云南千湖山第四纪冰川发育特点与环境变化

doi:10.11821/xb201205008

Abstract

Abstract: The Qianhu Mountain, one of the regions with Quaternary glacial remains in the Hengduan Mountains, is intensively influenced by the southwestern monsoon and has the important scientific significance in the research not only on glacial characteristics in western and eastern China, but also on the relationship between the climate change and tectonic uplift in the bordering mountains of eastern Tibetan Plateau. Field investigations show that the Quaternary erosion and sediment geomorphology are preserved above 3500 m in the main peak of the Qianhu Mountains and its surrounding areas. Glaciers mainly depended on the planation surface (3900-4000 m) and its relevant valleys, and the glacier type belongs to the small ice cap and the valley glacier entered the branch valley. Using geomorphology method and the lab optically stimulated luminescence (OSL) dating of glacial periods, this paper confirms the glacial advance only occurred during the last glacial cycle (LGC), that is, last glacial maximum (LGM, 22.2 ± 1.9 kaBP) in the mid-last glacial cycle (MIS3b, 37.3 ± 3.7 kaBP, 45.6 ± 4.3 kaBP), and in the early stage of last glacial cycle (MIS4). The glacial extent of the MIS3b is larger than that of last glacial maximum. This might be caused by different climate events alternated with wet and dry conditions during different glacial stages. Compared with the multi-glacier sequences in the Hengduan Mountains, the Qianhu Mountain only experienced the glacial advance during the last glacial cycle. It is the tectonic uplift coupled with the climate change that led the Qianhu Mountain to the snowline and witnessed the glacial advance.

Key words: Qianhu Mountain, last glacial cycle, tectonic uplift, stimulated luminescence dating

ZHANG Wei, LIU Beibei, LI Yonghua, FENG Jun, ZHANG Bing, WANG Zhilin, LI Dapeng. Quaternary Glacier Development and Environmental Evolution in Qianhu Mountain, Northwestern Yunnan Province[J].Acta Geographica Sinica, 2012, 67(5): 657-670.

