青海循化盆地晚更新世沉积序列与古气候

韩芳; 张克信; 韦一; 季军良; 徐亚东; 陈奋宁; 寇晓虎

doi:10.3799/dqkx.2010.098

Volume 35 Issue 5

Sep. 2010

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Article Navigation > Earth Science > 2010 > 35(5): 849-856

HAN Fang, ZHANG Ke-xin, WEI Yi, JI Jun-liang, Xu Ya-dong, CHEN Fen-ning, KOU Xiao-hu, 2010. Sedimentary Sequences and Paleoclimate of Late Pleistocene in Xunhua Basin, Qinghai Province. Earth Science, 35(5): 849-856. doi: 10.3799/dqkx.2010.098

Citation:

HAN Fang, ZHANG Ke-xin, WEI Yi, JI Jun-liang, Xu Ya-dong, CHEN Fen-ning, KOU Xiao-hu, 2010. Sedimentary Sequences and Paleoclimate of Late Pleistocene in Xunhua Basin, Qinghai Province. Earth Science, 35(5): 849-856. doi: 10.3799/dqkx.2010.098

Citation:

HAN Fang, ZHANG Ke-xin, WEI Yi, JI Jun-liang, Xu Ya-dong, CHEN Fen-ning, KOU Xiao-hu, 2010. Sedimentary Sequences and Paleoclimate of Late Pleistocene in Xunhua Basin, Qinghai Province. Earth Science, 35(5): 849-856. doi: 10.3799/dqkx.2010.098

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Sedimentary Sequences and Paleoclimate of Late Pleistocene in Xunhua Basin, Qinghai Province

doi: 10.3799/dqkx.2010.098

HAN Fang^{1, 2
,},
ZHANG Ke-xin^{1, 2, 3
,
,},
WEI Yi²,
JI Jun-liang^{1, 2},
Xu Ya-dong^{1, 2},
CHEN Fen-ning⁴,
KOU Xiao-hu^{1, 3}

1.
Key Laboratory of Biogeology and Environmental Geology of Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
Faulty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
Geological Survey of China University of Geosciences, Wuhan 430074, China
4.
Xi'an Institute of Geology and Mineral Resources, Xi'an 710054, China

Received Date: 2010-05-31
Publish Date: 2010-09-01

Abstract

Abstract

Sedimentological analyses of the third terrace along the banks of the Yellow River in Xunhua basin have yielded results that have more than regional significance. They are concerned with the reaction of rivers to climatic changes in the Pleistocene. Based on the field investigations, granularity, magnetic susceptibility, palynological records and optically stimulated luminescence (OSL) dating, the age of the third terrace was revealed. It shows that the Yellow River incised during the transition from interglacial to glacial. Evidences show that the paleoclimate and environment in Xunhua basin during the Late Pleistocene can be roughly divided into six stages: (1) 120—114 ka, the climate was warm and moist; (2) 114—105 ka, the climate turned cool and dry; (3) 105—98 ka, the climate was relatively warm and humid; (4) 98-85 ka, the climate turned cool and temperature; (5) 85—75 ka, the climate was warm and humid; (6) 75—63 ka, the climate was cold and dry, which can be compared with high-resolution ice core and marine oxygen isotope climate series.
- river terrace,
- granularity,
- magnetic susceptibility,
- environment evolution,
- Xunhua basin

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References(43)

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Sedimentary Sequences and Paleoclimate of Late Pleistocene in Xunhua Basin, Qinghai Province

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