新疆阿尔泰山东段冰碛物光释光测年研究

doi:10.11821/dlxb201805014

Abstract

Abstract:

The glacier is one of the most positive external forces for shaping the landscape of earth surface in alpine region. The geochronology study of glacial stratigraphy can provide insightful information about the ancient glacier process, which is sensitive to climate change. Compared to the sediments of ice lake and ice water terrace with complex material source, moraine is the direct product of glacial movement. Consequently, it can also reflect the glacier events that occurred in the past. The accurate dating of moraine can provide chronology evidence for improving the understanding of reconstruction of climate change patterns. The Altay Mountains is one of the major mountain ranges for understanding Quaternary glaciation in northwestern China. Most of the studies have focused on western Altay Mountains, Xinjiang. However, the chronology of the moraines in its eastern section is not well studied. In this study, OSL dating technique method was applied to determine the ages of the glacial moraine deposits of coarse grained quartz (90-125 μm) in the East Altay Mountains. According to analysis of the frequency distribution of De value and De(t) plots, most of the moraine samples showed partial bleaching. Therefore, the first-order kinetic equation was used to separate the CW-OSL curve into three component exponentials (fast, medium and slow components) and the fast components were used to determine these equivalent doses. The OSL dating results of moraines in East Altay Mountains deposited seperately in 32.33 ka, 16.07 ka, 8.41-8.07 ka, 6.83-6.48 ka and 4.62 ka. This implied that the glacier development process was identified with MIS3, MIS2, 8.2 ka Cold Events, Holocene Optimum and Neoglaciation, respectively. Observably, moraine can occur with glacial advance or recession during the warm or cold climate episodes, while the development of glaciers in the Altay Mountains was closely related to global climate change. This study demonstrates the successful application of quartz OSL with fast component signal to glacial sediments from the Altay Mountains. Furthermore, it can complement the geochronology data for moraine sedimentary records to reveal the glacier evolution history in the whole Altay Mountains region since 32 ka BP.

Key words: Altay Mountains, moraines, OSL dating, glacial movement

JIA Binbin,ZHOU Yali,ZHAO Jun. Optically stimulated luminescence dating of moraines in East Altay Mountains, Xinjiang[J].Acta Geographica Sinica, 2018, 73(5): 957-972.

