Statements (49)
| Predicate | Object |
|---|---|
| gptkbp:instanceOf |
geological formation
|
| gptkbp:abbreviation |
LIPs
|
| gptkbp:ageRange |
Precambrian to present
|
| gptkbp:associatedWith |
climate change
mass extinctions |
| gptkbp:canBe |
continental
hybrid oceanic |
| gptkbp:canRelease |
gptkb:halogens
volcanic gases CO2 SO2 |
| gptkbp:cause |
acid rain
ozone depletion oceanic anoxic events global environmental effects |
| gptkbp:characterizedBy |
large volume of magma
rapid emplacement |
| gptkbp:composedOf |
igneous rocks
|
| gptkbp:emplacementRate |
rapid (within a few million years)
|
| gptkbp:example |
gptkb:Siberian_Traps
gptkb:Columbia_River_Basalt_Group gptkb:Ontong_Java_Plateau gptkb:Deccan_Traps gptkb:Paraná-Etendeka_Province |
| gptkbp:firstDescribed |
geologists in the 20th century
|
| gptkbp:foundIn |
oceanic crust
continents |
| https://www.w3.org/2000/01/rdf-schema#label |
Large Igneous Provinces
|
| gptkbp:importantFor |
mineral resources
paleoclimate studies tectonic evolution |
| gptkbp:relatedTo |
trap rock
continental breakup continental flood basalts oceanic plateaus rift zones hotspots supercontinent cycles flood basalt provinces mantle plumes |
| gptkbp:studiedBy |
paleomagnetism
radiometric dating geochemical analysis |
| gptkbp:studiedIn |
geology
volcanology |
| gptkbp:volume |
>100,000 km³
|
| gptkbp:bfsParent |
gptkb:Deccan_Traps_volcanism
|
| gptkbp:bfsLayer |
6
|