全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...

西昆仑山甜水海北湖砂楔的形成与环境演变

DOI: 10.3969/j.issn.1001-7410.2011.01.15, PP. 112-119

Keywords: 甜水海,砂楔,围岩,环境演变

Full-Text   Cite this paper   Add to My Lib

Abstract:

青藏高原是世界上中低纬度地区冰缘最发育的区域,其中西昆仑山甜水海地区广泛分布着砂楔群等冰缘现象。砂楔是寒冷气候条件的产物,对古气候和古环境的重建具有重要意义。文章通过分析甜水海北湖砂楔矿物特征发现,砂楔填充物基本属于近源堆积;14C测年结果以及粒度再结合砂楔形态分析得出,该砂楔的形成经历了13.9kaB.P.,11.9kaB.P.和11.5kaB.P.这3个时期,这3个时期均属于气候小波动中的降温过程,但在甜水海地区它们所对应的降温幅度都不是特别大,大约分别为1.8℃,1℃和4℃。总的来说砂楔可以作为气候由暖湿转为冷干的指示剂。

References

[1]  3 徐叔鹰,张维信,徐德馥等.青藏高原东北边缘地区冰缘发展探讨.冰川冻土,1984, 6 (2):15~25
[2]  Xu Shuying,Zhang Weixin,Xu Defu et al.Discussion on the periglacial development in the northeast marginal region of Qinghai-Xizang Plateau. Journal of Glaciology and Geocryology,1984, 6 (2):15~25
[3]  4 梁凤仙,程国栋.青藏公路沿线的多边形-脉构造及其古气候意义.冰川冻土,1984, 6 (4):49~60
[4]  6 王乃昂,王 涛,高顺尉等.河西走廊末次冰期芒硝和砂楔与古气候重建.地学前缘,2000, 7 (增刊2):59~66
[5]  Wang Nai''ang,Wang Tao,Gao Shunwei et al.The sand wedge and mirabilite of the last ice age and paleoclimatic reconstruction in Hexi corridor,Gansu,West China. Earth Science Frontiers,2000, 7 (Suppl.2):59~66
[6]  7 王乃昂,王 涛,史正涛等.河西走廊未次冰期砂楔的发现及其古气候意义.冰川冻土,2001, 23 (1):46~50
[7]  Wang Nai''ang,Wang Tao,Shi Zhengtao et al.The discovery of sand wedges of the Last Glaciation in the Hexi Corridor and its paleoclimatic significance. Journal of Glaciology and Geocryology,2001, 23 (1):46~50
[8]  8 金会军,赵 林,王绍令等.青藏高原中东部全新世以来多年冻土演化及寒区环境变化.第四纪研究,2006, 26 (2):198~210
[9]  Jin Huijun,Zhao Lin,Wang Shaolin et al.Evolution of permafrost and environmental changes of cold regions in eastern and interior Qinghai-Tibetan Plateau since the Holocene. Quaternary Sciences,2006, 26 (2):198~210
[10]  9 崔之久.青藏高原冰缘地貌的基本特征.中国科学(A辑),1981,(6):724~733
[11]  Cui Zhijiu.The basic features of periglacial landform in Qinghai-Tibet Plateau. Science in China(Series A),1981,(6):724~733
[12]  10 刘东生,张新时,熊尚发等.青藏高原冰期环境与冰期全球降温.第四纪研究,1999,(5):385~396
[13]  Liu Tungsheng,Zhang Xinshi,Xiong Shangfa et al.Qinghai-Xizang Plateau glacial environment and global cooling. Quaternary Sciences,1999,(5):385~396
[14]  11 郭东信.青藏高原上的砂楔.冰川冻土,1979, 1 (1): 51,73
[15]  Guo Dongxin.The sand wedges in Qinghai-Xizang Plateau. Journal of Glaciology and Geocryology,1979, 1 (1): 51,73
[16]  Shi Yafeng,Li Jijun,Li Bingyuan eds.Uplift and Environment Changes on the Qinghai-Xizang Plateau in the Late Cenozioc.Guangzhou: Guangdong Science and Technology Press,1998.159~414
[17]  18 张培震,郑德文,尹功明等.有关青藏高原东北缘晚新生代的扩展与隆升的讨论.第四纪研究,2006, 26 (1):5~13
[18]  Zhang Peizhen,Zheng Dewen,Yin Gongmin et al.Discussion on Late Cenozoic growth and rise of northeastern margin of the Tibetan Plateau. Quaternary Sciences,2006, 26 (1):5~13
[19]  19 孔 屏,那春光.青藏高原的剥蚀与构造抬升.2007, 27 (1):1~9
[20]  Kong Ping,Na Chunguang.Erosion and uplift of Tibetan Plateau. Quaternary Science,2007, 27 (1):1~9
[21]  20 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 (1):222~231
[22]  Xuhua Shi,Erchie Wang,Gang Wang et al.Late Cenozoic Uplift of the Yulong Snow Mountain(5596m),SE Tibetan Plateau,caused by erosion and tectonic forcing. Quaternary Sciences,2008, 28 (1):222~231