References

[1]	Shi Yafeng, Liu Shiyin.The calculation of Chinese glacier's response to the globe climatic warming in the 21st century. Chinese Science Bulletin, 2000, 45(4): 434-438.
[1]	[施雅风, 刘时银. 中国冰川对 21 世纪全球变暖响应的预估. 科学通报, 2000, 45(4): 434-438.]http://www.cqvip.com/QK/94252X/200004/4231523.html
[2]	Augustin L, Barbante C, Barnes P R F, et al. Eight glacial cycles from an Antarctic ice core. Nature, 2004, 429(6992): 623-628.http://www.nature.com/doifinder/10.1038/nature02599
[3]	Rasmussen S O, Andersen K K, Svensson A M, et al.A new Greenland ice core chronology for the last glacial termination. Journal of Geophysical Research Atmospheres, 2006, 111(D6): 907-923.http://onlinelibrary.wiley.com/doi/10.1029/2005JD006079/abstract
[4]	Richards B.Luminescence dating of Quaternary sediments in the Himalaya and High Asia: A practical guide to its use and limitations for constraining the timing of glaciation. Quaternary International, 2000, 65(99): 49-61.http://www.sciencedirect.com/science/article/pii/S1040618299000361
[5]	Hu G, Yi C, Zhang J, et al.Late Quaternary glacial advances in the eastern Qilianshan, north-eastern Tibet, as inferred from luminescence dating of fluvioglacial sediments. Journal of Quaternary Science, 2016, 31(6): 587-597.http://doi.wiley.com/10.1002/jqs.v31.6
[6]	Cui Zhijiu, Yi Chaolu, Yan Jinfu.Quaternary glaciations in the Halasi River catchment and its surroundings in the Altai Mountains in Xinjiang, China. Journal of Glaciology and Geocryology, 1992, 14(4): 342-351.
[6]	[崔之久, 易朝路, 严竞浮. 新疆阿尓泰山喀纳斯河流域及其邻域第四纪冰川作用. 冰川冻土, 1992, 14(4): 342-351.]
[7]	Li Huhou.Aspect of luminescence dating. Quaternary Sciences, 1997, 17(3): 248-257.
[7]	[李虎侯. 释光技术测定年龄的现况. 第四纪研究, 1997, 17(3): 248-257.]
[8]	Xu Xiangke, Yang Jianqiang, Dong Guocheng, et al.OSL dating of glacier extent during the Last Glacial and the Kanas Lake basin formation in Kanas River valley, Altai Mountains, China. Geomorphology, 2009, 112(3): 306-317.http://linkinghub.elsevier.com/retrieve/pii/S0169555X09002554
[9]	Xu Xiangke.Late Pleistocene glacial geomorphology and dating in Kanas River valley, Altai Mountians [D]. Beijing: Graduate University of Chinese Academy of Sciences, 2010.
[9]	[许向科. 阿尔泰山喀纳斯河流域晚更新世冰川地貌与冰期序列测年[D]. 北京: 中国科学院研究生院, 2010.]
[10]	Jiang Heli, Zhao Jingdong, Yin Xiufeng, et al.New OSL chronology of the Last Glaciation in Kanas River Valley, Altay Mountains, China. Journal of Glaciology and Geocryology, 2012, 34(2): 304-310.
[10]	[江合理, 赵井东, 殷秀峰, 等. 阿尔泰山喀纳斯河流域末次冰期 OSL 年代学新证. 冰川冻土, 2012, 34(2): 304-310.]http://www.cqvip.com/QK/93756X/201202/41729606.html
[11]	Jiang Heli.A study on Quaternary glacial evolution sequences in the Kanas River, Altai Mountains [D]. Lanzhou: Northwest Normal University, 2012.
[11]	[江合理. 阿尔泰山喀纳斯河流域第四纪冰川演化序列: 基于光释光测年技术[D]. 兰州: 西北师范大学, 2012.]
[12]	Feng Jun.The application of remote sensing technology in the 1:50000 regional geology and mineral resources survey, Wuqiliketawu, Xinjiang [D]. Urumqi: Xinjiang University, 2014.
[12]	[凤骏. 遥感技术在新疆乌齐里克它乌一带1:5万区域地质矿产调查中的应用[D]. 乌鲁木齐: 新疆大学, 2014.]
[13]	Wang Lilun, Liu Chaohai, Wang Ping.Modern glaciers in Altay Mountains of China. Acta Geographica Sinica, 1985, 40(2): 142-154.
