柴北缘西段古-新近纪古气候演化

贾艳艳; 邢学军; 孙国强; 史基安; 刘士杰

doi:10.3799/dqkx.2015.176

Volume 40 Issue 12

Dec. 2015

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Jia Yanyan, Xing Xuejun, Sun Guoqiang, Shi Ji'an, Liu Shijie, 2015. The Paleogene-Neogene Paleoclimate Evolution in Western Sector of Northern Margin of Qaidam Basin. Earth Science, 40(12): 1955-1967. doi: 10.3799/dqkx.2015.176

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Jia Yanyan, Xing Xuejun, Sun Guoqiang, Shi Ji'an, Liu Shijie, 2015. The Paleogene-Neogene Paleoclimate Evolution in Western Sector of Northern Margin of Qaidam Basin. Earth Science, 40(12): 1955-1967. doi: 10.3799/dqkx.2015.176

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The Paleogene-Neogene Paleoclimate Evolution in Western Sector of Northern Margin of Qaidam Basin

doi: 10.3799/dqkx.2015.176

Jia Yanyan^{1, 2, 3, 4
,},
Xing Xuejun⁵,
Sun Guoqiang^{1, 2},
Shi Ji'an^{1, 2
,
,},
Liu Shijie⁴

1.
Key Laboratory of Petroleum Resources of Gansu Province, Lanzhou 730000, China
2.
Key Laboratory of Petroleum Resources Research, Chinese Academy of Sciences, Lanzhou 730000, China
3.
University of Chinese Academy of Sciences, Beijing 100049
4.
Research Institute of Petroleum Exploration & Development, Jidong Oilfield Company, PetroChina, Tangshan 063004, China
5.
Research Institute of Drilling & Production Technology, Jidong Oilfield Company, PetroChina, Tangshan 063004, China

Received Date: 2015-02-24
Publish Date: 2015-12-15

Abstract

Abstract

Paleoclimate is one of the main sedimentary dynamic factors for the formation of sequence stratigraphy of continental basin. The Paleogene-Neogene paleoclimate evolution in western sector of northern margin of Qaidam basin and surrounding areas was complex, but now paleoclimate evolution remains controversial. The elements, TOC and C, O stable isotope content of key well cores and rock debris were measured by geochemical methods. Correlation analysis between paleoclimate indicators shows that: Sr/Ba, Rb/Sr, Sr/Ca, TOC and chloride ion content can be the paleoclimate recovery indicators, however, δ¹³C and δ¹⁸O can't indicate the paleoclimate evolution process in the study area. Analysis of rock debris chloride ion data of key wells shows that the paleoclimate evolution process in the study area is arid-humid-arid. From Lulehe Formation to upper Shangganchaigou Formation, the paleoclimate gradually evolved from arid to humid climate, including 7 cycles, and lake water salinity decreased, the climate was humid and water was brackish overall. From Shangganchaigou Formation to Shizigou Formation, the paleoclimate evolved from humid to arid, including 12 cycles, and brackish water changed to medium brackish water.
- western sector of northern margin of Qaidam basin,
- Paleogene-Neogene,
- geochemistry,
- paleoclimate,
- evolution

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References(88)

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The Paleogene-Neogene Paleoclimate Evolution in Western Sector of Northern Margin of Qaidam Basin

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