Understanding degassing pathways along the 1886 Tarawera (New Zealand) volcanic fissure by combining soil and lake CO2 fluxes
CO2 flux measurements are often used to monitor volcanic systems, understand the cause of volcanic unrest, and map sub-surface structures. Currently, such measurements are incomplete at Tarawera (New Zealand), which erupted with little warning in 1886 and produced a ∼17 km long fissure. We combine n...
Saved in:
Main Authors: | Hughes, Ery C., Mazot, Agnes, Kilgour, Geoff, Asher, Cameron, Michelini, Marco, Britten, Karen, Chardot, Lauriane, Feisel, Yves, Werner, Cynthia |
---|---|
Other Authors: | Earth Observatory of Singapore |
Format: | Article |
Language: | English |
Published: |
2020
|
Subjects: | |
Online Access: | https://hdl.handle.net/10356/137019 |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Institution: | Nanyang Technological University |
Language: | English |
Similar Items
-
On depressurization of volcanic magma reservoirs by passive degassing
by: Newhall, Chris, et al.
Published: (2015) -
CO2 discharge from the bottom of volcanic Lake Rotomahana, New Zealand
by: Mazot, Agnes, et al.
Published: (2014) -
Degassing during quiescence as a trigger of magma ascent and volcanic eruptions
by: Girona, Társilo, et al.
Published: (2016) -
Rise from beneath: understanding volatile degassing in distinct volcanic systems through modelling
by: Yeo, Jeanne
Published: (2024) -
Necking and fracking may explain stationary seismicity and full degassing in volcanic silicic spine extrusion
by: Jiao, Liqing, et al.
Published: (2019)