[23]  21 中国科学院兰州冰川冻土研究所编.中国冰川目录(Ⅶ)——青藏高原内陆水系(班公错湖流域区).北京:科学出版社,1992.23~96
[24]  Lanzhou Institute of Glaciology and Geocryology,Chinese Academy of Sciences.Glacier Inventory of China(Ⅶ)——Qinghai-Xizang Plateau interior Area(Drainage Basin of the Bangong Lake).Beijing: Science Press,1992.23~96
[25]  18 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
[26]  Zhao Xitao,Zhang Yongshuang,Qu Yongxin et al.Pleistocene glaciations along the western foot of the Yulong Mountains and their relationship with the formation and development of the Jinsha River. Quaternary Sciences, 2007, 27 (1):35~44
[27]  19 沈永平,徐道明.西藏安多的湖泊变化与环境.冰川冻土,1994, 16 (2):173~180
[28]  Shen Yongping,Xu Daoming.Fluctuations of lakes and their environments since last glaciation in Amdo area,Tibet. Journal of Glaciology and Geocryology,1994, 16 (2):173~180
[29]  Xu Liubing,Zhou Shangzhe,Wang Jie.Pleistocene glaciations in the Shaluli Shan and the influences of southwest monsoon on the glaciations during the last glacial period. Quaternary Sciences,2005, 25 (5):620~629
[30]  22 赵希涛,吴中海,朱大岗等.念青唐古拉山脉西段第四纪冰川作用.第四纪研究,2002, 22 (2):424~433
[31]  Zhao Xitao,Wu Zhonghai,Zhu Dagang et al.Quaternary glaciations in the West Nyaiqentanglha Mountains. Quaternary Sciences, 2002, 22 (2):424~433
[32]  27 李栓科,李世杰.青藏高原北缘末次冰期最盛时期的湖侵及其原因.冰川冻土,1991, 13 (4):299~306
[33]  Li Shuanke,Li Shijie.Lake transgression and reasons during last glaciation maximum on the north margin of Qinghai-Xizang Plateau. Journal of Glaciology and Geocryology,1991, 13 (4):299~306
[34]  28 杨建强,崔之久,易朝露等.云南点苍山冰川湖泊沉积物磁化率的影响因素及其环境意义.第四纪研究,2004, 24 (5):591~597
[35]  Yang Jianqiang,Cui Zhijiu,Yi Chaolu et al.The influencing factors and environmental significance of magnetic susceptibility in the glacio-lacustrinal sediments on the Diancang Mountains,Yunnan Province. Quaternary Sciences,2004, 24 (5):591~597
[36]  29 李世杰,郑本兴,焦克勤.西昆仑山区湖泊初探.海洋与湖沼,1993, 24 (1):37~44
[37]  Li Shijie,Zheng Benxing,Jiao Keqin.Lakes in the Western Kunlun Mountain areas. Oceanologia et Limnologia Sinica,1993, 24 (1):37~44
[38]  25 王富葆,曹琼英,刘福涛.西昆仑山南麓湖泊和水系的近期变化.第四纪研究,1990,(4):316~325
[39]  Wang Fubao,Cao Qiongying,Liu Futao.The recent changes of lakes and drainage system in the south piedmont of West Kunlun Mts. ,China. Quaternary Sciences,1990,(4):316~325
[40]  26 李世杰,张宏亮,施雅风等.青藏高原甜水海盆地MIS 3阶段湖泊沉积与环境变化.第四纪研究,2008, 28 (1):122~131
[41]  Li Shijie,Zhang Hongliang,Shi Yafeng et al.A high resolution MIS 3 environmental change record derived from lacustrine deposit of Tianshuihai Lake,Qinghai-Tibet Plateau. Quaternary Sciences,2008, 28 (1):122~131
[42]  27 苏 珍.喀喇昆仑山——昆仑山地区冰川与环境.北京:科学出版社,1998.159~215
[43]  Su Zhen.The Glaciers and Environment in the Karakorum and Kunlun Mountains,Qinghai-Xizang Plateau.Beijing: Science Press,1998.159~215
[44]  38 Lachenbruch A H. Contraction theory of ice-wedge polygons; A qualitative discussion.In: Proceedings,First International Permafrost Conference.National Academy of Science,National Research Council of Canada,Publication 12871966.63~71
