Quantifying the buffering of oceanic oxygen isotopes at ancient midocean ridges
<p>To quantify the intensity of oceanic oxygen isotope buffering through hydrothermal alteration of the oceanic crust, a 2D hydrothermal circulation model was coupled with a 2D reactive transport model of oxygen isotopes. The coupled model calculates steady-state distributions of temperature,...
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2020-08-01
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| Series: | Solid Earth |
| Online Access: | https://se.copernicus.org/articles/11/1475/2020/se-11-1475-2020.pdf |