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The Deccan Traps are a large igneous province of west-central India (17–24°N, 73–74°E). They are one of the largest volcanic features on Earth, with lava erupted from multiple volcanic centres. The Traps consist of many layers of solidified flood basalt that together are more than about 2 kilometres (1.2 mi) thick, cover an area of about 500,000 square…
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deccan traps impact may india million plume years time eruptions cretaceous event indian volume paleogene eruption extinction major province réunion
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| widespread faulting | instance of | Features | 0.80 | text |
| frequent diking events | instance of | Features | 0.80 | text |
| high heat flux | instance of | Features | 0.80 | text |
| and positive gravity anomalies suggest that the extrusive phase of the Deccan Traps is associated with the existence of a triple junction which may have existed during the Late Cretaceous | instance of | Features | 0.80 | text |
| having been caused by a deep mantle plume | instance of | Features | 0.80 | text |
| Deccan Traps | related to Chicxulub crater | Although | 0.60 | section |
| Deccan Traps | related to Chicxulub crater | The | 0.60 | section |
| Deccan Traps | related to Chicxulub crater | Cretaceous | 0.60 | section |
| Deccan Traps | related to Chicxulub crater | Paleogene | 0.60 | section |
| Deccan Traps | related to Chicxulub crater | Pg | 0.60 | section |
| Deccan Traps | related to Chicxulub crater | However | 0.60 | section |
| Deccan Traps | related to Effect on mass extinctions and climate | The | 0.60 | section |
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