ISSN 1009-6248CN 61-1149/P Bimonthly

Supervisor:China Geological Survey

Sponsored by:XI'an Center of China Geological Survey
Geological Society of China

    • The Core Journals of China
    • The Key Magazine of China Technology
    • CSCD Included Journals
    • Scopus Included Journals
Advance Search
BIAN Xiao-wei, ZENG Zhong-cheng, ZHU Hai-ping, et al. The Discovery of the Mid-Pleistocene Glacial Tills and Its Geological Significance in Taxkorgan Stone Town Region of Xinjiang[J]. Northwestern Geology, 2014, 47(4): 131-140.
Citation: BIAN Xiao-wei, ZENG Zhong-cheng, ZHU Hai-ping, et al. The Discovery of the Mid-Pleistocene Glacial Tills and Its Geological Significance in Taxkorgan Stone Town Region of Xinjiang[J]. Northwestern Geology, 2014, 47(4): 131-140.

The Discovery of the Mid-Pleistocene Glacial Tills and Its Geological Significance in Taxkorgan Stone Town Region of Xinjiang

More Information
  • Received Date: June 18, 2014
  • Revised Date: October 10, 2014
  • Available Online: July 28, 2022
  • Published Date: December 04, 2014
  • The authors first found the three fossil glacial tills at the ancient army service station, stone town and gas station in Taxkorgan County. Geomorphic Types and distribution of the fossil glacial tills were the remaining glacial platform. The platform is about 3 100 m in height, and we can see a lot of glacial syenite boulders on it. The tafonis developed on glacial syenite boulders were classified into side-wall tafoni, basal tafoni, cellular tafoni according to their morphological characteristics and positions. Field geological investigation shows that the gravel cut down into the old moraine, and the OSL age of the gravel layer is (62.07 ± 2.44) Ka. Contrastive study of the fossil glacial tills in stone town region and the glacial moraine in Muztag Ata-Konggur Mountain was carried out, it is showed that the fossil glacial tills formed in late penultimate glacial period of mid-Pleistocene, and derived from the glacier advance of paleo-glacier in the Sidun Mountain. The discovery of the mid-Pleistocene glacial tills has very important geological significance: (1) the authors divided the Quaternary glaciers in the Sidun Mountain into four ice ages, namely late penultimate glacial period of mid-Pleistocene and last glacial period of late Pleistocene, as well as neoglacial period and little Ice Age of Holocene; (2) the Taxkorgan fault are left-lateral strike-slip faults; (3) the clear bounds and limited scales of Pleistocene glaciations in the Sidun mountain and Muztag are incompatible with imagining a successive ice sheet on the Plateau.
  • 陈杰, 李涛, 李文巧, 等. 帕米尔构造结及邻区的晚新生代构造与现今变形 [J]. 地震地质, 2011, 33(2): 241-259.
    Chen Jie, Li Tao, Li Wenqiao, et al. Late Cenozoic and present tectonic deformation in the Pamir salient, northwestern China [J]. Seismology and Geology, 2011, 33(2): 241-259.
