] Mancktelow N S. Nonlithostatic pressure during sediment subduction and the development and exhumation of high pressure metamorphic rocks[J]. J G R, 1995, 100(B1):571-583. [4] Coleman R G, Wang X. Overview of the geology and of UHPM[A]. In: Ultrahigh Pressure Metamorphism[C]. London: Cambridge Univ Press, 1995. 1-32. [5] Wang Fangzheng. A discussion on depth of forming high pressure and ultra-high pressure metamorphic rocks[J]. Journal of China University of Geosciences, 1996, 21(1):41-44.[王方正. 高压、超高压变质岩形成深度讨论[J]. 地球科学,1996,21(1):41-44.] [6] Lu Guxian, Chen Jing, Li Xiaobo,et al. Estimation of tectonic added pressure and depth of forming coesite-bearing eclogites[J]. Chinese Science Bulletin, 1998, 43 (24): 2 590-2 602.[吕古贤, 陈晶, 李晓波,等. 构造附加静水压力研究与含柯石英榴辉岩成岩深度测算[J]. 科学通报,1998,43(24):2 590-2 602.] [7] Dong Shuwen, Sun Xianzhi, Wang Gang, et al. Essential tectonics of Dabie Shan orogenic belt[J]. Chinese Science Bulletin, 1993, 38: 1884-1 888.[董树文,孙先知,王刚,等. 大别山造山带基本结构[J]. 科学通报, 1993,38:1 884-1 888.] [8] Hacker B, Ratschbachor L, Webb L, et al. U/Pb Ziron ages constrain the architecture of the Ultrahigh-pressure Qinling-Dabie Orogen[J]. China Earth Plan Sci Let, 1998, 161: 215-230. [9] Zhao X, Coe R. Paleomagnetic constraints in the collision and rotation of north and south China[J]. Nature, 1987, 327:141-144. [10] Yang Z Y, Courtillot V, Besse J, et al. Jurassic paleomagnetic constraints on the collision of the North and South China Blocks[J]. Geophys Res Lett, 1992, 19 (6): 577-580. [11] Gilder S, Courtillot V. Timing of North-South China collision from new middle to late Mesozoic paleomagnitic data from the North China block[J]. J G R , 1997,102 (B8): 17 713-17 728. [12] Eide E A. A model for the tectonic history of HP and UHPM regions in east central China[A]. In: Coleman R G, Wang X. Ultrahigh Pressure Metamorphism.[C]. London: Cambridge Univ Press, 1995. [13] Turcotte D L, Oxburgh E R. Stress accumulation in the lithosphere[J]. Tectonophysics,1976, 35:183-199. [14] Wang Ren, Ding Zhongyi. Global stress field caused by Earth's rotationchanging in the case of axial symmetry[J]. J Geomechanics, 1982,6:193-196.[王仁,丁中一. 轴对称情况下地球自转速度变化引起的全球应力场[J]. 地质力学论丛,1982,6:193-196.] [15] Hanks T C, Releigh C B. The conference on magnitude of deviatoric stress in the Earth's crust and uppermost mantle[J]. J G R, 1980, 85(B11):6 083-6 085. [16] Dong Shuwen, Wu Xuanzhi, Gao Rui, et al. On the crust velocity levels and dynamics of the Dabie Shan orogenic belt[J]. Acta Geophysica Sinica, 1998, 41(3): 349-361.[董树文,吴宣志,高锐,等. 大别造山带地壳速度结构与动力学[J]. 地球物理学报,1998,41(3):349-361.] [17] Gao Shan, Jin Zhenmin, Kern H, et al. Laboratory high temperature and high- pressure test study of seismic wave’s speed and density of ultrahigh-pressure eclogites from the Dabie Shan[J]. Chinese Science Bulletin, 1997, 42(8):862-865.[高山,金振民, Kern H,等. 大别超高压榴辉岩高温高压下地震波速和密度的初步实验研究[J]. 科学通报,1997,42(8):862-865.] [18] Wang C Y, Shi Y L, Zhou W. On the tectonics of the Himalaya and the Tibet plateau[J].J G R. 1982, 87(B4): 2 949-2 957. [19] Song Chuanzhong, Zhang Guowei. Rheojogy and Dynamics of the eastern Qinling orogenic belt[J]. Acta Geophysica Sinica,1998, 41(Supp.), 55-63. [宋传中,张国伟. 东秦岭造山带的流变学及动力学分析[J]. 地球物理学报,1998,41(增刊):55-63.] [20] Zeng Lixing. Laboratory test method study of deep rock physical mechanics[J]. Journal of Geomechanics, 1999, 5 (1):71-75. [曾立新. 深层岩石力学性质的试验方法[J]. 地质力学学报,1999,5(1):71-75.] [21] Yang Xiaoyong, Yang Xueming, Liu Deling, et al. A micro-structural evidences of tectonic superimposition (compound) by south part of TanchengLujiang Fault belt and Dabie -Jiaonan orogenic belt[J]. 1998, Acta Geophysica Sinica, 41(Suppl.), 123-132.[杨晓勇,杨学明,刘德良,等. 郯庐断裂带南段与大别胶南造山带构造复合的显微构造证据[J]. 地球物理学报,1998,41(增刊):123-132.] |