Image_3_Understanding Degassing Pathways Along the 1886 Tarawera (New Zealand) Volcanic Fissure by Combining Soil and Lake CO2 Fluxes.PDF

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Image_3_Understanding Degassing Pathways Along the 1886 Tarawera (New Zealand) Volcanic Fissure by Combining Soil and Lake CO2 Fluxes.PDF

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Description

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 new soil CO2 flux and C isotope measurements of Tarawera with previous data from Rotomahana and Waimangu (regions also along the 1886 fissure) to fingerprint the CO2 source, understand the current p...

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Image

Date created

24 Oct, 2019

Creator

Ery C. Hughes / Agnes Mazot / Geoff Kilgour / Cameron Asher / Marco Michelini / Karen Britten / Lauriane Chardot / Yves Feisel / Cynthia Werner

URL

https://figshare.com/articles/figure/Image_3_Understanding_Degassing_Pathways_Along_the_1886_Tara...

Related subjects

Tarawera / Waimangu / Rotomahana / CO2 flux / carbon isotopes / volcanic degassing / gas permeability / Solid Earth Sciences / Climate Science / Evolutionary Impacts of Climate Change / Atmospheric Sciences not elsewhere classified / Exploration Geochemistry / Inorganic Geochemistry / Isotope Geochemistry / Organic Geochemistry / Geochemistry not elsewhere classified / Igneous and Metamorphic Petrology / Ore Deposit Petrology / Palaeontology (incl. Palynology) / Structural Geology / Tectonics / Volcanology / Geology not elsewhere classified / Seismology and Seismic Exploration / Glaciology / Hydrogeology / Natural Hazards / Quaternary Environments / Earth Sciences not elsewhere classified

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