华南中-晚二叠世之交碳酸盐岩磁学特征及环境意义

李波; 薛武强; 颜佳新; 朱宗敏; 王艳; 马志鑫

doi:10.3799/dqkx.2015.102

Volume 40 Issue 7

Jul. 2015

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Article Navigation > Earth Science > 2015 > 40(7): 1226-1236

Li Bo, Xue Wuqiang, Yan Jiaxin, Zhu Zongmin, Wang Yan, Ma Zhixin, 2015. Magnetic Properties of Middle-Late Permian Carbonates in South China and Their Environmental Significances. Earth Science, 40(7): 1226-1236. doi: 10.3799/dqkx.2015.102

Citation:

Li Bo, Xue Wuqiang, Yan Jiaxin, Zhu Zongmin, Wang Yan, Ma Zhixin, 2015. Magnetic Properties of Middle-Late Permian Carbonates in South China and Their Environmental Significances. Earth Science, 40(7): 1226-1236. doi: 10.3799/dqkx.2015.102

Citation:

Li Bo, Xue Wuqiang, Yan Jiaxin, Zhu Zongmin, Wang Yan, Ma Zhixin, 2015. Magnetic Properties of Middle-Late Permian Carbonates in South China and Their Environmental Significances. Earth Science, 40(7): 1226-1236. doi: 10.3799/dqkx.2015.102

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Magnetic Properties of Middle-Late Permian Carbonates in South China and Their Environmental Significances

doi: 10.3799/dqkx.2015.102

Li Bo^{1, 2, 3
,},
Xue Wuqiang³,
Yan Jiaxin^{3
,
,},
Zhu Zongmin³,
Wang Yan⁴,
Ma Zhixin⁵

1.
Guangzhou Marine Geological Survey, China Geological Survey, Guangzhou 510075, China
2.
Key Laboratory of Marine Mineral Resources, Ministry of Land and Resources, Guangzhou 510075, China
3.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
4.
Guangdong Nonferrous Metals Geological Exploration Institution, Guangzhou 510080, China
5.
Chengdu Institute of Geology and Mineral Resources, China Geological Survey, Chengdu 610081, China

Received Date: 2014-11-21
Publish Date: 2015-07-15

Abstract

Abstract

As a reliable proxy for paleoclimate and paleoenvironment, magnetic parameter could provide valuable data for the research of global environmental changes and climatic processes. A detailed study has been carried out on rock magnetism in order to reveal the change of climate and environment and its reasons across Guadalupian-Lopingian (G-L) boundary at Tieqiao section in Laibin area, Guangxi, China. The results show that the dominant magnetic minerals from Tieqiao section are paramagnetic minerals with a small amount of magnetite and hematite as well. There is a remarkable change in the properties of rock magnetism near the G-L boundary. Magnetic susceptibility increases first and then decreases. Magnetic carriers show the trend of being transformed from hard magnetic minerals (hematite) to soft magnetic mineral (magnetite) and then turning to hard magnetic minerals (hematite). All of these changes occur within 4m-thick strata interval above and below the G-L boundary, and synchronize with the fluctuation of sea-level and ancient seawater temperature during late Middle Permian. The significant changes in magnetic parameters for Middle-Late Permian carbonates suggest that the migration and conversion of magnetic minerals between different spheres in earth system has shifted, which resulted from the climatic and environmental changes. High sea-level during Late Guadalupian and Early Lopingian resulted in the decrease in terrigenous supply in South China. Therefore, the magnetic carriers in Tieqiao section mainly are hematite through aeolian transportation during this period. However, pronounced regression during the Middle-Late Permian transition led to the expansion of exposed land area. Meanwhile, land plants experienced widespread extinction, which led to increased sediment source. The magnetic carriers in contemporaneous sediments of Tieqiao section are mainly fluvial magnetite.
- South China,
- Tieqiao section,
- Guadalupian-Lopingian,
- rock magnetism,
- regression,
- sediment,
- paleoenvironment

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References(68)

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