Bifurcation of the Yellowstone plume driven by subduction-induced mantle flow by Christopher Kincaid and others (2013, 10.1038/ngeo1774)

Authors: Christopher Kincaid, K. A. Druken, Ross W. Griffiths, Dave R. Stegman.

Nature Geoscience 6, 395–399. Laboratory slab rollback experiments generate opposite thermal progressions. The High Lava Plains branch is a passively advected thermal anomaly, distinct from the deformed conduit beneath the Snake River Plain. Author-uploaded full text: www.researchgate.net/publication/236694225_Bifurcation_of_the_Yellowstone_plume_driven_by_subduction-induced_mantle_flow