|Title||Bifurcation of the Yellowstone plume driven by subduction-induced mantle flow|
|Publication Type||Journal Article|
|Year of Publication||2013|
|Authors||Kincaid C, Druken KA, Griffiths RW, Stegman DR|
|Type of Article||Article|
|Keywords||basin; genesis; hotspot; laboratory models; magmatism; oregon; origin; plateau; province; slab|
The causes of volcanism in the northwestern United States over the past 20 million years are strongly contested(1). Three drivers have been proposed: melting associated with plate subduction(2,3); tectonic extension and magmatism resulting from rollback of a subducting slab(4-6); or the Yellowstone mantle plume(7-9). Observations of the opposing age progression of two neighbouring volcanic chains-the Snake River Plain and High Lava Plains-are often used to argue against a plume origin for the volcanism. Plumes are likely to occur near subduction zones(10), yet the influence of subduction on the surface expression of mantle plumes is poorly understood. Here we use experiments with a laboratory model to show that the patterns of volcanism in the northwestern United States can be explained by a plume upwelling through mantle that circulates in the wedge beneath a subduction zone. We find that the buoyant plume may be stalled, deformed and partially torn apart by mantle flow induced by the subducting plate. Using plausible model parameters, bifurcation of the plume can reproduce the primary volcanic features observed in the northwestern United States, in particular the opposite progression of two volcanic chains. Our results support the presence of the Yellowstone plume in the northwestern United States, and also highlight the power of plume-subduction interactions to modify surface geology at convergent plate margins.
|Short Title||Nat. Geosci.|