[1] Li Jijun, Fang Xiaomin, Ma Haizhou et al. Geomorphological and environmental evolution in the upper reaches ofHuanghe River during the Late Cenozoic. Science in China: Series D, 1996, 26(4): 316-322. [李吉均, 方晓敏, 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.]
[2] Wu Xihao, Jiang Fuchu, Wang Sumin et al. The questions about the Yellow River passing through the Sanmen Gorge andflowing east to the sea. Quaternary Science, 1998, 18(2): 188. [吴锡浩, 蒋复初, 王苏民等. 关于黄河贯通三门峡东流入海问题. 第四纪研究, 1998, 18(2): 188.]
[3] Lin A M, Yang Z Y, Sun Z M et al. How and when did Yellow River develop its square bend? Geology, 2001, 29: 951-954.
[4] Zhu Zhaoyu. The formation of river terraces and evolution of drainage system in the middle Yellow River. ActaGeographica Sinica, 1989, 44(4): 429-440. [朱照宇. 黄河中游河流阶地的形成与水系演化. 地理学报, 1989, 44(4):429-440.]
[5] Yue Leping, Lei Xiangyi, Qu Hongjun. The age of terrace development in the middle reaches of the Yellow River.Geological Review, 1997, 43(2): 186-192. [岳乐平, 雷祥义, 屈红军. 黄河中游水系的阶地发育时代. 地质论评, 1997, 43(2): 186-192.]
[6] Pan Baotian, Li Jijun, Cao Jixiu et al. The study of the geomorphic evolution and development of the Yellow River in theHualong Basin. Mountain Research, 1996, 14(3): 153-158. [潘保田, 李吉均, 曹继秀等. 化隆盆地地貌演化与黄河发育研究. 山地研究, 1996, 14(3): 153-158.]
[7] Nie Zongsheng, Li Ke. The discovery of the salawusu stratum group and its implication. Chinese Science Bulletin, 1988, 33(21): 1645-1649. [聂宗笙, 李克. 内蒙古包头地区萨拉乌苏组的发现及其意义. 科学通报, 1988, 33(21): 1645-1649.]
[8] Madsen D B, Chen Fahu, Oviatt C G et al. Late Pleistocene/Holocene wetland events recorded in southeast Tengger Desertlake sediments, NW China. Chinese Science Bulletin, 2003, 48: 1423-1429.
[9] Chen Fahu, Fan Yuxin, Chun Xi et al. Preliminary research on Megalake Jilantai-Fletao in the arid areas of China during the Late Quaternary. Chinese Science Bulletin, 2008, 53(10): 1207-1219. [陈发虎, 范育新, 春喜等. 晚第四纪“吉兰泰—河套”古大湖的初步研究. 科学通报, 2008, 53(10): 1207-1219.]
[10] Nie Zongsheng, Li Hong, Ma Baoqi. Fossil fauna in the late stage of late Pleistocene in the Hetao Basin, Innermongolia.Quaternary Science, 2008, 28(1): 14-25. [聂宗笙, 李虹, 马保起. 内蒙古河套盆地晚更新世晚期化石动物群. 第四纪研究, 2008, 28(1): 14-25.]
[11] Dou Suqin, Nie Zongsheng, Mai Xueshun. The sporo-pollen analysis of late Pleistocene deposits in Ho-bao basin of NeiMongol. Seismology and Geology, 1990, 12(3): 283-289. [窦素芹, 聂宗笙, 麦学舜. 内蒙古呼包盆地晚更新世孢粉组合及其意义. 地震地质, 1990, 12(3): 283-289.]
[12] Ma Baoqi, Li Dewen, Guo Wensheng. Geomorphological response to environmental changes during the late stage of latePleistocene in Hubao Basin. Quaternary Science, 2004, 24(6): 630-637. [马保起, 李德文, 郭文生. 晚更新世晚期呼包盆地环境演化与地貌响应. 第四纪研究, 2004, 24(6): 630-637.]