[13]	[王立伦, 刘潮海, 王平. 中国阿尔泰山的现代冰川. 地理学报, 1985, 40(2): 142-154.]
[14]	Qu Wenjun, Zhang Xiaoye, Wang Dan, et al.The important significance of westerly wind study. Marine Geology & Quaternary Geology, 2004, 24(1): 125-132.
[14]	[屈文军, 张小曳, 王丹, 等. 西风带研究的重要意义. 海洋地质与第四纪地质, 2004, 24(1): 125-132.]http://www.cqvip.com/Main/Detail.aspx?id=9193834
[15]	Chen Fahu, Chen Jianhui, Huang Wei.A discussion on the westerly-dominated climate model in mid-latitude Asia during the modern interglacial period. Earth Science Frontiers, 2009, 16(6): 23-32.
[15]	[陈发虎, 陈建徽, 黄伟. 中纬度亚洲现代间冰期气候变化的“西风模式”讨论. 地学前缘, 2009, 16(6): 23-32.]http://d.wanfangdata.com.cn/Periodical/dxqy200906003
[16]	Prescott J R, Hutton J T.Cosmic ray contributions to dose rates for luminescence and ESR dating: Large depths and long-term time variations. Radiation Measurements, 1994, 23(2-3): 497-500.http://linkinghub.elsevier.com/retrieve/pii/1350448794900868
[17]	Murray A S, Wintle A G.Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol. Radiation Measurements, 2000, 32(1): 57-73.http://linkinghub.elsevier.com/retrieve/pii/S135044879900253X
[18]	Wintle A G, Murray A S.Luminescence sensitivity changes in quartz. Radiation Measurements, 1999, 30(1): 107-118.http://linkinghub.elsevier.com/retrieve/pii/S1350448798000961
[19]	Wintle A G, Murray A S.A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols. Radiation Measurements, 2006, 41(4): 369-391.http://linkinghub.elsevier.com/retrieve/pii/S1350448705003227
[20]	Galbraith R F, Roberts R G.Statistical aspects of equivalent dose and error calculation and display in OSL dating: An overview and some recommendations. Quaternary Geochronology, 2012, 11(8): 1-27.http://linkinghub.elsevier.com/retrieve/pii/S1871101412000957
[21]	Zhang Yuzhu, Huang Chunchang, Pang Jiangli, et al.OSL dating of the sediment stratigraphy of the Lajia Ruins in the Guanting Basin in the Upper Yellow River Basin. Acta Geographica Sinica, 2013, 68(5): 626-639.
[21]	[张玉柱, 黄春长, 庞奖励, 等. 黄河上游官亭盆地喇家遗址地层光释光测年研究. 地理学报, 2013, 68(5): 626-639.]
[22]	Alexanderson H, Murray A S.Was southern Sweden ice free at 19-25 ka, or were the post LGM glacifluvial sediments incompletely bleached? Quatemary Geochronology, 2007, 2(1-4): 229-236.http://linkinghub.elsevier.com/retrieve/pii/S1871101406000434
[23]	Alexanderson H.Residual OSL signals from modern Greenlandic river sediments. Geochronometria, 2007, 26(1): 1-9.http://www.degruyter.com/view/j/geochr.2007.26.issue--1/v10003-007-0001-6/v10003-007-0001-6.xml
[24]	Tsukamoto S, Asahi K, Watanabe T, et al. Timing of past glaciations in Kanchenjunga Himal, Nepal by optically stimulated luminescence dating of tills. Quaternary International, 2002, 97/98(2): 57-67.http://linkinghub.elsevier.com/retrieve/pii/S1040618202000514
[25]	Zhang Zhigang, Wang Jian, Lai Zhongping, et al.Problems and analyses of optically stimulated luminescence studies of glacial deposits from Daocheng ice cap, Sichuan, China. Acta Geologica Sinica, 2012, 86(4): 602-610.
[25]	[张志刚, 王建, 赖忠平, 等. 稻城冰帽冰碛物光释光测年研究中遇到的问题及探讨. 地质学报, 2012, 86(4): 602-610.]http://d.wanfangdata.com.cn/Periodical/dizhixb201204006
