朝鲜平南盆地寒武系黄州群和法洞群的碳同位素漂移事件

金明哲; 杨正赫; 彭澎; 张志越; 朴贤旭; 卞创男; 朴雄; 郑哲寿; 翟明国

doi:10.3799/dqkx.2018.107

Volume 43 Issue 11

Nov. 2018

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Article Navigation > Earth Science > 2018 > 43(11): 4096-4108

Kim Myong-Chol, Yang Jong-Hyok, Peng Peng, Zhang Zhiyue, Park Hyon-Uk, Byon Chang-Nam, Park Ung, Jong Chol-Su, Zhai Mingguo, 2018. Carbon Isotope Excursions of Cambrian Hwangju and Bopdong Groups in Pyongnam Basin, Korean Peninsula. Earth Science, 43(11): 4096-4108. doi: 10.3799/dqkx.2018.107

Citation:

Kim Myong-Chol, Yang Jong-Hyok, Peng Peng, Zhang Zhiyue, Park Hyon-Uk, Byon Chang-Nam, Park Ung, Jong Chol-Su, Zhai Mingguo, 2018. Carbon Isotope Excursions of Cambrian Hwangju and Bopdong Groups in Pyongnam Basin, Korean Peninsula. Earth Science, 43(11): 4096-4108. doi: 10.3799/dqkx.2018.107

Citation:

Kim Myong-Chol, Yang Jong-Hyok, Peng Peng, Zhang Zhiyue, Park Hyon-Uk, Byon Chang-Nam, Park Ung, Jong Chol-Su, Zhai Mingguo, 2018. Carbon Isotope Excursions of Cambrian Hwangju and Bopdong Groups in Pyongnam Basin, Korean Peninsula. Earth Science, 43(11): 4096-4108. doi: 10.3799/dqkx.2018.107

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Carbon Isotope Excursions of Cambrian Hwangju and Bopdong Groups in Pyongnam Basin, Korean Peninsula

doi: 10.3799/dqkx.2018.107

1.
Institute of Geology, State Academy of Sciences, Pyongyang 3812100, DPR Korea
2.
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
3.
University of Chinese Academy of Sciences, Beijing 100049, China
4.
University of Pyongsong Coal Industry, Pyongsong 999093, DPR Korea

Received Date: 2018-05-23
Publish Date: 2018-11-15

Abstract

Abstract

The Cambrian strata in the Pyongnam basin in Korea include the Hwangju Group and the lower Bopdong Group. To compare the Cambrian strata of this basin with those in the adjacent regions and areas beyond, this paper performs biostratigraphy research and isotope analysis of carbon and oxygen isotopes of typical carbonates of the Hwangju Group (the Pyongsan, Junghwa, Hukgyo and Rimchon Fms.) and the lower Bopdong Group (the Mujin and Kopung Fms.). Based on biostratigraphic research, the Pyongsan and Junghua Formations should be no lower than Stage 3 and Stage 4, respectively. δ¹³C values in the Pyongsan Fm. range from 0 to -3.1‰, Junghua -4.7‰ to 2.0‰, Hukgyo -1.0‰ to 2.4‰, Rimchon -2.6‰ to 0.4‰, Mujin -1.3‰ to 0.4‰, and Kopung -1.0‰ to 2.4‰. Synthetically, it is argued that the Pyongsan, Junghua and Hukgyo Fms. belong to Stages 3-4 of Cambrian, the Rimchon Fm. is around the boundary of Series 2 and Miaoling Series, and the Kopung Fm. belongs to the Furong Series of Cambrian. And the three carbon excursions in the upper Junghwa-Hukgyo Fm. (positive), the lower Rimchon Fm. (negative) and the middle Kopung Fm. (positive) are comparable to the global events of the mIngxinsi carbon isotope excursion, redlichiid-olenellid extinction carbon isotope excursion and steptoean positive carbon isotope excursion, respectively.
- North China craton,
- Korean Peninsula,
- Pyongnam basin,
- Cambrian,
- carbon isotope excursion,
- biostratigraphy

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References(92)

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