    崔之久. 慕士塔格-公格尔冰川的某些特点及其开发利用的条件 [J]. 地理学报, 1960, 26: 35-44.
    Cui Zhijiu. Some Characteristics and Exploitation and Utilization of Muztagata-Kongur glaciers [J]. Acta Geographica Sinica, 1960, 26: 35-44.
    焦克勤, 姚檀栋, 李世杰. 西昆仑山 32 ka来的冰川与环境演变 [J]. 冰川冻土, 2000, 22(3): 250-256.
    Jiao Keqin, Yao Tan dong, Li Shijie. Evolution of glaciers and environment in the West Kunlun Mountains during the past 32ka [J]. Journal of Glaciology and Geocryology, 2000, 22(3): 250-256.
    柯珊, 罗照华, 莫宣学, 等. 帕米尔构造结塔什库尔干碱性杂岩同位素年代学研究 [J]. 岩石学报, 2008, 24(2): 315-324.
    Ke Shan, Luo Zhaohua, Mo Xuanxue, et al. The geochronology of Taxkorgan alkalic complex, Pamir syntax [J]. Acta Petrologica Sinica, 2008, 24(2): 315-324.
    李炳元. 地貌环境演化 [A]. 张青松, 李炳元, 编. 喀喇昆仑山-昆仑山地区晚新生代环境变化 [C]. 北京: 中国环境科学出版社, 1999, 178-196.
    Li Bingyuan. Landforms and circumstance evolution [A]. ZHANG Qing-song, LI Bing-yuan, et al. Karakorum-Kunlun mountains environmental change during late Cenozoic [C]. China Environmental Science Press, Beijing, 1999, 178-196.
    李德文, 崔之久, 李洪江, 等. 华北北部花岗岩风化穴形成机制与环境意义 [J]. 南京大学学报: 自然科学, 2003, 39(1): 120-128.
    Li Dewen, Cui Zhijiu, Li Hongjiang, et al. Genesis of granitic tafoni of northern north China and its environmental significance [J]. Journal of Nanjing University: Natural Sciences, 2003, 39(1): 120-128.
    李文巧, 陈杰, 袁兆德, 等. 帕米尔高原 1895 年塔什库尔干地震地表多段同震破裂与发震构造 [J]. 地震地质, 2011, 33(2): 260-276.
    Li Wenqiao, Chen Jie, Yuan Zhaode, et al. Coseismic surgace ruptures of multi segments and seismogenic fault of the Tashkoragan earthquake in Pamir [J]. Seismology and Geology, 2011, 33(2): 260-276.
    刘栋梁, 李海兵, 潘家伟, 等. 帕米尔东北缘-西昆仑的构造地貌及其构造意义 [J]. 岩石学报, 2011, 27(11): 3499-3512.
    Liu Dongliang, Li Haibing, Pan Jiawei, et al. Morphotectonic study from the northeastern margin of the Pamir to the West Kunlun range and its tectonic implications [J]. Acta Petrologica Sinica, 2011, 27(11): 3499-3512. 苏珍, 李世杰, 王志超. 喀喇昆仑山-昆仑山地区第四纪冰川遗迹与冰期划分 [A]. 苏珍, 谢自楚, 王志超, 等编. 喀喇昆仑山-昆仑山地区冰川与环境 [C]. 北京: 科学出版社, 1998, 140-149.
    Su Zhen, Li Shijie, Wang Zhichao. Quaternary glaciation in the Karakorum-Kunlun mountains [A]. SU Zhen, Xie Zichu, Wang Zhichao, et al. Glaciers and Environments in the Karakorum-Kunlun mountains [C]. Geological Publishing House, Beijing, 1998, 140-149.
    王国灿, 曹凯, 张克信, 等. 青藏高原新生代构造隆升阶段的时空格局 [J]. 中国科学(地球科学), 2011, 41(3): 332-349.
    Wang Guocan, Cao Kai, Zhang Kexin, et al. Spatio-temporal frame work of tectonic uplift stages of the Tibertan Plateau in Cenozoic [J]. Sci China Earth Sci, 2011, 41(3): 332-349.
    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 [J]. 中国科学: 地球科学, 2011, 41(3): 350-361.
    Wang Jie, Zhou Shangzhe, Zhao Jingdong, et al. Quaternary glacial geomorphology and glaciations of Kongur Mountain, eastern Pamir, China [J]. Sci China Earth Sci, 2011, 41(3): 350-361.
    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[J].地震地质,2005,27(4): 615-623.