References

[1] Li Jijun. Glaciers in the Hengduan Mountains. Beijing: Science Press, 1996: 157-172. [李吉均. 横断山冰川. 科学出版社, 1996: 157-160.]
[2] Xie Youyu, Cui Zhijiu. Yulong Mountains in north Yunnan//Shi Yafeng, Cui Zhijiu, Li Jijun et al.//Problems ofQuaternary Glaciers and Environment in East China. Beijing: Science Press, 1989: 106-119. [谢又予, 崔之久. 滇北玉龙山//施雅风, 崔之久, 李吉均等. 中国东部第四纪冰川与环境问题. 北京: 科学出版社, 1989: 106-119.]
[3] Ren Meie, Liu Zhenzhong, Yong Wanli et al. A primary study on geomorphology of Lijiang and Yulong mountain.Journal of Yunan University: Natural Sciences, 1957, 4: 9-18. [任美锷, 刘振中, 雍万里等. 丽江和玉龙山地貌的初步研究. 云南大学学报: 自然科学版, 1957, 4: 9-18.]
[4] Credner W. Observations on geology and morphology of Yunnan. Geological Survey of Kwangtung and Kwangsi(special publication), 1932, 10: 1-53.
[5] Huang Peihua. Discussing the Yunnan geomorphological research. Quaternaria Sinica, 1960, 3(1/2): 39-55. [黄培华. 论云南之地貌发育问题. 中国第四纪研究, 1960, 3(1/2): 39-55.]
[6] Wisman H V. The Pleistocence glaciation in China. Bulletin of the Geological Society of China, 1937, 17(2): 145-168.
[7] Yang Huairen, Xu Xin. Quaternary environmental changes in eastern China. Journal of Nanjing University: NaturalSciences, 1980, (1): 121-147. [杨怀仁, 徐馨. 中国东部第四纪自然环境的演变. 南京大学学报: 自然科学版, 1980,(1): 121-147.]
[8] Ou Xianjiao, Zeng Lanhua, Long Hao et al. Applicability of dating the quartz from the tills of Last Glacial in theHengduan Mountains. Journal of Glaciology and Geocryology, 2011, 33(1): 110-117. [欧先交, 曾兰华, 隆浩等. 横断山地区末次冰期冰碛物石英光释光测年的适应性. 冰川冻土, 2011, 33(1): 110-117.]
[9] Xu Liubing, Ou Xianjiao. Timing and style of Late Pleistocene glaciation in the Queer Shan, northern HengduanMountains in the eastern Tibetan Plateau. Journal of Quaternary Science, 2010, 25(6): 957-966.
[10] Wang Jian, Raisbeck G, Xu Xiaobin et al. Study on the 10Be dating of the glacial remains in the southern Shalulishanin the southeastern Tibet Plateau. Science in China: Series D, 2006, 36(8): 706-712. [王建, Raisbeck G, 徐孝彬. 青藏高原东南部沙鲁里山南端第四纪冰川作用的10Be年代学研究. 中国科学: D辑, 2006, 36(8): 706-712.]
[11] Zheng Benxing. Quaternary glaciation and glacier evolution in the Yulong Mount, Yunnan. Journal of Glaciology andGeocryology, 2000, 22(1): 58-61. [郑本兴. 云南玉龙雪山第四纪冰期与冰川演化模式. 冰川冻土, 2006, 36(8):706-712.]
[12] Zhao Xitao, Zhang Yongshuang, Qu Yongxin et al. Pleistocene glaciations along the western foot of the YulongMountains and their relationship with the formation and development of the Jinsha River. Quaternary Sciences, 2007,27(1): 35-44. [赵希涛, 张永双, 曲永新等. 玉龙山西麓更新世冰川作用及其与金沙江河谷发育的关系. 第四纪研究,2007, 27(1): 35-44.]
[13] Zhao Xitao, Qu Yongxin, Li Tiesong. Pleistocene glaciations along the eastern foot of Yulong Mountains. Journal ofGlaciology and Geocryology, 1999, 21(3): 242-248. [赵希涛, 曲永新, 李铁松. 玉龙山东麓更新世冰川作用. 冰川冻土, 1999, 21(3): 242-248.]
[14] Yang Jianqing, Cui Zhijiu, Yi Chaolu et al. About the Dali glaciation in Diancang Mountain. Science in China: SeriesD, 2007, 37(9): 1205-1211. [杨建强, 崔之久, 易朝路等. 关于点苍山“大理冰期”. 中国科学: D辑, 2007, 37(9):1205-1211.]
[15] Yang J Q, Zhang W, Cui Z J et al. Climate change since 11.5 ka on the Diancang massif on the southeastern marginof the Tibetan Plateau. Quaternary Research, 2010, 73: 304-312.
[16] Yang J Q, Zhang W, Cui Z J et al. Late Pleistocene glaciation of the Diancang and Gongwang Mountains, southeastmargin of the Tibetan Plateau. Quaternary International, 2006, 154/155: 52-62.
[17] Chen Qinluan, Zhao Weicheng. Aerial Images observation of glacial landforms at Diancang Mt. Dali, Yunnan. YunnanGeographic Environment Research, 1997, 9(2): 66-73. [陈钦峦, 赵维城. 从航片上观察点苍山冰川地貌.云南地理环境研究, 1997, 9(2): 66-73.]
[18] Kuang Mingsheng, Zhao Weicheng. Study on ESR dating of depositional stratums of late Pleistocene epoch inDiancangshan area about Dali city in Yunnan Province. Yunnan Geographic Environment Research, 1997, 9(1):49-57. [况明生, 赵维城. 云南大理点苍山地区更新世晚期沉积地层的ESR 测年研究. 云南地理环境研究, 1997, 9(1): 49-57.]
