Deep carbon cycling over the past 200 million years: a review of fluxes in different tectonic settings
Carbon is a key control on the surface chemistry and climate of Earth. Significant volumes of
carbon are input to the oceans and atmosphere from deep Earth in the form of degassed …
carbon are input to the oceans and atmosphere from deep Earth in the form of degassed …
[HTML][HTML] Volcanoes and the environment: Lessons for understanding Earth's past and future from studies of present-day volcanic emissions
TA Mather - Journal of Volcanology and Geothermal Research, 2015 - Elsevier
Volcanism has affected the environment of our planet over a broad range of spatial (local to
global) and temporal (< 1 yr to 100s Myr) scales and will continue to do so. As well as …
global) and temporal (< 1 yr to 100s Myr) scales and will continue to do so. As well as …
Massive and prolonged deep carbon emissions associated with continental rifting
Carbon from Earth's interior is thought to be released to the atmosphere mostly via
degassing of CO2 from active volcanoes,,,. CO2 can also escape along faults away from …
degassing of CO2 from active volcanoes,,,. CO2 can also escape along faults away from …
Carbon dioxide emissions from subaerial volcanic regions
Volcanism and metamorphism are the principal geologic processes that drive carbon
transfer from the interior of Earth to the surface reservoir. 1–4 Input of carbon to the surface …
transfer from the interior of Earth to the surface reservoir. 1–4 Input of carbon to the surface …
Eruptive activity of the Santorini Volcano controlled by sea-level rise and fall
C Satow, A Gudmundsson, R Gertisser… - Nature …, 2021 - nature.com
Sea-level change is thought to influence the frequencies of volcanic eruptions on glacial to
interglacial timescales. However, the underlying physical processes and their importance …
interglacial timescales. However, the underlying physical processes and their importance …
Displaced cratonic mantle concentrates deep carbon during continental rifting
Continental rifts are important sources of mantle carbon dioxide (CO2) emission into Earth's
atmosphere,–. Because deep carbon is stored for long periods in the lithospheric mantle …
atmosphere,–. Because deep carbon is stored for long periods in the lithospheric mantle …
Structural controls on fluid pathways in an active rift system: A case study of the Aluto volcanic complex
In volcanically and seismically active rift systems, preexisting faults may control the rise and
eruption of magma, and direct the flow of hydrothermal fluids and gas in the subsurface …
eruption of magma, and direct the flow of hydrothermal fluids and gas in the subsurface …
New insights into the initiation and venting of the Bronze-Age eruption of Santorini (Greece), from component analysis
TH Druitt - Bulletin of Volcanology, 2014 - Springer
The late-seventeenth century BC Minoan eruption of Santorini discharged 30–60 km 3 of
magma, and caldera collapse deepened and widened the existing 22 ka caldera. A study of …
magma, and caldera collapse deepened and widened the existing 22 ka caldera. A study of …
Spatially Variable CO2 Degassing in the Main Ethiopian Rift: Implications for Magma Storage, Volatile Transport, and Rift‐Related Emissions
Deep carbon emissions from historically inactive volcanoes, hydrothermal, and tectonic
structures are among the greatest unknowns in the long‐term (∼ Myr) carbon cycle. Recent …
structures are among the greatest unknowns in the long‐term (∼ Myr) carbon cycle. Recent …
New mafic magma refilling a quiescent volcano: Evidence from He‐Ne‐Ar isotopes during the 2011–2012 unrest at Santorini, Greece
AL Rizzo, F Barberi, ML Carapezza… - Geochemistry …, 2015 - Wiley Online Library
Abstract In 2011–2012, Santorini was characterized by seismic‐geodetic‐geochemical
unrest, which was unprecedented since the most‐recent eruption occurred in 1950 and led …
unrest, which was unprecedented since the most‐recent eruption occurred in 1950 and led …