Distribution, geochemistry and age of the Millennium eruptives of Changbaishan volcano, Northeast China – A review

doi:10.1007/s11707-014-0149-x

Front. Earth Sci.

2014, Vol. 8

Issue (2) : 216-230 https://doi.org/10.1007/s11707-014-0149-x

REVIEW ARTICLE

Distribution, geochemistry and age of the Millennium eruptives of Changbaishan volcano, Northeast China – A review

Chunqing SUN^1,³, Haitao YOU²(

), Jiaqi LIU¹(

), Xin LI⁴, Jinliang GAO^1,³, Shuangshuang CHEN^1,³

¹. Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
². Key Laboratory of Computational Geodynamics of Chinese Academy of Sciences, College of Earth Science, University of Chinese Academy of Sciences, Beijing 100049, China
³. University of Chinese Academy of Sciences, Beijing 100049, China
⁴. Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China

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Abstract

Large explosive volcanic eruptions generate extensive regional tephra deposits that provide favorable conditions for identifying the source of volcanoes, comparing the sedimentary strata of a region and determining their ages. The tephra layer, referred to as B-Tm, generated by the Millennium eruption of Changbaishan volcano, is widely distributed in Northeast China, Japan, D.P.R. Korea, and the nearby coastal area of Russia. It forms part of the widespread northeast Asian strata and is significant for establishing an isochronal stratigraphic framework. However, research on the temporal characterization and stratigraphic correlation of associated strata using this tephra layer is mainly concentrated in and near Japan. In northeastern China, this tephra layer is seldom seen and its application in stratigraphic correlations is even rarer. More importantly, the determination of accurate ages for both distal and proximal tephras has been debated, leading to controversy in discussions of its environmental impacts. Stratigraphic records from both distal and proximal Changbaishan ash show that this eruption generally occurred between 1,012 and 1,004 cal yr BP. Geochemical comparison between Changbaishan ash and the Quaternary widespread ash around Japan illustrates that Changbaishan ash is a continuous composition from rhyolitic to trachytic and its ratio of FeO_T to CaO is usually greater than 4, which can be used as a distinguishing identifier among worldwide contemporary eruptions.

Keywords Millennium eruption Changbaishan volcano tephrochronology B-Tm tephra

Corresponding Author(s): Haitao YOU,Jiaqi LIU

Issue Date: 24 June 2014

Cite this article:

Chunqing SUN,Haitao YOU,Jiaqi LIU, et al. Distribution, geochemistry and age of the Millennium eruptives of Changbaishan volcano, Northeast China – A review[J]. Front. Earth Sci., 2014, 8(2): 216-230.

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https://academic.hep.com.cn/fesci/EN/10.1007/s11707-014-0149-x
https://academic.hep.com.cn/fesci/EN/Y2014/V8/I2/216

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