[19] Wan Ye, Han Tianding, Zhu Jing et al. A study on geomorphological development and Quaternary palaeoglaciation ofthe Diancangshan-Luopingshan in western Yunnan. Tropical Geography, 2003, 23(4): 304-308. [万晔, 韩添丁, 朱静等. 云南点苍山—罗坪山地区地貌发育与第四纪冰川作用. 热带地理, 2003, 23(4): 304-308.]
[20] Iwata I, Yagi H, Feng Y Z. Glacial extent and ELAs during the Last Glacial period in Yunnan Province, China//Proceedings of International Symposium on Paleo-environmental Change in Tropical-subtropical Monsoon Asia.Special Publication, 1995, (24): 113-123.
[21] Zhou Shangzhe, Xu Liubing, Cui Jianxin et al. Quaternary glacial geomorphological development and environmentalchange in Shalulishan. Chinese Science Bulletin, 2004, 49(23): 2480-2484. [周尚哲, 许刘兵, 崔建新等. 沙鲁里山第四纪地貌发育与环境演变. 科学通报, 2004, 49(23): 2480-2484.]
[22] Zheng Benxing, Ma Qiuhua. A study on the geomophological characteristics and glaciations in paleo-Daocheng icecap, western Sichuan. Journal of Glaciology and Geocryology, 1995, 17(1): 23-32. [郑本兴, 马秋华. 川西稻城古冰帽的地貌特征与冰期探讨. 冰川冻土, 1995, 17(1): 23-32.]
[23] Cui Zhijiu, Wu Yongqiu, Liu Gengnian et al. On Kunlun-Yellow River tectonic movement. Science in China: SeriesD, 1998, 28(1): 53-59. [崔之久, 吴永秋, 刘耕年等. 关于“昆仑—黄河运动”. 中国科学: D辑, 1998, 28(1): 53-59.]
[24] Cui Zhijiu, Wu Yongqiu, Liu Gengnian. Discovery of the Kunlun-Huanghe movement and its nature. Chinese ScienceBulletin, 1997, 42(18): 1986-1989. [崔之久, 吴永秋, 刘耕年. 昆仑—黄河运动的发现及其性质. 科学通报, 1997, 42(18): 1986-1989.]
[25] Li Jijun, Fang Xiaomin, Ma Haizhou et al. Landform evolution on the upper reaches of the Yellow River and uplift inQinghai-Xizang Plateau since late Pliocene. Science in China: Series D, 1996, 26(4): 316-322. [李吉均, 方小敏, 马海洲等. 晚新生代黄河上游地貌演化与青藏高原隆起. 中国科学: D辑, 1996, 26(4): 316-322.]
[26] Li Jijun, Fang Xiaomin, Pan Baotian et al. Late Cenozoic intensive uplift of Qinghai-Xizang Plateau and its impactson environments in surrounding area. Quaternary Sciences, 2001, 21(5): 381-391. [李吉均, 方小敏, 潘保田等. 新生代晚期青藏高原强烈隆起及其对周边环境的影响. 第四纪研究, 2001, 21(5): 381-391.]
[27] Li Jijun, Fang Xiaomin. Uplift of Qinghai-Xizang Plateau and study on the changes of the environment. Chinese Science Bulletin, 1998, 43(15): 1569-1574. [李吉均, 方小敏. 青藏高原隆起与环境变化研究. 科学通报, 1998, 43(15): 1569-1574.]
[28] Zhou S Z, Wang X, Wang J et al. A preliminary study on timing of the oldest Pleistocene glaciation inQinghai-Xizang Plateau. Quaternary International, 2006, 154-155: 44-51.
[29] Shi Yafeng. Evolution of the cryosphere in the Tibetan Plateau, China, and its relationship with the global change inthe mid-Quaternary. Journal of Glaciology and Geocryology, 1998, 20(3): 197-208. [施雅风. 第四纪中期青藏高原冰冻圈的演化及其与全球变化的联系. 冰川冻土, 1998, 20(3): 197-208.]
[30] Shi Yafeng, Li Jijun, Li Bingyuan et al. Uplift of the Qinghai-Xizang (Tibetan) Plateau and East Asia environmentalchange during late Cenozoic. Acta Geographica Sinica, 1999, 54(1): 10-20. [施雅风, 李吉均, 李炳元等. 晚新生代青藏高原的隆升与东亚环境变化. 地理学报, 1999, 54(1): 10-20.]
[31] Cui Zhijiu, Chen Yixin, Zhang Wei et al. Research history, glacial chronology and origins of Quaternary glaciations inChina. Quaternary Sciences, 2011, 31(5): 1-16. [崔之久, 陈艺鑫, 张威等. 中国第四纪冰期历史、特征及成因探讨.第四纪研究, 2011, 31(5): 1-16.]
[32] Shi Yafeng, Cui Zhijiu. The Quaternary Glaciations and Environmental Variations in China. Shijiazhuang: HebeiScience and Technology Publishing House, 2006: 557. [施雅风, 崔之久. 中国第四纪冰川与环境变化. 石家庄: 河北科学技术出版社, 2006: 557.]
[33] Zhao Xitao, Zheng Mianping, Li Daoming. Formation and evolution of the ancient "Lake Xiaozhongdian" in Diqing,Yunnan and its relationship with development of the ancient "Lake Shigu" and the modern valley of the Jinsha River.Acta Geologica Sinica, 2007, 81(12): 1645-1651. [赵希涛, 郑绵平, 李道明. 云南迪庆小中甸古湖的形成演化及其与石鼓古湖和金沙江河谷发育的关系. 地质学报, 2007, 81(12): 1645-1651.]
