Carbon occurs in mantle samples in several chemical, mineralogical and morphological forms. It has been observed as CO2, CH4 and CO in fluid inclusions, as carbonate, graphite …
MS Ghiorso, GAR Gualda - Contributions to Mineralogy and Petrology, 2015 - Springer
A thermodynamic model for estimating the saturation conditions of H 2 O–CO 2 mixed fluids in multicomponent silicate liquids is described. The model extends the capabilities of rhyolite …
Subduction transports volatiles between Earth's mantle, crust, and atmosphere, ultimately creating a habitable Earth. We use isotopes to track carbon from subduction to outgassing …
We detail here the general concepts behind using noble gases as a tracer of crustal fluid processes and illustrate these concepts with examples applied to oil-gas-groundwater …
The flux of carbon into and out of Earth's surface environment has implications for Earth's climate and habitability. We compiled a global data set for carbon and helium isotopes from …
T Stachel, P Cartigny, T Chacko… - … in Mineralogy and …, 2022 - pubs.geoscienceworld.org
This chapter is devoted to the carbon and nitrogen stable isotope compositions of terrestrial diamonds with a strong focus on monocrystalline diamonds formed in Earth's mantle. The …
Ion microprobe measurements of the concentrations of H2O, CO2, F, S and Cl and the isotopic composition of hydrogen are reported for populations of olivine-hosted melt …
T Hammouda, S Keshav - Chemical Geology, 2015 - Elsevier
Carbon emission at volcanic centers requires a constant balance between output (mostly by volcanism, either at plate boundaries or intraplate) and input (mostly at trench settings) of …
Processes controlling the composition of seafloor hydrothermal fluids in silicic back-arc or near-arc crustal settings remain poorly constrained despite growing evidence for extensive …