Composition and flux of explosive gas release at LUSI mud volcano (East Java, Indonesia)

CO2 flux from Javanese mud volcanism

Studying the quantity and origin of CO2 emitted by back-arc mud volcanoes is critical to correctly model fluid-dynamical, thermodynamical, and geochemical processes that drive their activity and to constrain their role in the global geochemical carbon cycle. We measured CO2 fluxes of the Bledug Kuwu mud volcano on the Kendeng Fold and thrust belt in the back arc of Central Java, Indonesia, usin...

Megafauna at the Håkon Mosby Mud Volcano

Introduction Conclusions References

A prediction of the longevity of the Lusi mud eruption, Indonesia

Application of the Monopole Source to Quantify Explosive Flux During Vulcanian Explosions at Sakurajima Volcano (Japan)

Flux measurements of explosive degassing using a yearlong hydroacoustic record at an erupting submarine volcano

[1] The output of gas and tephra from volcanoes is an inherently disorganized process that makes reliable flux estimates challenging to obtain. Continuous monitoring of gas flux has been achieved in only a few instances at subaerial volcanoes, but never for submarine volcanoes. Here we use the first sustained (yearlong) hydroacoustic monitoring of an erupting submarine volcano (NW Rota-1, Maria...