[45]  39 Hugh M French. The Periglacial Environment(3rd edition).Chichester: John Wiley & Sons Ltd,2007.116~152
[46]  Li Yuanfang,Zhang Qingsong,Li Bingyuan.Ostracod fauna and environmental changes during the past 17000 years in the Western Tibet. Acta Geographica Sinica,1994, 49 (1):46~54
[47]  42 罗 超,杨 东,彭子成等.新疆罗布泊地区近3.2万年沉积物的气候环境记录.第四纪研究,2007, 27 (1):114~121
[48]  Luo Chao,Yang Dong,Peng Zicheng et al.Climatic and environmental records in the sediment of the Luobei billabong in Lop Nor,Xinjiang in recent 32ka. Quaternary Sciences,2007, 27 (1):114~121
[49]  43 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
[50]  Yi Chaolu,Cui Zhijiu,Xiong Heigang.Numerical Periods of Quaternary Glaciations in China. Quaternary Sciences,2005, 25 (5):609
[51]  1 王保来.土楔和冰楔假形及其古气候意义.冰川冻土,1991, 13 (1):67~76
[52]  Wang Baolai.Soil wedge and ice-wedge pseudomorphs and their paleoclimatic implications. Journal of Glaciology and Geocryology,1991, 13 (1):67~76
[53]  2 李作福,郭东信.多边形-脉构造及其环境意义.冰川冻土,1990, 12 (4):301~310
[54]  Li Zuofu,Guo Dongxin.Polygon-veins and their environmental significances. Journal of Glaciology and Geocryology,1990, 12 (4):301~310
[55]  Liang Fengxian,Cheng Guodong.Polygon-veins along the Qinghai-Xizang highway. Journal of Glaciology and Geocryology,1984, 6 (4):49~60
[56]  5 崔之久,赵 亮,Vandenberghe J等.山西大同、内蒙古鄂尔多斯冰楔、砂楔群的发现及其环境意义.冰川冻土,2002, 24 (6):708~716
[57]  Cui Zhijiu,Zhao Liang,Vandenberghe J et al.Discovery of ice wedge and sand-wedge networks in Inner Mongolia and Shanxi Province and their environmental significance. Journal of Glaciology and Geocryology,2002, 24 (6):708~716
[58]  12 程 捷,张绪教,田明中等.黄河源区冰楔假型群的发育及其古气候意义.第四纪研究,2006, 26 (1):92~98
[59]  Cheng Jie,Zhang Xujiao,Tian Mingzhong et al.Ice-wedge casts discovered in the source area of Yellow River,North East Tibetan Plateau and their paleoclimatic implications. Quaternary Sciences, 2006, 26 (1):92~98
[60]  13 俞祁浩, Kurt Roth,金会军等.中德合作三江源区和甜水海地区多年冻土退化过程科学考察和研究进展.冰川冻土,2006, 28 (6):844~849
[61]  Yu Qihao,Kurt Roth,Jin Huijun et al.Progress of the Sino-German joint researches on the degradation of permafrost on the Tibetan Plateau. Journal of Glaciology and Geocryology,2006, 28 (6):844~849
[62]  14 李吉均,文世宣,张青松等.青藏高原隆升的时代、幅度和形式探讨.中国科学(B辑),1979, 9 (6):608~616
[63]  Li Jijun,Wen Shixuan,Zhang Qingsong et al.A discussion on the period,amplitude and type of the uplift of the Qinghai-Xizang Plateau. Scientia Sinica(Series B),1979, 9 (6):608~616
[64]  15 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
[65]  Li Jijun,Fang Xiaomin,Pan Baotian et al.Late Cenozoic intensive uplift of Qinghai-Xizang Plateau and its impacts on environments in surrounding area. Quaternary Sciences,2001, 21 (5):381~391
[66]  16 张青松,周耀飞,陆祥顺等.现代青藏高原上升速度问题.科学通报,1991, 36 (7):529~531
[67]  Zhang Qingsong,Zhou Yaofei,Lu Xiangshun et al.On the present up lift speed of Qinghai-Xizang Plateau. Chinese Science Bulletin,1991, 36 (7):529~531
