The formation of explosive volcanos at the circum-Pacific convergent margin during the last century

Fanfan TIAN; Kun WANG; Guozhi XIE; Weidong SUN

doi:10.1007/s00343-022-2276-x

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The formation of explosive volcanos at the circum-Pacific convergent margin during the last century

Geology | Updated：2023-04-27

- The formation of explosive volcanos at the circum-Pacific convergent margin during the last century
- The formation of explosive volcanos at the circum-Pacific convergent margin during the last century
- 海洋湖沼学报（英文） 2023年41卷第1期页码：75-83
- Affiliations：
  
  1.Center of Deep Sea Research, Center of Ocean Mega Science, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
  2.Deep-Sea Multidisciplinary Research Center, Laoshan Laboratory, Qingdao 266237, China
  3.University of Chinese Academy of Sciences, Beijing 100049, China
- Author bio：
  
  Weidong SUN, E-mail: weidongsun@qdio.ac.cn
- Funds：
  
  the Strategic Priority Research Program of the Chinese Academy of Sciences(XDA22050103);the Taishan Scholar Program of Shandong(ts201712075);© Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag GmbH Germany, part of Springer Nature 2023
- DOI：10.1007/s00343-022-2276-x
  中图分类号：
- 收稿：2022-07-11，
  
  录用：2022-8-26，
  
  网络首发：2022-08-30，
  
  纸质出版：2023-01
- Accepted：
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The formation of explosive volcanos at the circum-Pacific convergent margin during the last century[J]. 海洋湖沼学报（英文）, 2023,41(1):75-83.

Fanfan TIAN, Kun WANG, Guozhi XIE, et al. The formation of explosive volcanos at the circum-Pacific convergent margin during the last century[J]. Journal of Oceanology and Limnology, 2023, 41(1): 75-83.
The formation of explosive volcanos at the circum-Pacific convergent margin during the last century[J]. 海洋湖沼学报（英文）, 2023,41(1):75-83. DOI： 10.1007/s00343-022-2276-x.

Fanfan TIAN, Kun WANG, Guozhi XIE, et al. The formation of explosive volcanos at the circum-Pacific convergent margin during the last century[J]. Journal of Oceanology and Limnology, 2023, 41(1): 75-83. DOI： 10.1007/s00343-022-2276-x.

摘要

Abstract

The circum-Pacific convergent margin is known as "the Ring of Fire"

with abundant volcano eruptions. Large eruptions are rare but very disastrous. It remains obscure how are large explosive volcanos formed and where are the danger zones. Three largest eruptions since 1900

the Hunga Tonga-Hunga Ha'apai

the Mt. Pinatubo

and the Novarupta were found to be associated with subductions of volatile-rich sediments and located close to slab windows. Among them

the Hunga Tonga-Hunga Ha'apai is close to subducting seamount chains; the Mt. Pinatubo is right next to subducting fossil ridges. Both seamount chains and fossil ridges have water depths much shallower than the carbonate compensation depths (CCD) in the Pacific Ocean. Seismic image shows that a seamount is subducting towards the Novarupta volcano. Subduction of volatile-rich sediments and a slab window nearby are the two most important favorable conditions for catastrophic eruptions. Slab windows expose the mantle wedge to the hot asthenosphere

which increases the temperature and dramatically promotes the partial melting of the carbonate-fluxed domains

forming volatile-rich magmas that powered explosive eruptions.

关键词

Keywords

references

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