1998/05/01 by Stephen Self, L. Keszthelyi, T. Thórdarson · 372 citations
Earth and Planetary Sciences · #Basalt #Crust #Earth science #Flood basalt #Geochemistry #Geological and Geochemical Analysis #Geological formations and processes #Geology #Geology and Paleoclimatology Research #Lava #Paleontology #Petrology #Tectonics #Volcanism #Volcano
paper · doi:10.1146/annurev.earth.26.1.81
published in Annual Review of Earth and Planetary Sciences 26(1), 81-110 (Annual Reviews)
openalex publication_date 1998/05/01 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/16
▪ Abstract Pahoehoe lava flows are common in every basaltic province, and their submarine variants, pillow lavas and sheet flows, cover the bulk of the Earth. Pahoehoe flows are emplaced by inflation—the injection of molten lava underneath a solidified crust. Only in the past few years has an understanding of the inflation process and the ability to recognize ancient inflated lava flows been achieved. All large terrestrial basaltic flow fields studied to date, including flood basalts, were emplaced as thermally efficient, inflated, compound pahoehoe sheet flows. This leads us to propose that this is the standard way of emplacing large lavas (the SWELL hypothesis). The atmospheric impact of such flood basalt eruptions could have been protracted and severe, providing a plausible link between flood basalt eruptions and mass extinctions.