华北房山景儿峪组顶部古风化壳常量元素地球化学特征及其古气候意义

马晓晨; 王家生; 陈粲; 王舟

doi:10.3799/dqkx.2018.235

Volume 43 Issue 11

Nov. 2018

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Ma Xiaochen, Wang Jiasheng, Chen Can, Wang Zhou, 2018. Major Element Compositions and Paleoclimatic Implications of Paleo-Regolith on Top Jingeryu Formation in Fangshan, North China. Earth Science, 43(11): 3853-3872. doi: 10.3799/dqkx.2018.235

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Ma Xiaochen, Wang Jiasheng, Chen Can, Wang Zhou, 2018. Major Element Compositions and Paleoclimatic Implications of Paleo-Regolith on Top Jingeryu Formation in Fangshan, North China. Earth Science, 43(11): 3853-3872. doi: 10.3799/dqkx.2018.235

Citation:

Ma Xiaochen, Wang Jiasheng, Chen Can, Wang Zhou, 2018. Major Element Compositions and Paleoclimatic Implications of Paleo-Regolith on Top Jingeryu Formation in Fangshan, North China. Earth Science, 43(11): 3853-3872. doi: 10.3799/dqkx.2018.235

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Major Element Compositions and Paleoclimatic Implications of Paleo-Regolith on Top Jingeryu Formation in Fangshan, North China

doi: 10.3799/dqkx.2018.235

Ma Xiaochen^{1,2
,},
Wang Jiasheng^{1,2
,
,},
Chen Can^1,2,
Wang Zhou^1,2

1.
State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
College of Marine Science and Technology, China University of Geosciences, Wuhan 430074, China

Received Date: 2018-07-09
Publish Date: 2018-11-15

Abstract

Abstract

The geochemical composition of regolith can reflect its development processes and the background climatic characteristics of weathering processes, and geochemical compositions of the paleo-regolith formed in earth history can reveal the type of paleo-regolith and record paleoclimatic changes. The record between the Late Neoproterozoic (the Jingeryu Formation) and the Cambrian (the Fujunshan Formation) in North China is a stratigraphic hiatus due to the tectonic uplift and erosion. A typical paleo-regolith widely occurs and is supposed to have recorded paleoclimate changes during the Late Neoproterozoic to Early Cambrian. According to the compositions of major elements, enrichment in elemental migrations and coefficient of weathering distribution of paleo-regolith on the topmost Jingeryu Formation in the Fangshan area, North China, this study suggests that:(1) The major element compositions of the paleo-regolith on the topmost Jingeryu Formation are dominated by the elements of SiO₂, Al₂O₃, TFe₂O₃, CaO. And the elements of Al₂O₃, TFe₂O₃, TiO₂, K₂O are relatively concentrated in the middle-to-upper parts of the regolith while the SiO₂ is slightly lost. (2) The vertical variations of geochemical proxies such as SiO₂/Al₂O₃, SiO₂/(Al₂O₃+TFe₂O₃), chemical index of alteration (CIA), residual coefficient and BA value indicate that the paleo-regolith should have been formed under a warm and humid condition with moderate chemical weathering. The chemical weathering might have gone through an evolution from weak to strong and again to weak in degree. (3) Compared to the element geochemical characteristics of modern regolith on the topmost carbonate settings from Hunan, Guizhou and Yunnan, it is inferred that the paleo-regolith on the topmost Jingeryu Formation has relatively lower deficiency in Si and enrichment in Fe and Al. Consequently, by comprehensive analysis of the geochemical characteristics of paleo-regolith on the topmost Jingeryu Formation and changes in paleo-latitude of the North China block from the Late Neoproterozoic to the Cambria, it is proposed that the paleo-regolith on the topmost Jingeryu Formation might have been formed under conditions of a warm and humid tropical to subtropical climate siallite-clay regolith.
- geochemistry,
- paleo-regolith,
- paleoclimate,
- Fangshan,
- Jingeryu Formation

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References(98)

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Major Element Compositions and Paleoclimatic Implications of Paleo-Regolith on Top Jingeryu Formation in Fangshan, North China

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