Understanding controls on hydrothermal dolomitisation: insights from 3D reactive transport modelling of geothermal convection
<p>The dominant paradigm for petrogenesis of high-temperature fault-controlled dolomite, widely known as “hydrothermal dolomite” (HTD), invokes upwelling of hot fluid along faulted and fractured conduits from a deep over-pressured aquifer. However, this model has several inherent ambiguities w...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2020-12-01
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| Series: | Solid Earth |
| Online Access: | https://se.copernicus.org/articles/11/2439/2020/se-11-2439-2020.pdf |