ZHANG Wei, CUI Zhijiu, LI Yonghua . The glacial extent and glacial advance/retreat asynchroncity in East Asia during Last Glaciation[J]. Journal of Geographical Sciences, 2005 , 15(3) : 293 -304 . DOI: 10.1360/gs050304

[1] Arkhipov S A, Firsov L V, Panichev V A et al., 1973. New data on the stratigraphy and geochronology of the Middle Ob terraces. In: The Pleistocene of Siberia and Adjacent Areas. Moscow: Nauka, 21-34. (in Russia)

[2] Barnard P L, Owen L A, Finkel R C, 2004. Style and timing of glacial and paraglacial sedimentation in a monsoon-influenced high Himalayan environment, the upper Bhagirathi valley, Gavhwal Himalaya. Sedimentary Geology, 165(3-4): 199-221.

[3] Benn D I, Owen L A, 1998. The role of the Indian summer monsoon and the mid-latitude westerlies in Himalayan glaciation: review and speculative discussion. Journal of Geological Society, 155: 353-363.

[4] Cui Z J, Yang J F, Liu G N et al., 1999. Evidence of Quaternary glaciers in high mountains of Taiwan. Chinese Science Bulletin, 44(20): 2220-2224.

[5] Cui Z J, Yang J F, Liu G N et al., 2000. Monsoon development and glacier disappearance: from the point of view of glacier revolution features during Last Glaciation in Xueshan, Taiwan. Journal of Glaciology and Geocryology, 22(1): 7-14. (in Chinese)

[6] Cui Z J, Yang C F, Liu G N et al., 2002. The Quaternary glaciation of Shesan Mountain in Taiwan and glacial classification in monsoon areas. Quaternary International, 97-98, 147-153.

[7] Ding L F, Kang X C, 1985. The influences of Qilianshan glaciers on climatic condition and characteristic of glacial development. Memories of Lanzhou Institute of Glaciology and Geocryology, CAS, Vol. 5. Beijing: Science Press, 9-15. (in Chinese)

[8] Finkel R C, Owen L A, Barnard P L et al., 2003. Beryllium-10 dating of Mount Everest moraines indicates a strong monsoonal influence and glacial synchroneity throughout the Himalaya. Geology, 31: 561-564.

[9] Gillespie A, Molnar P, 1995. Asynchronous maximum advances of mountain and continental glaciers. Reviews of Geophysics, 33(3): 311-365.

[10] Guo H W, Chen Y, Li J J, 1995. A preliminary study on the sequences of glaciers, loess records and terraces of the southern foothills of Lenglong Ling in Qilian Mountains. Journal of Lanzhou University, 31: 102-110. (in Chinese)

[11] Ju Y J, 2004. Glacial advance/retreat and climate change in the middle part of North-Tianshan. Doctoral Thesis, 34-37.

[12] Kerschner K, 1985. Quantitative paleoclimatic inferences from late glacial snowline, timberline and rock glacial data, Tyrolean Alps Australia. Zeitschrift Gletscherkunde und Geologies, 21: 363-369.

[13] Kind N V, 1972. Late Quaternary climatic changes and glacial events in the old and new world. In: Radiocarbon Chronology, Section 12, 24th I.G.C., 55-61.

[14] Kuang M S, Zhao W C, 1997. ESR dating research on depositional layer during late Pleistocene in Diancang mountain, Dali, Yunnan province, China. Yunnan Geographic Environment Research, 1: 49-57. (in Chinese)

[15] Li B Y, Li J J, 1991. Glacial Remains Distributional Map of Quaternary Glaciation in Tibetan Plateau. Beijing: Science Press. (in Chinese)

[16] Li J J, Wen S X, Zhang Q S et al., 1979. A discussion on the period, amplitude and type of uplift of the Qinghai-Xizang Plateau. Science in China, (6): 608-616.

[17] Li J J, 1992. Glacial relics of monsoonal Asia in the Last Glaciation. Quaternary Sciences, (4): 332-339. (in Chinese)

[18] Ono Y, 1984. Last glacial paleoclimate reconstructed from glacial and periglacial landforms in Japan. Geographical Review of Japan (Series B), 57(1): 87-100.

[19] Ono Y, 1991. Glacial and periglacial paleoenvironments in the Japanese Islands. Daiyonki-Kenkyu (The Quaternary Research), 30: 203-211.

