火山灰全岩与原位分析差异：以四海龙湾记录的1 600年前金龙顶子火山喷发为例

孙春青; 游海涛; 刘嘉麒; 储国强; 刘强

doi:10.3799/dqkx.2016.007

Volume 41 Issue 1

Jan. 2016

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Sun Chunqing, You Haitao, Liu Jiaqi, Chu Guoqiang, Liu Qiang, 2016. Differences between Whole Rock and Insitu Analysis on Tephra: Evidence from the 1 600 a cal. BP Eruption of Jinlongdingzi Volcano. Earth Science, 41(1): 97-104. doi: 10.3799/dqkx.2016.007

Citation:

Sun Chunqing, You Haitao, Liu Jiaqi, Chu Guoqiang, Liu Qiang, 2016. Differences between Whole Rock and Insitu Analysis on Tephra: Evidence from the 1 600 a cal. BP Eruption of Jinlongdingzi Volcano. Earth Science, 41(1): 97-104. doi: 10.3799/dqkx.2016.007

Citation:

Sun Chunqing, You Haitao, Liu Jiaqi, Chu Guoqiang, Liu Qiang, 2016. Differences between Whole Rock and Insitu Analysis on Tephra: Evidence from the 1 600 a cal. BP Eruption of Jinlongdingzi Volcano. Earth Science, 41(1): 97-104. doi: 10.3799/dqkx.2016.007

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Differences between Whole Rock and Insitu Analysis on Tephra: Evidence from the 1 600 a cal. BP Eruption of Jinlongdingzi Volcano

doi: 10.3799/dqkx.2016.007

Sun Chunqing^{1,2
,},
You Haitao^2,3,
Liu Jiaqi^{1
,
,},
Chu Guoqiang¹,
Liu Qiang¹

1.
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
2.
Department of Earth Science, University of Chinese Academy of Sciences, Beijing 100049, China
3.
Key Laboratory of Computational Geodynamics of Chinese Academy of Sciences, College of Earth Science, University of Chinese Academy of Sciences, Beijing 100049, China

Received Date: 2015-07-02
Publish Date: 2016-01-15

Abstract

Abstract

Tephra layers with unknown ages are usually identified and fingerprinted by their glass compositions. But, such correlations may be problematic when they own heterogeneous glass compositions. Lake Sihailongwan locates in the Longgang volcanic field and its varved lacustrine sediments can preserve the volcanic products from surrounding areas. Additionally, its varve-chronology can provide an advantage chronological framework for recent geological events which are difficult to date by other dating methods. A core drilled from Lake Sihailongwan (core 2008) shows that there is a tephra layer at 78-79 cm and an age of AD 308 was assigned to it by varve-chronology. The volcanic glass exhibits a heterogeneous composition, ranging from basaltic trachyandesite to tephriphonolite. Such a heterogeneous characteristic of glass shards from this tephra layer can be clearly revealed by the biplots of FeO, TiO₂ and Al₂O₃ vs. MgO. For the applications to the tephrostratigraphy, whole rock analysis of tephra may be wrong and could not reflect the heterougeneous of primary magma while composition of glass is a better choice.
- lake Sihailongwan,
- tephra,
- volcanic glass,
- tephrochronology,
- Jinlongdingzi,
- petrology

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References(49)

References

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Differences between Whole Rock and Insitu Analysis on Tephra: Evidence from the 1 600 a cal. BP Eruption of Jinlongdingzi Volcano

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