Submarine cores record magma evolution toward a catastrophic eruption at Kikai Caldera

T Hanyu, N Seama, K Kaneko, Q Chang… - … Earth & Environment, 2024 - nature.com
Magma evolution toward a caldera-forming eruption remains uncertain in many cases owing
to the lack of successive volcanic records before catastrophic eruptions. Here we take an …

Magmatic evolution of the Kikai caldera revealed by zircon triple dating and its chemistry

H Ito - Scientific Reports, 2025 - nature.com
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 …

The selective geography of volcanism in oral traditions

L Franks, PD Nunn, A McCallum - Quaternary Research, 2024 - cambridge.org
Oral traditions describing details of ancient volcanic eruptions and their effects survive
throughout the inhabited world. Many such eruptions, especially those having catastrophic …

The proximal volcaniclastic materials of Fukutoku‐Oka‐no‐Ba in the Izu‐Bonin arc show contrasting characteristics to the drift pumice of the 2021 eruption

K Yoshida, Y Tamura, T Sato, E Tanaka, N Tada… - Island Arc, 2023 - Wiley Online Library
Abstract Fukutoku‐Oka‐no‐Ba is a submarine volcano located at 24° 17.1′ N/141° 28.9′
E in the Izu–Bonin arc, and is one of the most active volcanoes in Japan. This volcano …

Cogenetic Origin of Magmatic Enclaves in Peralkaline Felsic Volcanic Rocks from the Sanshui Basin, South China

P Chen, B Qian, Z Zhou, N Fang - Minerals, 2023 - mdpi.com
Centimeter-scale magmatic enclaves are abundant in peralkaline felsic volcanic rocks in the
Sanshui Basin. Their lithology is mainly syenite and syenitic porphyry, and they mainly …

A cristobalite-bearing syenitic enclave in a drift pumice derived from the 2021 eruption of Fukutoku-Oka-no-Ba

KK Yoshida, H Sawada, Y Maruya… - Journal of Mineralogical …, 2024 - jstage.jst.go.jp
Abstract The 2021 eruption of Fukutoku-Oka-no-Ba (FOB), which is a submarine volcano
located at the southern end of the Izu-Ogasawara arc, produced a large number of pumice …