华北盆地南部济源地区和尚沟组凝灰岩锆石U-Pb定年及其地层学意义

杨文涛; 张鸿禹; 方特; 冯婉莹; 彭深远

doi:10.3799/dqkx.2021.211

Volume 48 Issue 10

Oct. 2023

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Article Navigation > Earth Science > 2023 > 48(10): 3770-3780

Yang Wentao, Zhang Hongyu, Fang Te, Feng Wanying, Peng Shenyuan, 2023. Zircon U-Pb Age and Stratigraphic Significance of Tuff in Heshanggou Formation, Southern North China Basin. Earth Science, 48(10): 3770-3780. doi: 10.3799/dqkx.2021.211

Citation:

Yang Wentao, Zhang Hongyu, Fang Te, Feng Wanying, Peng Shenyuan, 2023. Zircon U-Pb Age and Stratigraphic Significance of Tuff in Heshanggou Formation, Southern North China Basin. Earth Science, 48(10): 3770-3780. doi: 10.3799/dqkx.2021.211

Citation:

Yang Wentao, Zhang Hongyu, Fang Te, Feng Wanying, Peng Shenyuan, 2023. Zircon U-Pb Age and Stratigraphic Significance of Tuff in Heshanggou Formation, Southern North China Basin. Earth Science, 48(10): 3770-3780. doi: 10.3799/dqkx.2021.211

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Zircon U-Pb Age and Stratigraphic Significance of Tuff in Heshanggou Formation, Southern North China Basin

doi: 10.3799/dqkx.2021.211

1.
School of Resource and Environment, Henan Polytechnic University, Jiaozuo 454003, China
2.
Collaborative Innovation Center of Coalbed Methane and Shale Gas for Central Plains Economic Region, Henan Province, Jiaozuo 454003, China
3.
Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China

Received Date: 2021-10-10
Available Online: 2023-10-31
Publish Date: 2023-10-25

Abstract

Abstract

In order to constrain the timing for biological recovery and climate change after the Permian-Triassic extinction in North China basin, in this contribution it applies zircon LA-ICP-MS dating of the newly discovered tuff layer in the upper part of the Heshanggou Formation in Jiyuan area. Some zircons occur as short cylindrical shape, with a few elongated grains. All zircons were not rounded, and showed obvious oscillatory zoning characteristics under a cathodoluminescence microscope. After removing zircons with enriched LREE, the remaining zircons showed a weighted mean U-Pb age of 244.6±2.8 Ma. The results show that the stratigraphic age of Heshanggou Formation spanned to the Middle Triassic Anisian age. The new age constrains that the terrestrial ecosystem in North China Basin was fully rebuilt during the Anisian after recovered during the Olenekian, which is consistent with the recovery time of marine ecosystem. The paleoclimate transition from extreme greenhouse to medium greenhouse also occurred in the Anisian age, which is consistent with the continuous global cooling trend in the Middle Triassic.
- Heshanggou Formation,
- Triassic,
- tuff,
- biological recovery,
- paleoclimate,
- climate change,
- stratigraphy

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References(55)

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