[26]	Hebenstreit R, Ivy-Ochs S, Kubik P W, et al.Lateglacial and early Holocene surface exposure ages of glacial boulders in the Taiwanese high mountain range. Quaternary Science Reviews, 2011, 30(3/4): 298-311.http://linkinghub.elsevier.com/retrieve/pii/S0277379110003987
[27]	Fuchs M, Wagner G A.Recognition of insufficient bleaching by small aliquots of quartz for reconstructing soil erosion in Greece. Quaternary Science Reviews, 2003, 22(10): 1161-1167.http://linkinghub.elsevier.com/retrieve/pii/S0277379103000398
[28]	Zhang J F, Zhou L P, Yue S Y.Dating fluvial sediments by optically stimulated luminescence: Selection of equivalent doses for age calculation. Quaternary Science Reviews, 2003, 22(10-13): 1123-1129.http://linkinghub.elsevier.com/retrieve/pii/S0277379103000544
[29]	Huntley D J, Godfreysmith D I, Thewalt M L W. Optical dating of sediments. Nature, 1985, 313(5998): 105-107.http://www.nature.com/doifinder/10.1038/313105a0
[30]	Bailey R M, Singarayer J S, Ward S, et al.Identification of partial resetting using De as a function of illumination time. Radiation Measurements, 2003, 37(4): 511-518.http://linkinghub.elsevier.com/retrieve/pii/S1350448703000635
[31]	Bailey R M.Paper I: The use of measurement-time dependent single-aliquot equivalent-dose estimates from quartz in the identification of incomplete signal resetting. Radiation Measurements, 2003, 37(6): 673-683.http://linkinghub.elsevier.com/retrieve/pii/S1350448703000787
[32]	Singarayer J S, Bailey R M.Component-resolved bleaching spectra of quartz optically stimulated luminescence: Preliminary results and implications for dating. Radiation Measurements, 2004, 38(1): 111-118.http://linkinghub.elsevier.com/retrieve/pii/S1350448703002506
[33]	Li S H, Li B.Dose measurement using the fast component of LM-OSL signals from quartz. Radiation Measurements, 2006, 41(5): 534-541.http://linkinghub.elsevier.com/retrieve/pii/S1350448705003318
[34]	Bulur E.An alternative technique for optically stimulated luminescence (OSL) experiment. Radiation Measurements, 1996, 26(5): 701-709.http://linkinghub.elsevier.com/retrieve/pii/S1350448797828843
[35]	Gu Hongliang, Huang Chunchang, Zhou Yali, et al.OSL dating of the eolian loess and palaeosol on the low terrace land in the upper Hanjiang River valley. Quaternary Sciences, 2012, 32(3): 516-526.
[35]	[顾洪亮, 黄春长, 周亚利, 等. 江上游湖北段低阶地风成黄土—古土壤释光测年研究. 第四纪研究, 2012, 32(3): 516-526.]
[36]	Agatova A R, Nazarov A N, Nepop R K, et al.Holocene glacier fluctuations and climate changes in the southeastern part of the Russian Altai (South Siberia) based on a radiocarbon chronology. Quaternary Science Reviews, 2012, 43(12): 74-93.http://linkinghub.elsevier.com/retrieve/pii/S0277379112001539
[37]	Zhang Wei, Fu Yanjing, Liu Beibei, et al.Geomorphological process of late Quaternary glaciers in Kanas River Valley of the Altay Mountains. Acta Geographica Sinica, 2015, 70(5): 739-750.
[37]	[张威, 付延菁, 刘蓓蓓, 等. 阿尔泰山喀纳斯河谷晚第四纪冰川地貌演化过程. 地理学报, 2015, 70(5): 739-750.]http://d.wanfangdata.com.cn/Periodical/dlxb201505006
[38]	Bond G, Broecker W, Johnsen S, et al.Correlations between climate records from North Atlantic sediments and Greenland ice. Nature, 1993, 365(6442): 143-147.http://www.nature.com/doifinder/10.1038/365143a0