[34] Zhang Yiguang. Climatic division of the Hengduan mountainous region. Mountain Research, 1989, 7(1): 21-28. [张谊光. 横断山区气候规划. 山地研究, 1989, 7(1): 21-28.]
[35] Ming Qingzhong, Su Huai, Shi Zhengtao et al. Last five Heinrich events revealed by lacustrine sediments fromXiaozhongdian Basin in Yunnan Province. Acta Geographica Sinica, 2011, 66(1): 123-130. [明庆忠, 苏怀, 史正涛等.云南小中甸盆地湖相沉积记录最近的5 次Heinrich事件. 地理学报, 2011, 66(1): 123-130.]
[36] Cui Z J, Yang C F, Liu G N et al. The Quaternary glaciation of Shesan Mountain in Taiwan and glacial classificationin monsoon areas. Quaternary International, 2002, 97-98: 147-153.
[37] Zhang W, Cui Z J, Feng J L et al. Late Pleistocene glaciation of the Hulifang massif of Gongwang Mountains. Journalof Geographical Sciences, 2005, 15(4): 448-458.
[38] Yi Chaolu, Liu Kexin, Cui Zhijiu. AMS dating and significance of the glacial tills since the Last Glacial Cycle inUrumqi River, Tian Shan. Chinese Science Bulletin, 1998, 43(6): 655-656. [易朝路, 刘克新, 崔之久. 天山乌鲁木齐河河源末次冰期以来冰川沉积物AMS测年及其意义. 科学通报, 1998, 43(6): 655-656.]
[39] Zhou Shangzhe, Xu Liubing, Colgan et al. Using cosmogenic nuclides ~10Be dating Guxiang Ice Stage and Baiyu IceStage. Chinese Science Bulletin, 2007, 52(8): 945-950. [周尚哲, 许刘兵, Colgan 等. 古乡冰期和白玉冰期的宇宙成因核素10Be测年. 科学通报, 2007, 52(8): 945-950.]
[40] Cui Z J, Yang J F, Liu G N et al. Discovery of Quaternary glacial evidence on Shesan Mountain in Taiwan, China.Chinese Science Bulletin, 2000, 45: 566-571.
[41] Murray A S, Wintle A G. Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol.Radiation Measurements, 2000, 32: 57-73.
[42] Murray A S, Wintle A G. The single aliquot regenerative dose protocol: Potential for improvements in reliability.Radiation Measurements, 2003, 37: 377-381.
[43] Rhodes E J. Observations of thermal transfer OSL signals in glacigenic quartz. Radiation Measurements, 2000, 32:595-602.
[44] Lu Y C, Wang X L, Wintle A G. A new OSL chronology for dust accumulation in the last 130, 000 yr for the ChineseLoess Plateau. Quaternary Research, 2000: 1-9.
[45] Wang Xulong, Lu Yanchou, Li Xiaoni. Luminescence dating of fine-grained quartz in Chinese loess-simplifiedmultiple aliquot regenerative-dose (MAR) protocol. Seismology and Geology, 2005, 27(4): 615-623. [王旭龙, 卢演俦,李晓妮. 细颗粒石英光释光测年简单多片再生法. 地震地质, 2005, 27(4): 615-623.]
[46] Liu Shuzhen, Chai Zongxin. Geomorphologic characteristics in Hengduan Mountain region. Exploration of Nature,1986, 15(1): 139-143. [刘淑珍, 柴宗新. 横断山区地貌特征. 大自然探索, 1986, 15(1): 139-143.]
[47] Xu Liubing, Zhou Shangzhe, Wang Jie. Pleistocene glaciations in the Shaluli Shan and the influences of southwestmonsoon on the glaciations during the last glacial period. Quaternary Sciences, 2005, 25(5): 620-629. [许刘兵, 周尚哲, 王杰. 沙鲁里山更新世冰川作用及西南季风波动对末次冰期冰川作用的影响. 第四纪研究, 2005, 25(5):620-629.]
[48] Wang Zhilin. Glaciers and environment of Helan Mountain [D]. Dalian: Liaoning Normal University, 2011: 31-34. [王志麟. 贺兰山的冰川与环境[D]. 大连: 辽宁师范大学, 2011: 31-34.]
[49] Rost K T. Plaeoclimate field studies in and along the Qinling Shan (central China). GeoJournal, 1994, 34(1): 102-120.
[50] Zhang W, Cui Z J, Li Y H. Review of the timing and extent of glaciers during the last glacial cycle in the borderingmountains of Tibet and in East Asia. Quaternary International, 2006, 154-155: 32-43.
[51] Shi Yafeng, Zheng Benxing, Li Shijie et al. Studies on altitude and climatic environment in the middle and east partsof Tibetan Plateau during Quaternary Maximum Glaciation. Journal of Glaciology and Geocryology, 1995, 17(2):97-112. [施雅风, 郑本兴, 李世杰等. 青藏高原中东部最大冰期时代高度与气候环境探讨. 冰川冻土, 1995, 17(2):97-112.]
[52] He Kezhao, He Haosheng, Zhao Chonghe. Tectonic Evolution of Mesozoic-Cenozoic in Western Yunnan. Beijing:Seismological Press, 1993: 77-86. [何科昭, 何浩生, 赵崇贺. 滇西中新生代构造演化. 北京: 地震出版社, 1993:77-86.]
