柴达木盆地北缘古-新近纪河湖相沉积物颜色的气候意义

李星波; 季军良; 曹展铭; 王朴; 吴武军; 孙玲

doi:10.3799/dqkx.2020.329

Volume 46 Issue 9

Oct. 2021

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Article Navigation > Earth Science > 2021 > 46(9): 3278-3289

Li Xingbo, Ji Junliang, Cao Zhanming, Wang Pu, Wu Wujun, Sun Ling, 2021. The Climatic Significance of the Color of the Paleo-Neogene Fluvial and Lacustrine Sediments in the Northern Qaidam Basin. Earth Science, 46(9): 3278-3289. doi: 10.3799/dqkx.2020.329

Citation:

Li Xingbo, Ji Junliang, Cao Zhanming, Wang Pu, Wu Wujun, Sun Ling, 2021. The Climatic Significance of the Color of the Paleo-Neogene Fluvial and Lacustrine Sediments in the Northern Qaidam Basin. Earth Science, 46(9): 3278-3289. doi: 10.3799/dqkx.2020.329

Citation:

Li Xingbo, Ji Junliang, Cao Zhanming, Wang Pu, Wu Wujun, Sun Ling, 2021. The Climatic Significance of the Color of the Paleo-Neogene Fluvial and Lacustrine Sediments in the Northern Qaidam Basin. Earth Science, 46(9): 3278-3289. doi: 10.3799/dqkx.2020.329

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The Climatic Significance of the Color of the Paleo-Neogene Fluvial and Lacustrine Sediments in the Northern Qaidam Basin

doi: 10.3799/dqkx.2020.329

Li Xingbo^{1
,
,},
Ji Junliang^{1
,
,
,},
Cao Zhanming²,
Wang Pu³,
Wu Wujun³,
Sun Ling¹

1.
School of Geography and Information Engineering, China University of Geosciences, Wuhan 430078, China
2.
The Fifth Oil Production Plant, Qinghai Oilfield Branch of CNPC, Haixi 816499, China
3.
Research Institute of Petroleum Exploration and Development-Northwest, PetroChina, Lanzhou 730020, China

Received Date: 2020-08-13
Available Online: 2021-10-14
Publish Date: 2021-10-14

Abstract

Abstract

Cenozoic sediments up to 10 000 meters thick in the Qaidam basin recorded the Tibetan plateau uplift and paleoclimate changes. Based on the high-resolution magnetic polarity dating scale of the Dahonggou section in the northern margin of the basin,the color measurement of the Paleo-Neogene fluvial and lacustrine sediments in this section is performed. Furthermore,integrating the sedimentary facies,regional tectonic and paleoclimate records,this paper discusses the factors affecting the color parameters of river-lacustrine sediments and the climate evolution of the Qaidam basin during the Paleo-Neogene period. The research results show that the change of sediment color in Dahonggou section is basically consistent with the global temperature trend,indicating that temperature is the main factor affecting color parameters,especially the redness (a^*) value,but the sedimentary facies changes,especially changes in the oxidation-reduction environment above and below the water,also have an important influence on the color parameters. According to the changes of color parameters on the time scale,the climate change in the Qaidam basin has been divided into 8 stages: (a) hot and humid during 52.0-44.2 Ma,(b) gradually becomes dry in the fluctuation of dryness and wetness during 44.2-33.7 Ma,(c) further dries during 33.7-27.1 Ma,(d) gradually becomes wet during 27.1-19.7 Ma,(e) relatively dry during 19.7-17.0 Ma,(f) warm and humid during 17.0-13.3 Ma,(g) rapidly dries during 13.3-9.5 Ma,(h) becomes further arid during 9.5-7.0 Ma. The main factors affecting the Paleo-Neogene climate change in the Qaidam basin include global temperature,the Para-Tethys Sea,the uplift of the Tibetan plateau and the East Asian summer monsoon.
- Tibetan plateau,
- Qaidam basin,
- Paleo-Neogene,
- color,
- paleoclimate,
- stratigraphy

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References(50)

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The Climatic Significance of the Color of the Paleo-Neogene Fluvial and Lacustrine Sediments in the Northern Qaidam Basin

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