= Bifurcation of the Yellowstone plume driven by subduction-induced mantle flow by Christopher Kincaid and others
{tag=Work by Christopher Kincaid}
{tag=Work by K. A. Druken}
{tag=Work by Ross W. Griffiths}
{tag=Work by Dave R. Stegman}
{title2=2013}
{title2=10.1038/ngeo1774}
https://www.nature.com/articles/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: https://www.researchgate.net/publication/236694225_Bifurcation_of_the_Yellowstone_plume_driven_by_subduction-induced_mantle_flow
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