K. A. Druken coauthored physical models of interacting subduction and mantle plumes. The experiments examine whether changing three-dimensional flow can account for contrasting volcanic progressions near Yellowstone, connecting surface patterns with a testable transport mechanism.[ref]
Bifurcation of the Yellowstone plume driven by subduction-induced mantle flow by Christopher Kincaid and others. Abstract: laboratory model and opposing volcanic progressions
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