October 2016 LIP of the Month

Large Igneous Provinces: Global Listing in Spreadsheet Format (version: 30 October 2016)

Richard E. Ernst

Department of Earth Sciences, Carleton University, Ottawa, Canada; &

Faculty of Geology and Geography, Tomsk State University, Tomsk, Russia


Download: Global LIP Table 2.1 REV FINAL.XLSX

The attached spreadsheet (Excel format) is a global listing of Large Igneous Provinces (LIPs). The file has been extracted and partially updated (in red font) from Table 1.2 in Ernst (2014). It includes LIPs and interpreted LIP “fragments” (Ernst, 2007) and also Silicic LIPs (SLIPS). This has been produced in response to numerous requests for a spreadsheet version. Danni Mathieson is acknowledged for her help in converting Table 1.2 in Ernst (2014) to spreadsheet format.

This spreadsheet version complements the April 2015 LIP of the Month [http://www.largeigneousprovinces.org/15apr] “Large Igneous Provinces: Updated Compilation” which provided a PDF of Figure 1.6 (Global maps showing the distributions of LIPs and SLIPs) and Table 1.2 (Tabulation of LIPs and SLIPs record), both from Ernst (2014). 

Looking forward, you can expect periodic updates of this spreadsheet.  Also plans for an ArcGIS version are proceeding [January 2015 LIP of the Month, http://www.largeigneousprovinces.org/15jan].


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Ciborowski, T.J.R., Kerr, A.C., Ernst, R.E. (2015). The Early Proterozoic Matachewan Large Igneous Province: Geochemistry, Petrogenesis, and Implications for Earth Evolution. Journal of Petrology, 56 (8): 1459-1494.

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de Kock, M.O., Ernst, R.E., Söderlund, U., et al. (2014). Dykes of the 1.11 Ga Umkondo LIP, Southern Africa: clues to a complex plumbing system. Precambrian Research, 249: 129-143.

El Bahat, A., Ikenne, M., Söderlund, U., et al. (2013). U–Pb ages of dolerite dykes in the Bas Drâa Inlier of the Anti-Atlas of Morocco: newly identified 1380 Ma event in the West African Craton. Lithos, 174: 85–98.

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Ernst, R.E. (2007). Mafic–ultramafic Large Igneous Provinces (LIPs): importance of the pre-Mesozoic record. Episodes, 30: 107–113.

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Ernst, R.E. & Bell, K. (2010). Large Igneous Provinces (LIPs) and carbonatites. Mineralogy and Petrology, 98: 55–76.

Ernst, R.E. & Bleeker, W. (2010). Large igneous provinces (LIPs), giant dyke swarms, and mantle plumes: significance for breakup events within Canada and adjacent regions from 2.5 Ga to the Present. Canadian Journal of Earth Sciences, 47: 695–739.

Ernst, R.E. & Buchan, K.L. (2001). Large mafic magmatic events through time and links to mantle-plume heads. In Ernst, R.E. & Buchan, K.L. (eds.), Mantle Plumes: Their Identification through Time. Boulder, CO: Geological Society of America, Special Paper 352, pp. 483–575.

Ernst, R.E. & Buchan, K.L. (2004). Igneous rock associations in Canada 3: Large Igneous Provinces (LIPs) in Canada and adjacent regions: 3 Ga to Present. Geoscience Canada, 31 (3): 103–126.

Ernst, R.E. & Jowitt, S.M. (2013). Large Igneous Provinces (LIPs) and Metallogeny. Society of Economic Geologists Special Publication, 17: 17–51.

Ernst, R.E. & Srivastava, R.K. (2008). India’s place in the Proterozoic world: constraints from the large igneous provinces (LIP) record. In Srivastava, R.K., Sivaji, Ch., & Chalapathi Rao, N.V. (eds.), Indian Dykes: Geochemistry, Geophysics, and Geochronology. New Delhi, India: Narosa Publishing House Pvt. Ltd, pp. 41–56.

Ernst, R.E., Wingate, M.T.D., Buchan, K.L., & Li, Z.X. (2008). Global record of 1600–700 Ma Large Igneous Provinces (LIPs): implications for the reconstruction of the proposed Nuna (Columbia) and Rodinia supercontinents. Precambrian Research, 160: 159–178.

Ernst, R.E., Pereira, E., Hamilton, M.A., et al. (2013). Mesoproterozoic intraplate magmatic “barcode” record of the Angola portion of the Congo craton: newly dated magmatic events at 1500 and 1110 Ma and implications for Nuna supercontinent reconstructions. Precambrian Research, 230: 103–118.

Ernst, R.E, Hamilton, M.A., Söderlund, U., et al. (2016a). Long-lived connection between southern Siberia and northern Laurentia in the Proterozoic. Nature Geoscience, v. 9, p. 464-469.

Ernst, R.E., Okrugin, A.V., Veselovskiy, R.V., et al. (2016b). The 1501 Ma Kuonamka Large Igneous Province of northern Siberia: U-Pb geochronology, geochemistry, and links with coeval magmatism on other crustal blocks. Russian Geology and Geophysics, 57: 653-671.

Evans, D.A.D., Trindade, R.I.F., Catelani, E.L., et al. (2016). Return to Rodinia? Moderate to high paleolatitude of São Francisco/Congo craton at 920 Ma:  In:  Li, Z.X., D.A.D. Evans & J.B. Murphy (eds,): Supercontinent Cycles Through Earth History Geological Society of London Special Publication 424. doi:10.1144/SP424.1, p. 167-190.

French, J.E., Heaman, L.M., Chacko, T., & Srivastava, R.K. (2008). 1891–1883 Ma Southern Bastar–Cuddapah mafic igneous events, India: a newly recognized large igneous province. Precambrian Research, 160: 308–322.

French, J.E. & Heaman, L.M. (2010). Precise U–Pb dating of Paleoproterozoic mafic dyke swarms of the Dharwar craton, India: implications for the existence of the Neoarchean supercraton, Sclavia. Precambrian Research, 183: 416–441.

Gladkochub, D.P., Pisarevsky, S.A., Donskaya, T.V., et al. (2010). Proterozoic mafic magmatism in Siberian craton: an overview and implications for paleocontinental reconstruction. Precambrian Research, 183: 660–668.

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Gohl, K., Uenzelmann-Neben, G., & Grobys, N. (2011). Growth and dispersal of a Southeast African Large Igneous Province. South African Journal of Geology, 114: 379–386.

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Gumsley, A.P., Bleeker, W., Chamberlain, K., et al. (2015). U-Pb TIMS and in-situ SIMS dating of baddeleyite and zircon from sub-volcanic sills of the Ongeluk Formation (Transvaal Supergroup) in the Griqualand West sub-basin, Kaapvaal Craton, with implications for Snowball Earth and the Great Oxygenation Event.  In 2015 Joint Assembly (AGU, GAC, MAC, CGU) Abstract Proceedings.pdf, p. 378-379, Montreal May 2016

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Ivanov, A.V., He, H.-Y., Yan, L.-K., et al. (2013). Siberian Traps large igneous province: evidence for two flood basalt pulses around the Permo-Triassic boundary and in the Middle Triassic, and contemporaneous granitic magmatism. Earth Science Reviews, 122: 58–76.

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