[20] Ono Y, Naruse T, 1997. Snowline elevation and eolian dust flux in the Japanese islands during isotope stage 2 and stage 4. Quaternary International, 37: 45-54.

[21] Owen L A, Kamp U, Spencer J Q et al., 2002. Timing and style of late Quaternary glaciation in the eastern Hindu Kush, Chitral, northern Pakistan: a review and revision of the glacial chronology based on new optically stimulated luminescence dating. Quaternary International, 97-98: 41-45.

[22] Phillips W M, Sloan V E, Shroder J F et al., 2000. Asynchronous glaciation at Nanga Parbat, North Himalaya Mountains, Pakistan. Geology, 28: 431-434.

[23] Richards B W, Owen L A, Rhodes E J, 2000. Timing of late Quaternary glaciations in the Himalayas of northern Pakistan. Journal of Quaternary Science, 15: 283-297.

[24] Rost K T, 1994. Paleoclimatic field studies in and along the Qinling-shan (central China). Geojournal, 34(1): 107-120.

[25] Sch?fer J M, Tschudi S, Zhao Z Z et al., 2001. The limited influence of glaciations in Tibet on global climate over the past 170000 yr. Earth and Planetary Science Letters, 194: 287-297.

[26] Shi Y F, Cui Z J, Li J J et al., 1989. Problems of Quaternary Glaciation and Environment in China. Beijing: Science Press, 1-364.

[27] Shi Y F, 2002. Characteristics of late Quaternary monsoon glaciation on the Tibetan Plateau and in East Asia, Quaternary International, 97/98: 79-91.

[28] Shi Y F, Yao T D, 2002. MIS3b (54-44ka BP) cold period and glacial advance in middle and low latitudes. Journal of Glaciology and Geocryology, 24(1): 1-9. (in Chinese)

[29] Su Z, 1984. Discussing about the Quaternary glacial problems of Lushan from the results of modern glaciers in China. Journal of Glaciology and Geocryology, 6(2): 141-153. (in Chinese)

[30] Tsukada M, 1967. Vegetation in subtropical Formosa paleo-climate. Palaeogeography Palaeoclimatology Palaeoecology, 7(3): 49-64.

[31] Velichko A A, Konono Y M, Faustova M A et al., 1997. The last glaciation of earth: size and volume of ice-sheets. Quaternary International, 41/42: 43-51.

[32] Wang J T, 1981. Ancient glaciers at the head of Urumqi River, Tian Shan. Journal of Glaciology and Cryopedology, 3: 55-63. (in Chinese)

[33] Wu X H, 1985. Some problems about the glacial remains and the glacial developmental condition. In: Proceedings of the Chinese Quaternary Glacial and Periglacial Symposium. Beijing: Science Press, 143-148. (in Chinese)

[34] Xie C L, Jian Z M, Zhao Q H et al., 1996. The paleogeographic configuration of China seas and its climatic influence during the Last Glacial Maximum. Quaternary Sciences, (2): 1-9. (in Chinese)

[35] Yi C L, Liu K X, Cui Z J, 1998. AMS dating on glacial tills at the source area of Urumqi River in the Tianshan Mountains and its implications. Chinese Science Bulletin, 43: 1749-1751.

[36] Yi C L, Jiao K Q, Liu K X et al., 2001, ESR dating on tills and the Last Glaciation at the headwaters of the Urumqi river, Tianshan Mountains, China. Journal of Glaciology and Geocryology, 23(4): 389-393. (in Chinese)

[37] Zhang W, Cui Z J, 2003. Glaciation sequences of the Last Glaciation in Gongwangshan and Jiaozishan Mountain in northeastern Yunnan Province. Research of Soil and Water Conservation, 10(3): 94-96. (in Chinese)

[38] Zhao J D, Zhou S Z, Shi Z T et al., 2001. ESR dating of glacial tills of Baishuihe River on the southern slope of Lenglongling in the eastern part of Qilian Mountains. Journal of Lanzhou University, 37: 110-117. (in Chinese)

[39] Zhao J D, Zhou S Z, Cui J X et al., 2002. ESR dating of glacial tills at the headwaters of the Urumqi River in the Tianshan Mountains. Journal of Glaciology and Geocryology, 24: 737-743. (in Chinese)