[1] Baker V R, Benito G, Rudoy, 1993. A paleohydrology of Late Pleistocene superflooding, Altay Mountains, Siberia. Science, 259: 48–350.
[2] Cao Guangjie, Wang Jian, Qu Guixian, 2006. Formation & sedimentary characteristics of the Yangtze River incised- valley in Nanjing. Journal of Henan University (Natural Science), 36(1): 66–69. (in Chinese)
[3] Cao Guangjie, Wang Jian, Xiong Wanying et al., 2006. Sedimentary characteristics of the Yangtze River’s paleovalley in Nanjing since the Last Glacial Maximum. Marine Geology & Quaternary Geology, 26(1): 23–28. (in Chinese)
[4] Dou Guoren, 1999. Incipient motion of coarse and fine sediment. Journal of Sediment Research, (6): 1–9. (in Chinese)
[5] Fang Jinqi, 1990. The numerical analog of the sea-level rise affecting the Yangtze River middle and lower reaches since late ice age. Science in China (Series B), 20(8): 870–878. (in Chinese)
[6] Guo Xumin, 1983. Evolution of sedimentary environment of the Changjiang estuary area since the late stage of late Pleistocene. Chinese Journal of Geology, 18(4): 402–408. (in Chinese)
[7] Han Qiwei, He Mingmin, 1999. The Incipient Disciplinarian and Incipient Velocity of Sediment. Beijing: Science Press. (in Chinese)
[8] Institute of Geography, CAS, Yangtze River Institute of Water Resources and Hydro-Power Research, 1985.
[9] Channel Properties and Evolution in the Yangtze River’s Middle and Lower Reaches. Beijing: Science Press, 60–61. (in Chinese)
[10] Jiang Sishan, Ang Chaohai, Yang Huicheng et al., 1986. A preliminary research on the ancient channel of the Qinhuai River and the age of its sediments. Acta Geologica Sinica, 60(1): 89–101. (in Chinese)
[11] Judith Maizels, 1990. Raised channel systems indicators of palaeohydrologic change: A case study from Oman. Palaeogeography, Palaeoclimatology, Palaeoecology, 76(3/4): 241–277.
[12] Kemp Justine, 2007. Evidence for regionally wet conditions before the LGM in southeast Australia: OSL ages from a large palaeochannel in the Lachlan Valley. Journal of Quaternary Science, 22(5): 423–427.
[13] Lambeck Kurt, 1990. Late Pleistocene, Holocene and present sea-levels: Constraints of future change. Palaeogeography, Palaeoclimatology, Palaeoecology, 89: 205–217.
[14] Li Congxian, Zhang Guijia, 1995. A sea-running Changjiang River during the last glaciation? Acta Geographica Sinica, 50(5): 459–463. (in Chinese)
[15] Liu Jian, Yu Ge, Chen Xiang et al., 2002. Simulation of climate during the mid-Holocene and the Last Glacial Maximum in East Asia. Progress in Nature Science, 12(7): 713–720. (in Chinese)
[16] Liu Yu, He Jinhai, Liu Weiliang et al., 2007. MM5 simulations of the China regional climate of the LGM (II): Influences of land area, vegetation, and large-scale circulation background. Acta Meteorologica Sinica, 12(2): 151–159. (in Chinese)
[17] Maizels J K, 1983. Palaeovelocity and palaeodischarge determination for coarse gravel deposits. In: Gregory K (ed.). Background to Palaeohydrology. Chichester: Wiley, 101–139.
[18] Qian Yun, Qian Yongfu, Zhang Yaocun, 1998. Study on scenarios and mechanism of the regional climate change of East Asia in the Last Ice-age. Scientia Atmospherica Sinica, 22(3): 283–293. (in Chinese)
[19] Rotnicki K, 1991. Retrodiction of palaeodischarges of meandering and sinuous rivers and its palaeoclimatic implications. In: Starkel L et al. Temperate Palaeohydrology. Chichester: Wiley, 431–470.
[20] Sidorchuk A Yu, Borisova O K, 2000. Method of paleogeographical analogues in paleohydrological reconstructions. Quaternary International, 72(1): 95–106.
[21] Williams G P, 1988. Paleofluvial estimates from dimensions of former channels and meanders. In: Baker V et al. Flood Geomorphology. Chichester: Wiley, 321–334.
[22] Xia Dongxing, Liu Zhenxia, 2001. Tracing the Changjiang River’s flowing route into the sea during the last glacial maximum. Acta Oceanologica Sinica, 23(5): 88–95. (in Chinese)
[23] Yang Dayuan, 1986. The paleoenvironment of the mid-lower regions of Changjiang in the full-glacial period of Late Pleistocene. Acta Geographica Sinica, 41(4): 302–310. (in Chinese)
[24] Yang Dayuan, 1989. Changes of water level in the mid-lower reaches of the Changjiang River since the end of Late Pleistocene. Quaternary Sciences of China, 8(1): 114–119. (in Chinese)
[25] Yang Huairen, 1987. Quaternary Geology. Beijing: Higher Education Press. (in Chinese)
[26] Yang Huairen, Han Tongchun, Yang Dayuan et al., 1983. Processes and causal mechanism of migrations of the Changjiang since Late Pleistocene. Journal of Nanjing University (Natural Science), (2): 341–350. (in Chinese)
[27] Yang Huairen, Xu Xin, Yang Dayuan et al., 1995. Environmental Changes and Ecosystems in the Yangtze River’s Middle and Lower Reaches. Nanjing: Hohai University Press, 86–93. (in Chinese)
[28] Yu Ge, Chen Xing, Liu Jian et al., 2000. Simulation and diagnosis of East Asian climate in the Last Glacial Maximum. Chinese Science Bulletin, 45(20): 2153–2159. (in Chinese)
[29] Zheng Yiqun, Yu Ge, Wang Sumin et al., 2002. Simulations of Last Glacial Maximum climate of East Asia by regional climate model. Science in China (Series D), 32(10): 871–880. (in Chinese)
[30] Zhu Yongqi, 1984. Primary study on the physiognomy in East China Sea continental shelf. In: Collection of Studies on the East China Sea. Beijing: China Ocean Press, 65–70. (in Chinese)
|