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Eclogitization is the tectonic process in which eclogite, a high-pressure metamorphic facies, is formed. This leads to an increase in the density of regions of Earth's crust, which leads to changes in plate motion at convergent boundaries (where rock sinks beneath other rock).
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subduction continental crust eclogites slab eclogite rocks metamorphic density mantle exhumation granulites models increase tectonic oceanic undertow zones also study
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Eclogitization | is a | tectonic process in which eclogite | 0.90 | text |
| Eclogitization | is a | mechanism for continuing subduction after slab detachment in a subduction zone | 0.90 | text |
| the Alps | instance of | Certain areas | 0.80 | text |
| Zagros | instance of | Certain areas | 0.80 | text |
| and Himalayas | instance of | Certain areas | 0.80 | text |
| intracontinental deformation | instance of | A plethora of geologic settings have been modeled | 0.80 | text |
| subduction | instance of | A plethora of geologic settings have been modeled | 0.80 | text |
| and continental collision to determine the density | instance of | A plethora of geologic settings have been modeled | 0.80 | text |
| buoyancy impact of eclogitization | instance of | A plethora of geologic settings have been modeled | 0.80 | text |
| Eclogitization | related to Field studies and simulations | The Western Gneiss Region | 0.60 | section |
| Eclogitization | related to Field studies and simulations | Bergen Arc | 0.60 | section |
| Eclogitization | related to Field studies and simulations | Western Norway | 0.60 | section |
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