[13] Jia Tiefei, Yin Shan, Zhao Ming et al. A study of the lake deposits on the Tuoketuo section of Yellow River in the earlyand middle stage of Pleistocene. Journal of Inner Mongolia Normal University: Natural Science Edition, 2001, 30(1):74-78. [贾铁飞, 银山, 赵明等. 黄河托克托段早中更新世湖相地层剖面的建立及其意义. 内蒙古师大学报: 自然科学版, 2001, 30(1): 74-78.]
[14] Li Jianbiao, Ran Yongkang, Guo Wensheng. Research on the lacustrine strata of the Tuoketuo mesa, Hetao Basin, China.Quaternary Science, 2005, 25(5): 630-639. [李建彪, 冉永康, 郭文生. 河套盆地托克托台地湖相层研究. 第四纪研究,2005, 25(5): 630-639.]
[15] Li Jianbiao, Ran Yongkang, Guo Wensheng. Division of Quaternary beds and environment evolution in Hubao Basin inChina. Quaternary Science, 2007, 27(4): 632-644. [李建彪, 冉永康, 郭文生. 呼包盆地第四纪地层与环境演化. 第四纪研究, 2007, 27(4): 632-644.]
[16] Chen Fahu, Fan Yuxin, Madsen D B et al. Preliminary study on the formation mechanism of the“Jilantai-Hetao”megalake and the lake evolutionary history in Hetao Region. Quaternary Science, 2008, 28(5): 865-873. [陈发虎, 范育新,Madsen D B等. 河套地区新生代湖泊演化与“吉兰泰—河套”古大湖形成机制的初步研究. 第四纪研究, 2008, 28(5):865-873.]
[17] Li Jianbiao. A study on the lake forming environment and tectonic activity during the late Quaternary in the Hetao BasinInner Mongolia Autonomous Region, China [D]. Beijing: Institute of Geology, State Seismological Bureau, 2006. [李建彪. 河套盆地晚第四纪成湖环境变化与构造活动研究[D]. 北京: 国家地震局地质研究所, 2006.]
[18] Yu Huifu. The research progress and comparative study to measure content of carbonate. Marine Geology Letters, 2007, 23(1): 35-39. [郁慧福. 碳酸盐测定方法现状及方法比较. 海洋地质动态, 2007, 23(1): 35-39.]
[19] Atiken M J. An Introduction to Optical Dating. Oxford: Oxford University Press, 1998.
[20] Roberts R G, Walsh G, Murray A S et al. Luminescence dating of rock art and past environments using mud-wasp nests innorthern Australia. Nature, 1997, 387: 696-699.
[21] Murray A S, Roberts R G. Determining the burial time of single grains of quartz using optically stimulated luminescence.Earth and Planetary Science Letters, 1997, 152: 163-180.
[22] Spooner N A, Olley J M, Questiaux D G et al. Optical dating of an aeolian deposit on the Murrumbidgee floodplain.Quaternary Science Reviews, 2001, 20: 835-840.
[23] Jacobs Z, Wintle A G, Roberts R G et al. Equivalent dose distributions from single grains of quartz at Sibudu, SouthAfrica: Context, causes and consequences for optical dating of archaeological deposits. Journal of Archaeological Science,2008, 35: 1808-1820.
[24] Feathers J K. Single-grain OSL dating of sediments from the Southern High Plains, USA. Quaternary Science Reviews,2003, 22: 1035-1042.
[25] Murray A S, Roberts, R G. Measurement of the equivalent dose in quartz using a regenerative-dose single-aliquotprotocol. Radiation Measurements, 1998, 29: 503-515.
[26] Murray A S, Wintle A G. Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol.Radiation Measurements, 2000, 32: 57-73.
[27] Murray A S, Olley J M, Caitcheon G G. Measurement of equivalent doses in quartz from contemporary water-lainsediments using optically stimulated luminescence. Quaternary Science Reviews, 1995, 14: 365-371.
[28] Lang A, Zolitschka B. Optical dating of annually laminated lake sediments: A test case from Holzmaar/Germany.Quaternary Science Reviews, 2001, 20: 737-742.
[29] Zheng Y E, Zhou L P, Zhang J F. Optical dating of the upper 22 m of cored sediments from Daihai Lake, northern China.Quaternary Geochronology, 2010, 5: 228-232.
