A MULTICHANNEL SEISMIC STUDY OF LITHOSPHERIC FLEXURE ACROSS THE HAWAIIAN-EMPEROR SEAMOUNT CHAIN

Existing models assume that the thickened crust beneath seamounts is the result of a surface volcanic load flexing an elastic plate. New results suggest that flexed oceanic crust beneath the Hawaiian-Emperor seamount chain is underlain by a 4-km thick deep crustal body. We intepret the body as a dee...

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Main Authors: Watts, A, Tenbrink, U, Buhl, P, Brocher, T
格式: Journal article
語言:English
出版: 1985
實物特徵
總結:Existing models assume that the thickened crust beneath seamounts is the result of a surface volcanic load flexing an elastic plate. New results suggest that flexed oceanic crust beneath the Hawaiian-Emperor seamount chain is underlain by a 4-km thick deep crustal body. We intepret the body as a deep crustal sill complex associated with the tholeiitic stage of volcano building along the chain. © 1985 Nature Publishing Group.