[39]	Bond G, Showers W, Cheseby M, et al.A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates. Science, 1997, 278(5341): 1257-1266.http://www.sciencemag.org/cgi/doi/10.1126/science.278.5341.1257
[40]	Imbrie J, Hays J D, Martinson D G, et al.The orbital theory of Pleistocene climate: Support from a revised chronology of the marine δ18O record. Milankovitch & Climate Part, 1984, 126(1): 269-305.
[41]	Yang Bao, Shi Yafeng.Warm-humid climate in northwest China during the period of 40~30 ka B.P.: Geological records and origin. Quaternary Sciences, 2003, 23(1): 60-68.
[41]	[杨保, 施雅风. 40~30 ka B.P.中国西北地区暖湿气候的地质记录及成因探讨. 第四纪研究, 2003, 23(1): 60-68.]http://d.wanfangdata.com.cn/Periodical/dsjyj200301007
[42]	Ma Yuzhen, Zhang Hucai, Li Jijun.Environment during late Pleistoncence in Tengger Desert, China. Acta Botanica Sinica, 1998, 40(9): 871-879.
[42]	[马玉贞, 张虎才, 李吉均. 腾格里沙漠晚更新世孢粉植物群与气候环境演变. 植物学报, 1998, 40(9): 871-879.]http://d.wanfangdata.com.cn/Periodical/zwxb199809016
[43]	Rhodes T E, Gasse F, Lin R, et al.A Late Pleistocene-Holocene lacustrine record from Lake Manas, Zunggar (northern Xinjiang, western China). Palaeogeography Palaeoclimatology Palaeoecology, 1996, 120(1-2): 105-121.http://linkinghub.elsevier.com/retrieve/pii/0031018295000372
[44]	Pachur H J, Wünnemann B, Zhang H.Lake Evolution in the Tengger Desert, northwestern China, during the last 40,000 years. Quaternary Research, 1995, 44(2): 171-180.https://www.cambridge.org/core/product/identifier/S0033589400024364/type/journal_article
[45]	Li Bingyuan.The last greatest lakes on the Xizang (Tibetan) Plateau. Acta Geographica Sinica, 2000, 55(5): 174-182.
[45]	[李炳元. 青藏高原大湖期. 地理学报, 2000, 55(5): 174-182.]
[46]	Jiang Qingfeng, Qian Peng, Zhou Tong, et al.Preliminary research on ancient lacustrine sediments in Lake Ulungur in arid Central Asia since late MIS-3. Journal of Lake Sciences, 2016, 28(2): 444-454.
[46]	[蒋庆丰, 钱鹏, 周侗, 等. MIS-3晚期以来乌伦古湖古湖相沉积记录的初步研究. 湖泊科学, 2016, 28(2): 444-454.]http://d.wanfangdata.com.cn/Periodical/hpkx201602025
[47]	Long Hao, Shen Ji.Underestimated 14C-based chronology of late Pleistocene high lake-level events over the Tibetan Plateau and adjacent areas: Evidence from the Qaidam Basin and Tengger Desert. Science China: Earth Sciences, 2015, 45(1): 52-65.
[47]	[隆浩, 沈吉. 青藏高原及其邻区晚更新世高湖面事件的年代学问题: 以柴达木盆地和腾格里沙漠为例. 中国科学: 地球科学, 2015, 45(1): 52-65.]
[48]	Liu X J, Lai Z P, Fan Q S, et al.Timing for high lake levels of Qinghai Lake in the Qinghai-Tibetan Plateau since the last Interglaciation based on quartz OSL dating. Quaternary Geochronology, 2010, 5(2): 218-222.http://linkinghub.elsevier.com/retrieve/pii/S1871101409000624
[49]	Mao Peini, Pang Jiangli, Huang Chunchang, et al.Climate change during the late stages of MIS 3 period inferred from the loess record in the upper record in the upper Hanjiang River Valley. Quaternary Sciences, 2017, 37(3): 535-547.
[49]	[毛沛妮, 庞奖励, 黄春长, 等. 汉江上游黄土记录的 MIS 3 晚期气候变化特征. 第四纪研究, 2017, 37(3): 535-547.]http://www.dsjyj.com.cn/EN/Y2017/V37/I3/535
[50]	Shi Yafeng, Zheng Benxing, Yao Tandong.Glaciers and environments during the Last Glacial Maximum (LGM) on the Tibetan Plateau. Journal of Glaciology and Geocryology, 1997, 19(2): 97-113.