[68]  17 施雅风,李吉均,李炳元编著.青藏高原晚新生代的隆升与环境变化.广州:广东科技出版社,1998.159~414
[69]  20 类延斌,张虎才,尚华明等.青藏高原年保玉则山末次冰期中期以来的湖泊演化与古冰川发育.第四纪研究,2008, 28 (1):132~139
[70]  Lei Yanbin,Zhang Hucai,Shang Huaming et al.Lake evolution and glaciation of the Nianbaoyuze Mountain in the Tibetan Plateau since the middle of the last glacial. Quaternary Sciences,2008, 28 (1):132~139
[71]  21 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
[72]  28 Pettijohn F J, Potter P E,Siever R.Sand and Sandstone.Beijing: Science Press,1977.35~40
[73]  29 和钟铧,刘招君,郭 巍.柴达木盆地北缘大煤沟剖面重矿物分析及其地质意义.世界地质,2001, 20 (3):279~284
[74]  He Zhonghua,Liu Zhaojun,Guo Wei.The heavy mineral analysis and its geological significance of Dameigou section in Northern Qaidam Basin. World Geology,2001, 20 (3):279~284
[75]  30 陆洁民,郭召杰,赵泽辉等.新生代酒西盆地沉积特征及其与祁连山隆升关系的研究.高校地质学报,2004, 10 (1):50~61
[76]  Lu Jiemin,Guo Zhaojie,Zhao Zehui et al.Cenozoic sedimentation characteristics of Jiuxi Basin and uplift history of Northern Qilian Mountain. Geological Journal of China Universities,2004, 10 (1):50~61
[77]  31 陈 静,王 哲,王张华等.长江三角洲东西部晚新生代地层中的重矿物差异及其物源意义.第四纪研究,2007, 27 (5):700~708
[78]  Chen Jing,Wang Zhe,Wang Zhanghua et al.Heavy mineral distribution and its provenance implication in late Cenozoic sediments in western and eastern area of the Changjiang River delta. Quaternary Sciences,2007, 27 (5):700~708
[79]  32 黎 兵,李 勇,张开均等.青藏高原东缘晚新生代大邑砾岩的物源分析与水系变迁. 第四纪研究,2007, 27 (1):64~73
[80]  Li Bing,Li Yong,Zhang Kaijun et al. Provenance of the siliciclastic rocks of the Late Cenozoic Dayi Formation and drainage change at eastern margin of the Tibetan Plateau. Quaternary Sciences,2007, 27 (1):64~73
[81]  33 康春国,李长安,邵 磊.江汉平原主要河流沉积物重矿物特征与物源区岩性的响应.第四纪研究,2009, 29 (2):334~342
[82]  Kang Chunguo,Li Chang''an,Shao Lei.Heavy mineral characteristics of river sediments in Jianghan Plain and its response to provenance rock types. Quaternary Sciences,2009, 29 (2):334~342
[83]  34 Folk R L, Ward W C.Brazos river bar: A study in the signification of grain size parameters. Journal of Sedimentary Petrology,1957, 27 :3~26
[84]  35 成都地质学院陕北队编.沉积岩(物)粒度分析及其应用.北京:地质出版社,1976.55~103
[85]  Shanbei Team of Chengdu Institute of Geology ed.Grain Size Analysis of the Sedimentary Rock(Sediment)and its Application.Beijing: Geological Publishing House,1976.55~103
[86]  36 Murton J B, Worsley P,Gozdzik J.Sand veins and wedges in cold aeolian environments. Quaternary Science Reviews,2000, 19 (9):899~922
[87]  37 Lachenbruch A H. Mechanics of Thermal Contraction Cracks and Ice-wedge Polygons in Permafrost.New York: Geological Society of America,1962.69
[88]  40 刘耕年,崔之久,伍永秋等.昆仑山垭口热水剖面18000年以来的环境变化记录.地质力学学报,1997, 3 (4):39~45
[89]  Liu Gengnian,Cui Zhijiu,Wu Yongqiu et al.Record of environmental change in Reshui profile at Kunlunshan pass since 18kaBP. Journal of Geomechanics,1997, 3 (4):39~45
[90]  41 李元芳,张青松,李炳元.青藏高原西北部17000年以来的介形类及环境演变.地理学报,1994, 49 (1):46~54

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133