2011 GSA Annual Meeting in Minneapolis (912 October 2011)
Paper No. 272-6
Presentation Time: 2:55 PM-3:10 PM


GREGG, Patricia M., College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, 104 Wilkinson Hall, Corvallis, OR 97331, DE SILVA, Shanaka, Geosciences, Oregon State University, Wilkinson Hall 104, Corvallis, OR 97331, desilvas@geo.oregonstate.edu, GROSFILS, Eric B., Geology Department, Pomona College, 185 E. 6th Street, Rm. 232, Claremont, CA 91711, and PARMIGIANI, John P., School of Mechanical, Industrial, and Manufacturing Engineering, Oregon State University, 204 Rogers Hall, Corvallis, OR 97331

Supereruptions (>VEI 7.5 >450 km3 of magma) are a common feature of the geologic record and are typically associated with ignimbrite flare-ups. Although they may be dwarfed by some silicic eruptions associated with LIPS (VEI 9), supereruptions represent one of the most catastrophic of terrestrial geologic phenomena. While the field characteristics and timing of these massive silicic outpourings is becoming increasingly well documented, the conditions that lead to the development, evolution and eventual eruption of such large volumes are less clear. Increased mantle power input (thermal and material flux) and its impact on the thermomechanical evolution of the crust and magma production is clearly important in producing and growing large, viable silicic magma bodies. Under these conditions, current models of overpressure-driven eruption triggers are untenable for most supereruptions and a new model for triggering these eruptions is required. We have developed a 2D finite-element model (Gregg et al., 2011) that for the first time takes into account the viscoelastic behavior of the country rock and helps identify the conditions that lead to the triggering of supereruptions. We show that roof collapse is the inevitable result of growth of magma bodies beyond a threshold size and this results in catastrophic eruption. This model is consistent with the physical volcanology of many supereruptions and the structural development of many of the large caldera complexes that source such eruptions.

Gregg, P.M., S.L. de Silva , E.B. Grosfils, and J.P. Parmigiani, Temperature-dependent mechanics of triggering catastrophic caldera-forming eruptions, in review, 2011.

2011 GSA Annual Meeting in Minneapolis (912 October 2011)
General Information for this Meeting
Session No. 272
Recent Advances in Studies of Large-Volume Silicic Volcanism: Stratigraphy, Architecture, Evolution
Minneapolis Convention Center: Room 101FG
1:30 PM-5:30 PM, Wednesday, 12 October 2011

Geological Society of America Abstracts with Programs, Vol. 43, No. 5, p. 651

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