[50]	[施雅风, 郑本兴, 姚檀栋. 青藏高原末次冰期最盛时的冰川与环境. 冰川冻土, 1997, 19(2): 97-113.]http://www.cqvip.com/Main/Detail.aspx?id=2554431
[51]	Yang Dong, Luo Chao, Peng Zicheng, et al.A pollen record and the paleoclimatic and environmental evolution in Lop-nur, Xinjiang in 32.0~9.1 ka B.P. Quaternary Sciences, 2009, 29(4): 755-766.
[51]	[杨东, 罗超, 彭子成, 等. 新疆罗布泊地区 32.0~9.1 kaB.P.期间的孢粉记录及其古气候古环境演化. 第四纪研究, 2009, 29(4): 755-766.]http://www.dsjyj.com.cn/en/y2009/v29/i4/755
[52]	Ran Min.Paleoclimatic changes in Central Asian arid area during past 50000 years based on loess records [D]. Lanzhou: Lanzhou University, 2012.
[52]	[冉敏. 中亚干旱区黄土记录的过去5万年以来古气候变化历史[D]. 兰州: 兰州大学, 2012.]
[53]	Alley R B, ágústsdóttir A M.The 8k event: Cause and consequences of a major Holocene abrupt climate change. Quaternary Science Reviews, 2005, 24(10/11): 1123-1149.http://linkinghub.elsevier.com/retrieve/pii/S0277379105000314
[54]	Wang Shaowu.8.2 ka BP cold events. Advances in Climate Change Research, 2008, 4(3): 193-194.
[54]	[王绍武. 8.2 ka BP 冷事件. 气候变化研究进展, 2008, 4(3): 193-194.]
[55]	Wu Jinglu, Shen Ji, Wang Sumin, et al.Charaters of climate and environment of the early Holocene in Aibi Lake, Xinjiang Province. Science in China (Series D), 2003, 33(6): 569-575.
[55]	[吴敬禄, 沈吉, 王苏民, 等. 新疆艾比湖地区湖泊沉积记录的早全新世气候环境特征. 中国科学: 地球科学, 2003, 33(6): 569-575.]http://www.cqvip.com/qk/97753a/200312/7998609.html
[56]	Willemse N W, T?rnqvist T E.Holocene century-scale temperature variability from West Greenland lake records. Geology, 1999, 27(7): 580-584.https://pubs.geoscienceworld.org/geology/article/27/7/580-584/189513
[57]	Jiao Keqin, Yao Tandong, Li Shijie.Evolution of glaciers and environment in the west Kunlun Mountains during the past 32 ka. Journal of Glaciology and Geocryology, 2000, 22(3): 250-256.
[57]	[焦克勤, 姚檀栋, 李世杰. 西昆仑山32 ka 来的冰川与环境演变. 冰川冻土, 2000, 22(3): 250-256.]http://d.wanfangdata.com.cn/Periodical_bcdt200003010.aspx
[58]	Xu Yingqin.The sporo-pollen plant communities in the Holocene in the Small Yourdusi Basin, Tianshan Mountians, Xinjiang. Arid Land Geography, 1999, 22(3): 82-88.
[58]	[许英勤. 新疆天山小尤尔都斯盆地全新世孢粉植物群与环境演变. 干旱区地理, 1999, 22(3): 82-88.]
[59]	Yonekura Nobuyuki.Late Quaternary vertical crustal movements in and around the Pacific as deduced from former shoreline data. American Geophysical Union, 1983: 41-50.http://onlinelibrary.wiley.com/doi/10.1029/GD011p0041/pdf
[60]	Shi Yafeng, Kong Zhaochen, Wang Sumin, et al.Climate and environment in the heyday of the Holocene warm period in China. Science China, 1993, 23(8): 865-873.
[60]	[施雅风, 孔昭宸, 王苏民, 等. 中国全新世大暖期鼎盛阶段的气候与环境. 中国科学, 1993, 23(8): 865-873.]
[61]	Chen Huizhong, Jin Jiong, Dong Guangrong.Holocene evolution processes of Gurbantunggut Desert and climatic changes. Journal of Desert Research, 2001, 21(4): 333-339.
[61]	[陈惠中, 金炯, 董光荣. 全新世古尔班通古特沙漠演化和气候变化. 中国沙漠, 2001, 21(4): 333-339.]http://www.cqvip.com/Main/Detail.aspx?id=6071813
[62]	Dong Lina, Lu Huayu, Wang Xiaoyong, et al.A tentative reconstruction of the border migration of Xinjiang deserts during the Last Glacial Maximum and Holocene Optimum. Quaternary Sciences, 2013, 33(2): 398-400.
