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Epidosite (/ɪˈpɪdəsaɪt/) is a highly altered epidote and quartz bearing rock. It is the result of slow hydrothermal alteration or metasomatism of the basaltic sheeted dike complex and associated plagiogranites that occurs below the massive sulfide ore deposits which occur in ophiolites. Most epidosites represent the zone of intense metal leaching below…
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result sheeted sulfide deposits epidote quartz metasomatism basaltic plagiogranites ophiolites ɪˈpɪdəsaɪt highly altered bearing rock slow hydrothermal alteration dike complex
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Epidosite | related to External links | Encyclopædia Britannica | 0.60 | section |
| Epidosite | related to External links | Vol | 0.60 | section |
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