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- W2034289971 abstract "Apatite fission-track analysis of samples that cover a 4-kilometer vertical section from the western flank of Denali (Mount McKinley), North America's highest mountain, suggests that the mountain massif was formed by rapid uplift (> 1 kilometer per million years) beginning approximately 6 million years ago (Ma). Uplift was a result of the morphology of the Denali fault and a change in motion of the Pacific plate with respect to North America at approximately 5 Ma, which created opposing tangential vectors of relative movement along the fault and forced the intervening crustal blocks upward." @default.
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- W2034289971 date "1993-01-22" @default.
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- W2034289971 title "Late Cenozoic Uplift of Denali and Its Relation to Relative Plate Motion and Fault Morphology" @default.
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- W2034289971 doi "https://doi.org/10.1126/science.259.5094.497" @default.
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