[30] Owen L A, Bright J, Finkel R C et al. Numerical dating of a Late Quaternary spit-shoreline complex at the northern end ofSilver Lake playa, Mojave Desert, California: A comparison of the applicability of radiocarbon, luminescence, terrestrial cosmogenic nuclide, electron spin resonance, U-series and amino acid racemization methods. Quaternary International,2007, 166: 87-110.
[31] Thomsen K J, Murray A S, Botter-Jensen L et al. Determination of burial dose in incompletely bleached fluvial samplesusing single grains of quartz. Radiation Measurements, 2007, 42: 370-379
[32] Duller G AT. Single grain optical dating of glacigenic deposits. Quaternary Geochronology, 2006, 1: 296-304.
[33] Berger G W, Doran P T, Thomsen K J. Single-grain and multigrain luminescence dating of on-ice and lake-bottomdeposits at Lake Hoare, Taylor Valley, Antarctica. Quaternary Geochronology, 2010, 5: 679-690.
[34] Olley J M, Caitcheon G G. The origin of dose distributions in fluvial sediments, and the prospect of dating single grains ofquartz from fluvial deposits using optically stimulated luminescence. Radiation Measurements, 1999, 30: 207-217.
[35] Olley J M, Pietsch T, Roberts R G. Optical dating of Holocene sediments from a variety of geomorphic settings usingsingle grains of quartz. Geomorphology, 2004, 60: 337-358.
[36] Thomsen, K J, Murray A S, B￠tter-Jensen L B et al. Determination of burial dose in incompletely bleached fluvial samplesusing single grains of quartz. Radiation Measurements, 2007, 42: 370-379.
[37] Prescott J R, Hutton J T. Cosmic ray contributions to dose rates for luminescence and ESR dating: Large depths andlong-term time variations. Radiation Measurements, 1994, 23: 497-500.
[38] Zhu Dagang, Zhao Xitao, Meng Xiangang et al. First discovery of late Pleistocene lacustrine-beach rock around the NamCo in the northern Tibetan Plateau. Geological Bulletin of China, 2002, 21(3): 175. [朱大岗, 赵希涛, 孟宪刚等. 藏北高原环纳木错首次发现晚更新世湖滩岩. 地质通报, 2002, 21(3): 175.]
[39] Zhu Dagang, Zhao Xitao. Late Pleistocene lacustrine-beach rock around the Nam Co in Xizang. Geological Review, 2003,49(4):432-439. [朱大岗, 赵希涛. 西藏纳木错晚更新世湖滩岩. 地质论评, 2003, 49(4):432-439.]
[40] Chen Jing'an, Wan Guojiang, Tang Degui et al. The record of lake sediments in grain size and isotope during the recentclimate change in Erhai. Progress in Natural Science, 2000, 10(3) : 253-259. [陈敬安, 万国江, 唐德贵等. 洱海近代气候变化的沉积物粒度与同位素记录. 自然科学进展, 2000, 10(3): 253-259.]
[41] Chen Jing'an, Wan Guojiang, Zhang Feng et al. The record of lake sediments in different scales: Taking grain size forexample. Science in China: Series D, 2003, 33(6): 563-568. [陈敬安, 万国江, 张峰等. 不同时间尺度下的湖泊沉积物环境记录: 以沉积物粒度为例. 中国科学: D辑, 2003, 33(6): 563-568.]
[42] Yin Zhiqiang, Qin Xiaogang, Wu Jinshui et al. Multimodal grain-size distribution cahracteristic and formation mechanismof lake sediments. Quaternary Science, 2008, 28(2): 345-353. [殷志强, 秦小光，吴金水等. 湖泊沉积物粒度多组分特征及其成因机制研究. 第四纪研究, 2008, 28(2): 345-353.]
[43] Lerman A. Lakes: Chemistry, Geology, Physics. Wang Sumin et al. trans. Beijing: Geological Publishing Housing,1989. [莱尔曼A. 湖泊的化学、地质学和物理学. 王苏民等译. 北京: 地质出版社, 1989.]
