CO2 outgassing during collisional orogeny is facilitated by the generation of immiscible fluids
Outgassing of CO2 during collisional orogeny can be explained by the generation of immiscible CO2-rich fluids and hydrosaline brines in metamorphosed sediments, according to thermodynamic modelling applied to the Himalaya.
Main Authors: | , , |
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Format: | Article |
Language: | English |
Published: |
Nature Portfolio
2022-01-01
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Series: | Communications Earth & Environment |
Online Access: | https://doi.org/10.1038/s43247-022-00340-w |