Magmatic evolution of the Kikai caldera revealed by zircon triple dating and its chemistry
Abstract Reconstructing the volcanic history of the Kikai caldera, a large active volcano that produced a ~ 160 km3 eruption at 7.3 ka off the southern coast of Kyushu Island (southwest Japan), is crucial to assess potential future volcanic hazards at both regional and global scales. However, reveal...
Saved in:
Main Author: | |
---|---|
Format: | Article |
Language: | English |
Published: |
Nature Portfolio
2025-01-01
|
Series: | Scientific Reports |
Online Access: | https://doi.org/10.1038/s41598-025-87264-5 |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
_version_ | 1832585692550529024 |
---|---|
author | Hisatoshi Ito |
author_facet | Hisatoshi Ito |
author_sort | Hisatoshi Ito |
collection | DOAJ |
description | Abstract Reconstructing the volcanic history of the Kikai caldera, a large active volcano that produced a ~ 160 km3 eruption at 7.3 ka off the southern coast of Kyushu Island (southwest Japan), is crucial to assess potential future volcanic hazards at both regional and global scales. However, revealing its volcanic history before the 7.3 ka eruption has been challenging due to the caldera being mostly submerged. In this study, we present evidence that the Kikai caldera erupted a geochemically distinct silicic lava at ~ 250 ka by using zircon triple (U-Pb, Th-Pb, U-Th) dating and its chemistry. The presence of 1.5–1.0 Ma zircons in the 7.3 ka eruption deposits suggests that zircon crystallization in the Kikai caldera began during this period. We further infer large eruptions occurred around 0.7–0.6 Ma, suggesting that the Kikai caldera may have experienced at least 5 major eruptions during its 1.0–1.5-million-year magmatic evolution. |
format | Article |
id | doaj-art-21d60f44ae954e268110300cee7e071c |
institution | Kabale University |
issn | 2045-2322 |
language | English |
publishDate | 2025-01-01 |
publisher | Nature Portfolio |
record_format | Article |
series | Scientific Reports |
spelling | doaj-art-21d60f44ae954e268110300cee7e071c2025-01-26T12:34:14ZengNature PortfolioScientific Reports2045-23222025-01-0115111210.1038/s41598-025-87264-5Magmatic evolution of the Kikai caldera revealed by zircon triple dating and its chemistryHisatoshi Ito0Central Research Institute of Electric Power IndustryAbstract Reconstructing the volcanic history of the Kikai caldera, a large active volcano that produced a ~ 160 km3 eruption at 7.3 ka off the southern coast of Kyushu Island (southwest Japan), is crucial to assess potential future volcanic hazards at both regional and global scales. However, revealing its volcanic history before the 7.3 ka eruption has been challenging due to the caldera being mostly submerged. In this study, we present evidence that the Kikai caldera erupted a geochemically distinct silicic lava at ~ 250 ka by using zircon triple (U-Pb, Th-Pb, U-Th) dating and its chemistry. The presence of 1.5–1.0 Ma zircons in the 7.3 ka eruption deposits suggests that zircon crystallization in the Kikai caldera began during this period. We further infer large eruptions occurred around 0.7–0.6 Ma, suggesting that the Kikai caldera may have experienced at least 5 major eruptions during its 1.0–1.5-million-year magmatic evolution.https://doi.org/10.1038/s41598-025-87264-5 |
spellingShingle | Hisatoshi Ito Magmatic evolution of the Kikai caldera revealed by zircon triple dating and its chemistry Scientific Reports |
title | Magmatic evolution of the Kikai caldera revealed by zircon triple dating and its chemistry |
title_full | Magmatic evolution of the Kikai caldera revealed by zircon triple dating and its chemistry |
title_fullStr | Magmatic evolution of the Kikai caldera revealed by zircon triple dating and its chemistry |
title_full_unstemmed | Magmatic evolution of the Kikai caldera revealed by zircon triple dating and its chemistry |
title_short | Magmatic evolution of the Kikai caldera revealed by zircon triple dating and its chemistry |
title_sort | magmatic evolution of the kikai caldera revealed by zircon triple dating and its chemistry |
url | https://doi.org/10.1038/s41598-025-87264-5 |
work_keys_str_mv | AT hisatoshiito magmaticevolutionofthekikaicalderarevealedbyzircontripledatinganditschemistry |