    Wang Xulong, Lu Yanchou, Li Xiaoni. Luminescence dating of fine-grained quartz in Chinese loess-simplified multipliquot regene rative-dose(mar)protocol [J]. Seismology and Geology, 2005, 27(4): 615-623.
    王亚伟, 廖小莹, 刘良, 等. 西昆仑塔什库尔干苦子干碱性杂岩体的成因及其构造意义 [J]. 西北地质, 2013, 46(4): 1-24.
    Wang Yawei, Liao Xiaoying, Liu Liang, et al. Petrogenesis and tectonic implications of the Cenozoic alkaline complex in Kuzigan, Taxkorgan, west kunlun. [J]. Northwestern Geology, 2013, 46(4): 1-24.
    肖序常, 刘训, 高锐, 等. 西昆仑及邻区岩石圈结构构造演化-塔里木南-西昆仑多学科地学断面简要报道 [J]. 地质通报, 2002, 21: 63-68.
    Xiao Xuchang, Liu Xun, Gao Rui, et al. Lithospheric structure and tectonic evolution of the West Kunlun and its adjacent areas: Brief report on the South Tarim-West Kunlun multidisciplinary geoscience transect [J]. Geological Bulletin of China. 2002, 21: 63-68.
    郑本兴. 青藏高原真的有大冰盖吗?[J]. 地质论评, 1989, 35(6): 543-551.
    Zheng Benxing. Did a large ice sheet really occur on the Qinghai-xizang plateau? [J]. Geological Review, 1989, 35(6): 543-551.
    郑景雄, 周尚哲, 王杰, 等. 东帕米尔高原冰川花岗岩漂砾风化穴初步研究 [J].华南师范大学学报(自然科学版), 2009, 3: 109-126.
    Zheng Jingxiong, Zhou Shangzhe, Wang Jie, et al. A preliminary study on tafoni developed on glacial granite boulders in eastern pamir[J]. Journal of South China Normal University (Natural Science Edition), 2009, 3: 109-126.
    周尚哲, 李吉均. 冰期之青藏高原新研究 [J]. 地学前缘, 2001, 8(1): 67-75.
    Zhou Shangzhe, Li Jijun. A new study on Qinghai-Tibet plateau in ice ages [J]. Earth Science Frontiers, 2001, 8(1): 67-75.
    Aitken M T. An Introduction to Optical Dating [M]. New York: Oxford University Press, 1998, 114-116.
    Andred M F, Hall K. Honeycomb development on Alexander island, glacial history ofGeorge VI Sound and palaeoclimatic implications [J]. Geomorphology, 2005, 65: 117-138.
    Derbyshire E, Shi Y, Li Jet al. Quaternary glaciation of Tibet: The geological evidence [J]. Quaternary Science Review, 1991, 10(6): 485-510.
    Ducea M N, Lutkov V, Minaev V T, et al. Building the Pamirs: The view from the underside [J]. Geology, 2003, 31: 849-852.
    Huinink H P, Pel L, Kopinga K. Simulating the growth of tafoni [J]. Earth Surface Processes and Land-forms, 2004, 29: 1225-1233.
    Liu Q, Tapponnier P, Bourjot L et al. Recent movement along the northern segment of the Karakorum fault system [A]. In: The Muji-Tashgorgan Graben. International Symposium on the Karakorum and Kunlun Mountains [C]. Chinese Academy of Sciences, Kashi, China, 1992.
    Lu Y C, Wang X L, Wintle A G. A new OSL chronology for dust accumulation in the last 130,000 yr for the Chinese Loess Plateau [J]. Quaternary Research, 2007, 67(1): 152-160.
    Matte P, Tapponnier P, Arnaud N et al. Tectonics of western Tibet, between the Tarim and the Indus [J]. Earth and Planetary Science Letters, 1996, 142(3-4): 311-330.
    Murray A S and Wintle A G. The single aliquot regenerative dose protocol: Potential for improvements in reliability [J]. Radiation Measurements, 2003, 37: 377-381.
    Ono Y, Liu D, Zhao Y. Paleoenvironment of Tibetan Plateau viewed fromglacial fluctuations in the north foot of the west Kunlun Mountains [J]. Journal of Geology in Japan, 1997, 106(2): 184-198.
    Rutter N. Problematic ice sheets [J]. Quaternary International, 1995, 38: 19-37.
    Seong Y B, Owen L A, Yi C L, et al. Geomorphology of anomalously high glaciated mountains at the northwestern end of Tibet: Muztag Ata and Kongur Shan [J]. Geomorphology, 2009, 103: 227-250.
    Strecker MR, Frisch W, Hamburger MW et al. Quaternary deformation in the eastern Pamirs, Tajikistan and Kyrgyzstan [J]. Tectonics, 1995, 14(5): 1061-1079.
  • Related Articles

Catalog

    Article views (2728) PDF downloads (2578) Cited by()

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return