[62]	[东丽娜, 鹿化煜, 王晓勇, 等. 末次盛冰期和全新世大暖期新疆地区沙漠边界移动初探. 第四纪研究, 2013, 33(2): 398-400.]http://www.cqvip.com/QK/97036X/201302/45117935.html
[63]	Wang Shaowu, Cai Jingning, Zhu Jinhong, et al.Studies on climate change in China. Climatic and Environment Reaserch, 2002, 7(2): 137-145.
[63]	[王绍武, 蔡静宁, 朱锦红, 等. 中国气候变化的研究. 气候与环境研究, 2002, 7(2): 137-145.]http://d.wanfangdata.com.cn/Periodical/qhyhjyj200202002
[64]	Liu Gengnian, Fu Hairong, Cui Zhijiu, et al.An 8000 years environment change record of lacustrine deposits of Foyechi Lake at Taibai Mountains. Research of Soil and Water Conservation, 2005, 12(4): 1-4.
[64]	[刘耕年, 傅海荣, 崔之久, 等. 太白山佛爷池湖泊沉积理化分析反映的 8000 a BP 以来环境变化. 水土保持研究, 2005, 12(4): 1-4.]
[65]	Yi Chaolu, Cui Zhijiu, Xiong Heigang.Numerical periods of Quaternary glaciations in China. Quaternary Sciences, 2005, 25(5): 609-619.
[65]	[易朝路, 崔之久, 熊黑钢. 中国第四纪冰期数值年表初步划分. 第四纪研究, 2005, 25(5): 609-619.]
[66]	Zhao Jindong, Shi Yafeng, Wang Jie.Comparison between Quaternary glaciations in China and the Marine Oxygen Isotope Stage (MIS): An improved schema. Acta Geographica Sinica, 2011, 66(7): 867-884.
[66]	[赵井东, 施雅风, 王杰. 中国第四纪冰川演化序列与 MIS 对比研究的新进展. 地理学报, 2011, 66(7): 867-884.]http://d.wanfangdata.com.cn/Periodical_dlxb201107001.aspx
[67]	Wu Yongqiu, Cui Zhijiu, Liu Gengnian, et al.Glaciation sequences in the Kunlunshan pass area. Journal of Glaciology and Geocryology, 1999, 21(1): 71-76.
[67]	[伍永秋, 崔之久, 刘耕年, 等. 昆仑山垭口地区的冰期系列. 冰川冻土, 1999, 21(1): 71-76.]http://www.cqvip.com/QK/93756X/199901/3505187.html
[68]	Wang Jie, Zhou Shangzhe, Zhao Jingdong, et al.Quaternary glacial geomorphology and glaciations of Kungur Mountain, eastern Pamir, China. Science China Earth Science, 2011, 41(3): 350-361.
[68]	[王杰, 周尚哲, 赵井东, 等. 东帕米尔公格尔山地区第四纪冰川地貌与冰期. 中国科学: 地球科学, 2011, 41(3): 350-361.]
[69]	Wu Guanghe.A preliminary observarion on Neolaciation in Qilian Mountains. Journal of Glaciology and Geocryology, 1984, 6(2): 53-60.
[69]	[伍光和. 祁连山新冰期冰碛的初步观察. 冰川冻土, 1984, 6(2): 53-60.]
[70]	Zhou Shangzhe, Li Jijun, Zhang Shiqiang, et al.Glacial geomorphology and ice ages in the Bailang River Basin, Qilian Mountains. Journal of Glaciology and Geocryology, 2001, 23(2): 131-138.
[70]	[周尚哲, 李吉均, 张世强, 等. 祁连山摆浪河谷地的冰川地貌与冰期. 冰川冻土, 2001, 23(2): 131-138.]http://d.wanfangdata.com.cn/Periodical/bcdt200102005
[71]	Li Jijun, Wen Shixuan, Zhang Qingsong, et al.Exploration of the time, range and formation of Tibet Plateau. Science in China, 1979(6): 608-616.
[71]	[李吉均, 文世宣, 张青松, 等. 青藏高原隆起的时代、幅度和形式的探讨. 中国科学, 1979,(6): 608-616.]
[72]	Zhou Yali, Lu Huayu, Mason J A, et al.Optically stimulated luminescence dating of aeolian sand in the Otindag dune field and Holocene climate change. Science China (Series D), 2008, 38(4): 452-462.
[72]	[周亚利, 鹿化煜, Mason J A, 等. 浑善达克沙地的光释光年代序列与全新世气候变化. 中国科学: 地球科学, 2008, 38(4): 452-462.]http://www.cqvip.com/QK/71135X/201107/29096137.html
[73]	An Chengbang, Feng Zhaodong, Tang Lingyu, et al.Environmental changes and cultural transition at 4 cal. ka BP in Central Gansu. Acta Geographica Sinica, 2003, 58(5): 743-748.
[73]	[安成邦, 冯兆东, 唐领余, 等. 甘肃中部4000年前环境变化与古文化变迁. 地理学报, 2003, 58(5): 743-748.]http://www.cqvip.com/QK/90059X/20035/8836724.html