[53] He Kezhao, He Haosheng, Cai Hongbiao. Formation and evolution of the western Yunnan orogenic belt. GeologicalReview, 1996, 42(2): 97-105. [何科昭, 何浩生, 蔡红飙. 滇西造山带的形成与演化. 地质论评, 1996, 42(2): 97-105.]
[54] Shi Xuhua, Wang Erqi, Wang Gang et al. Late Cenozoic uplift of the Yulong Snow Mountain (5596 m) SE TibetanPlateau caused by erosion ad tectonic forcing. Quaternary Sciences, 2008, 28(2): 222-231. [石许华, 王二七, 王刚等.青藏高原东南缘玉龙雪山(5596m) 晚新生代隆升的侵蚀与构造控制作用. 第四纪研究, 2008, 28(2): 222-231.]
[55] Luo Jianning, Xiao Yonglin, Su Junzhou et al. The study of the uplift of Diancangshan MT and the molasse depositsat its piedmont. Contribution to the Geology of the Qinghai-Xizang (Tibet) Plateau, 1985, 17: 81-97. [罗建宁, 肖永林,苏俊周等. 滇西点苍山的抬升与山前磨拉石沉积. 青藏高原地质文集, 1985, 17: 81-97.]
[56] Wang Erqi, Fan Chun, Wang Gang et al. Deformational and geomorphic processes in the formation of the AilaoShan-Diancang range, west Yunnan. Quaternary Sciences, 2006, 26(2): 220-227. [王二七, 樊春, 王刚等. 滇西哀牢山-点苍山形成的构造和地貌过程. 第四纪研究, 2006, 26(2): 220-227.]
[57] Wu Zhonghai, Zhang Yongshuang, Hu Daogong et al. Discussion on the dynamical mechanism and effect for normalfault in late Quaternary of eastern Haba-Yulongxueshan fault. Science in China: Series D, 2008, 38(11): 1361-1375. [吴中海, 张永双, 胡道功等. 滇西北哈巴—玉龙雪山东麓断裂的晚第四纪正断层作用及其动力学机制探讨. 中国科学:D辑, 2008, 38(11): 1361-1375.]
[58] Han Zhujun, Guo Shunmin, Xiang Hongfa et al. Seismotectonic environment of occurring on February 3, 1996 Lijiangm =7.0 earthquake, Yunnan Province. Acta Seismologica Sinica, 2004, 26(4): 410-418. [韩竹军, 虢顺民, 向宏发等.1996 年2 月3 日云南丽江7.0级地震发生的构造环境. 地震学报, 2004, 26(4): 410-418.]
[59] Chen Fubin, Chen Jiliang, Xu Yifeng et al. The neotectonic analysis of the Quaternary deposits and sterpperdlandforms in Mt. Yunlongxueshan-Mt. Cang region. Acta Geographica Sinica, 1992, 47(5): 430-440. [陈富斌, 陈继良,徐毅峰等. 玉龙雪山—苍山地区第四纪沉积与层状地貌的新构造分析. 地理学报, 1992, 47(5): 430-440.]
[60] Li Xianggen, Ran Yongkang, Peng Gui et al. Active faults and their relationship with seismic activities in Dali ofYunnan Province and its adjacent regions. Seismology and Geology, 1986, 8(4): 51-61. [李祥根, 冉永康, 彭贵等. 云南大理及其邻近地区活断层和地震活动特征. 地震地质, 1986, 8(4): 51-61.]
[61] Li Jijun. Glacial relics of monsoonal Asia in the last glaciation. Quaternary Sciences, 1992, (4): 332-340. [李吉均. 季风亚洲末次冰期的古冰川遗迹. 第四纪研究, 1992, (4): 332-340.]
[62] Shi Yafeng, Yao Tandong. MIS3b (54~44 ka B.P.) cold period and glacial advance in middle and low latitudes. Journalof Glaciology and Geocryology, 2002, 24(1): 1-9. [施雅风, 姚檀栋. 中低纬度MIS3b (54-44 ka B.P.) 冷期与冰川前进. 冰川冻土, 2002, 24(1): 1-9.]
[63] Owen L A, Finkel R C, Caffee M W. A note on the extent of glaciation throughout the Himalaya during the globalLast Glacial Maximum. Quaternary Science Reviews, 2002, 21(1-3): 147-157.
[64] Berger A L. Long-term variations of caloric insolation resulting from the Earth s orbital elements. QuaternaryResearch, 1978, 9(2): 139-167.
[65] Pan Baotian, Wang Jianmin. Loess record of Qinghai-Xizang Plateau monsoon variations in the eastern part of theplateau since the last interglacial. Quaternary Sciences, 1999, (4): 330-335. [潘保田, 王建民. 末次间冰期以来青藏高原东部季风演化的黄土沉积记录. 第四纪研究, 1999, (4): 330-335.]
[66] Shi Yafeng, Yu Ge, Liu Xiaodong et al. Reconstruction of the 30~40 ka B. P. enhanced Indian monsoon climate basedon geological records from the Tibetan Plateau. Palaeogeography, Palaeoclimatology, Palaecology, 2011, 169(1/2):69-83.
[67] Shi Yafeng. Characteristics of Late Quaternary monsoonal glaciation on the Tibetan Plateau and in East Asia.Quaternary International, 2002, 97/98: 79-91.
[68] Yin Yong, Fang Nianqiao, Hu Chaoyong et al. Palaeo-environmental evolution deduced from organic carbon stable isotope compositions of Napahai Lake sediments in northwestern Yunnan, China. Journal of Lake Science, 2001, 13(4): 289-295. [殷勇, 方念乔, 胡超涌等. 云南中甸纳帕海古环境演化的有机碳同位素记录. 湖泊科学, 2001, 13(4):289-295.]

