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How Large Igneous Provinces affect global climate, sometimes cause mass extincti...
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Gravity and magnetic modelling of layered mafic–ultramafic intrusions in large i...
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Precise U-Pb ages and geochemistry of Palaeoproterozoic mafic dykes from souther...
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When do mantle plumes destroy diamonds?
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Archean mafic dyke swarms near the Cameron River and Beaulieu River volcanic bel...
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Gravity and magnetic modelling of layered mafic–ultramafic intrusions in large i...
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Precise U–Pb ages and geochemistry of Palaeoproterozoic mafic dykes from souther...
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Radiating rifts and dyke swarms of the middle Paleozoic Yakutsk plume of eastern...
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Giant radiating dyke swarms on Earth and Venus
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The high arctic LIP in Canada: Trace element and sm–nd isotopic evidence for the...
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When do mantle plumes destroy diamonds?
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U-Pb Geochronology and Geochemistry of the Povungnituk Group of the Cape Smith B...
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Precambrian mafic dyke swarms in the Singhbhum craton (eastern India) and their...
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A New Ectasian Event of Basitic Magmatism in the Southern Siberian Craton
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Geochemical characterization of a reconstructed 1110 Ma Large Igneous Province
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Petrography, mineralogy and SIMS U-Pb geochronology of 1.9–1.8 Ga carbonatites a...
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Related Subjects
Geology
Large Igneous Province
diamond window
kimberlite
large igneous province
lithosphere
mantle plume
1110 Ma dykes swarms
Anoxia
Apatite
Baddeleyite
Cape Smith belt
Dharwar Craton
Earth-Surface Processes
Eastern Dharwar craton
Extinction
Flood basalt
Geochemistry
Geochemistry and Petrology
Geochemistry-reconstruction
Geochronology
Global warming
Ice age
Isachsen Formation
Large Igneous Provinces
Large Igneous Provinces (LIPs)
Large igenous province
Mafic dyke swarms
Mafic dykes
Magnesiocarbonatite
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