Optically stimulated luminescence dating of moraines in East Altay Mountains, Xinjiang

RichHTML

PDF (PC)

Like

Knowledge

Cited

Abstract

Cite this article

share this article

References

Related Articles 6

Metrics

Comments

[1]	CUAN Yuda, HUANG Chunchang, PANG Jiangli, ZHOU Yali, ZHANG Yuzhu, GUO Yongqiang, WANG Haiyan, ZHAO Qiqi. OSL dating of the pedo-stratigraphic sequence and the prehistoric flash floods and mudflows over the Lajia Ruins of Qinghai Province [J]. Acta Geographica Sinica, 2019, 74(11): 2371-2384.
[2]	Yuzhu ZHANG, Chunchang HUANG, Yinglu CHEN, Zhihai TAN, Lirong YANG, Yunxiang ZHANG, Haijun QIU, Bo LIU, Fazhu ZHAO. Age and provenance of Younger Dryas paleo-aeolian sandlayers in the Jin-Shaan Gorges of the Yellow River [J]. Acta Geographica Sinica, 2017, 72(5): 790-803.
[3]	Wei ZHANG, Yanjing FU, Beibei LIU, Liang LIU, Zhijiu CUI, Yuanhuang SHI, Siwen WANG. Geomorphological process of late Quaternary glaciers in Kanas river valley of the Altay Mountains [J]. Acta Geographica Sinica, 2015, 70(5): 739-750.
[4]	ZHANG Yuzhu, HUANG Chunchang, PANG Jiangli, ZHOU Yali, ZHA Xiaochun, WANG Longsheng, ZHOU Liang. OSL dating of the sediment stratigraphy of the Lajia Ruins in the Guanting Basin in the Upper Yellow River Basin [J]. Acta Geographica Sinica, 2013, 68(5): 626-639.
[5]	HU Fangen, LI Zhizhong, JIN Jianhui, ZHAO Qian, ZHANG Hui, WANG Xianli, XIA Jing, CHEN Xiuling. Coastal environment evolution record from Anshan coastal aeolian sand of Jinjiang, Fujian Province, based on the OSL dating [J]. Acta Geographica Sinica, 2013, 68(3): 343-356.
[6]	MAO Longjiang, MO Duowen, JIANG Leping, JIA Yaofeng,LI Minglin, ZHOU Kunshu, SHI Chenxi. Environmental Change since Mid- Pleistocene Recorded in Shangshan Achaeological Site in Zhejiang [J]. Acta Geographica Sinica, 2008, 63(3): 293-300.