One possible source of these structures is dense thermochemical piles overlying ultra-low velocity zones.Campbell and Griffith showed that komatiite was probably formed due to these structures. The largepositive Clapeyron slope of the post-perovskite transition has a significant impact on their formation. HansRamberg pioneered the use of large-scale models to study these structures. W. J. Morgan was the firstperson to propose the existence of these structures. They consist of a hot tail and a co
One possible source of these structures is dense thermochemical piles overlying ultra-low velocity zones.Campbell and Griffith showed that komatiite was probably formed due to these structures. The largepositive Clapeyron slope of the post-perovskite transition has a significant impact on their formation. HansRamberg pioneered the use of large-scale models to study these structures. W. J. Morgan was the firstperson to propose the existence of these structures. They consist of a hot tail and a cooler head. Thesestructures explain giant oceanic plateaus, large igneous provinces, continental flood basalts, and hotspotvolcanism. For 10 points, identify these columnar upwellings in the mantle.
One possible source of these structures is dense thermochemical piles overlying ultra-low velocity zones.
mantle plume