Quaternary Glacier Development and Environmental Evolution in Qianhu Mountain, Northwestern Yunnan Province

PDF (PC)

Like

Knowledge

Cited

Abstract

Cite this article

share this article

References

Related Articles 6

Metrics

Comments

[1]	Nairui WANG, Zhiyong HAN, Xusheng LI, Gang CHEN, Xianyan WANG, Huayu LU. Tectonic uplift of Mt. Lushan indicated by the steepness indices of the river longitudinal profiles [J]. Acta Geographica Sinica, 2015, 70(9): 1516-1525.
[2]	Shujian XU, Xinchao DING, Zhichao NI. The sedimentary characteristics of Buxi loess profile in Shandong Province and their paleoclimatic and palaeoenvironment significance [J]. Acta Geographica Sinica, 2014, 69(11): 1707-1717.
[3]	CHEN Yixin, ZHANG Mei, LI Chuanchuan, LI Yingkui, LIU Gengnian. Fluvial Incision Process and Its Tectonic Implications of Golmud River since Last Glaciation Maximum [J]. Acta Geographica Sinica, 2011, 66(11): 1540-1550.
[4]	ZHANG Wei,YAN Ling,CUI Zhijiu,YANG Jianqiang. Glacial Environment during the Last Glacial Cycle in the Mountains of East Asia [J]. Acta Geographica Sinica, 2009, 64(1): 33-42.
[5]	LI Dewen, CUI Zhijiu, LIU Gengnian. A Development Model of Red Weathering Crust on Limestones: an Example from Hunan, Guangxi, Guizhou, Yunnan and Tibet [J]. Acta Geographica Sinica, 2002, 57(3): 293-300.
[6]	Shi Yafeng, Li Jijun, Li Bingyuan, Yao Tandong, Wang Suming, Li Shijie, Cui Zhijiu, Wang Fubao, Pan Baotian, Fang Xiaomin, Zhang Qingsong . UPLIFT OF THE QINGHAI—XIZANG (TIBETAN) PLATEAU AND EAST ASIA ENVIRONMENTAL CHANGE DURING LATE CENOZOIC [J]. Acta Geographica Sinica, 1999, 54(1): 10-20.