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Article Navigation >  Acta Sedimentologica Sinica  > 1997  >  15(1): 168-171

Qin Zuodong, Feng Qi. Relationship Between Holocene Sediment snd Climatic Change in the Plain Area of Northern Taklimakan Desert kk Take Xiaotang Section As Example[J]. Acta Sedimentologica Sinica, 1997, 15(1): 168-171.
Citation: Qin Zuodong, Feng Qi. Relationship Between Holocene Sediment snd Climatic Change in the Plain Area of Northern Taklimakan Desert kk Take Xiaotang Section As Example[J]. Acta Sedimentologica Sinica, 1997, 15(1): 168-171.
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Relationship Between Holocene Sediment snd Climatic Change in the Plain Area of Northern Taklimakan Desert kk Take Xiaotang Section As Example

  • 1 Shanxi Normal University Linfen 041004;

  • 2 Institute of Glaciology and Geocryology Lanzhou 730000

  • Received Date: 1996-06-12
  • Publish Date: 1997-03-10
  • By analyzing the Characteristics of granular and chemical compositions of the Xiaotang profile, he change of Holocene climate in the plain area of northern Taklimakan Desert has been revealed. The sedi-mentary fades mainly consists of clay formed by fluvial washing and aeolian layer caused by wind. Claymaterials coincide with the typical fades of modern river, while the aeolian deposit is similar to the fea-tures of present driftgand. Movement and conversion of elements in sedimentary layers are clowly relat-ed with the climate and hydrographic dandlitions at that time. The- dry and high temperature- dry climate since Holocene has been crented under the background of global climate with impact of localdesert landscape. meanwhile, the windy and dry climate is produced. It is objectively recorded in sedi-mentary fades.
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    4 李天杰郑应顺等.土壤地理学.北京:高等教育出版社.1987. 17 一26.

    5 黄汝昌.陆相沉积中古气候演变及元素的迁移、采集和演化.中国

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    6 司任振球.塔干地区干湿波动与全球温度变化关系探讨.中国沙漠 1994, 14( 2).

    7 李保生末次冰期以来塔里术盆地沙漠黄土的沉积与演化.中一 科学(B).1993, ( 6).

    8 董光荣.高尚玉金炯等.青海共和盆地土地沙漠化与防治. 经.北京:科学出版社，1993, 74- 100.
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  • Received:  1996-06-12
  • Published:  1997-03-10

Relationship Between Holocene Sediment snd Climatic Change in the Plain Area of Northern Taklimakan Desert kk Take Xiaotang Section As Example

  • 1 Shanxi Normal University Linfen 041004;
  • 2 Institute of Glaciology and Geocryology Lanzhou 730000
  • Received Date: 1996-06-12
  • Publish Date: 1997-03-10

Abstract: By analyzing the Characteristics of granular and chemical compositions of the Xiaotang profile, he change of Holocene climate in the plain area of northern Taklimakan Desert has been revealed. The sedi-mentary fades mainly consists of clay formed by fluvial washing and aeolian layer caused by wind. Claymaterials coincide with the typical fades of modern river, while the aeolian deposit is similar to the fea-tures of present driftgand. Movement and conversion of elements in sedimentary layers are clowly relat-ed with the climate and hydrographic dandlitions at that time. The- dry and high temperature- dry climate since Holocene has been crented under the background of global climate with impact of localdesert landscape. meanwhile, the windy and dry climate is produced. It is objectively recorded in sedi-mentary fades.

Qin Zuodong, Feng Qi. Relationship Between Holocene Sediment snd Climatic Change in the Plain Area of Northern Taklimakan Desert kk Take Xiaotang Section As Example[J]. Acta Sedimentologica Sinica, 1997, 15(1): 168-171.
Citation: Qin Zuodong, Feng Qi. Relationship Between Holocene Sediment snd Climatic Change in the Plain Area of Northern Taklimakan Desert kk Take Xiaotang Section As Example[J]. Acta Sedimentologica Sinica, 1997, 15(1): 168-171.
shu

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