Permo-Triassic paleogeographic, paleoclimatic and paleoceanographic evolutions in eastern Tethys and their coupling

摘要

［1］Yang, Z. Y., Wu. S. B., Yin, H. E et al., Permo-Triassic Events of South China (in Chinese), Beijing: Geological Publishing House, 1991, 1-180.［2］Jin Y. G., Wang, Y.. Wang, W. et al., Pattern of marine mass extinction near the Permian-Triassic boundary in South China,Science, 2000, 289(5478): 432-36.［3］Ziegler. A. M., Michael, L., Hulver. M. L. et al., Permian world topography and climate, in Late Glacial and Postglacial Environmental Changes——Quaternary, Carboniferous-Permian and Proterozoic (ed., Maitini, I. P.), New York: Oxford Univ. Press, 1997, 111-146.［4］Crowley, T. J., Pangea climate, In Pangea: Paleoclimate, Tectonics and Sedimentation during Accretion, Zenith and Breakup of a Supercontinent (ed., Klein, G. D.), Colorado: Geological Society of America Special Paper 288, 1994,25-39.［5］Parrish, J. T., Climate of the supercontinent Pangea, The Journal of Geology, 1993, 101:215-233.［6］Ziegler. A. M., Phytogeographic patterns and continental configurations during the Permian Period, in Palaeozoic Palaeogeography and Biogeography (eds, McKerrow, W. S., Scotese, C. R.), London: Geological Society Memoir 12, 1990,363-379.［7］Yan, J. X., Liu, B. P., Zhang, H. Q., Palaeogeographic implications of Carboniferous to Permian oolitic limestones in the Changning-Menglian belt of west Yunnan, Journal of Palaeogeography (in Chinese), 1999,1 (3): 13-18.［8］Yin, H. F., Peng, Y. Q., The Triassic of China and its interregional correlation, in Permian-Triassic Evolution of Tethys and Western Circum-Pacific (eds., Yin, H. F., Dickins, J. M., Shi, G. R. et al.), Amsterdam: Elsevier, 2000, 197-220.［9］Yan. J. X.,Permian-Triassic paleoclimatic of eastern Tethys and its paleogeographic implication, Earth Science (in Chinese), 1999, 24(1): 13-20.［10］Yan, J. X., Yin, H. F., Paleoclimatic constraints for Early Permian paleogeography of eastern Tethys, In Permian-Triassic Evolution of Tethys and Western Circum-Pacific (eds., Yin, H, F., Dickins, J. M., Shi, G. R. et al), Amsterdam: Elsevier,2000, 1-15.［11］Metcalfe, I., Gondwanaland dispersion, Asian accretion and evolution of eastern Tethys, Australian Journal of Earth Sciences, 1996, 43: 605-23.［12］Zhong. D. L., Paleo-Tethyan Orogeny in the Western Yunnan and Sichuan (in Chinese), Beijing: Science Press, 1998, 1-231.［13］Brookfield, M. E., The Himalayan passive margin from Precambrian to Cretaceous times, Sedimentary Geology, 1993, 84:1-35.［14］Blendinger, W., Furnish, W. M., Glenister, B. F., Permian cephalopod limestones, Oman Mountains: evidence for a Permian seaway along the northern margin of Gondwana, Palaogeography, Paleoclimatology, Palaeoecology, 1992, 93:13-20.［15］Zhao, X. X., Coe, R. S., Gilder, S. A. et al., Palaeomagnetic constraints on the palaeogeography of China: implications for Gondwanaland, Australian Journal of Earth Sciences, 1996, 43: 643-672.［16］Laveine, J. E, The distribution of Eurasiatic late Paleozoic floras: a main tool for paleogeographic relationships, Biostratigraphy of Mainland Southeast Asia-Facies & Paleontology, 1993, 2: 347-359.［17］Yin, H. F., Zhang, K. X., Characteristics of the eastern Kunlun orogenic belt, Earth Science (in Chinese), 1997, 22(4): 339-342.［18］Biah, Q. T., Chang, C. F., Zheng, X. S., Basic geotectonic characteristics of the Hoh Xil region of Qinghai Province, China, Scientia Geologica Sinica (in Chinese), 1997, 32(1): 37-6.［19］Lin, J. L., Watts, D. R., Paleomagnetic study of the Tibetan Plateau, in Geological Evolution of the Tibetan Plateau (ed., Sino-Britain Scientific Expedition Team) (in Chinese), Beijing: Science Press, 1990, 242-281.［20］Ye, X. H., Li, J. F., Palaeomagnetism and evolution of Tibetan Plates and Tethys, Journal of Chengdu College of Geology (in Chinese), 1987, 14(1): 65-79.［21］Archbold, N. W., Shi, G. R., Western Pacific Permian marine invertebrate palaeobiogeography, Australian Journal of Earth Sciences, 1996, 43: 635-41.［22］McLoughlin, S., Lindstrom, S., Drinnan, A. N., Gondwana floristic and sedimentological trends during the Permian-Triassic transition, new evidence from the Amery Group, northern Prince Charles Mountains. East Antarctica, Antarctic Science, 1997, 9(3): 281-298.