Late cenozoic uplift of Denali and its relation to relative plate motion and fault morphology

Paul G Fitzgerald, Edmund Stump, Thomas F. Redfield

Research output: Contribution to journalArticle

76 Citations (Scopus)

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 ∼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 ∼5 Ma, which created opposing tangential vectors of relative movement along the fault and forced the intervening crustal blocks upward.

Original languageEnglish (US)
Pages (from-to)497-499
Number of pages3
JournalScience
Volume259
Issue number5094
StatePublished - Jan 22 1993

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North America
Apatites

ASJC Scopus subject areas

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Late cenozoic uplift of Denali and its relation to relative plate motion and fault morphology. / Fitzgerald, Paul G; Stump, Edmund; Redfield, Thomas F.

In: Science, Vol. 259, No. 5094, 22.01.1993, p. 497-499.

Research output: Contribution to journalArticle

Fitzgerald, Paul G ; Stump, Edmund ; Redfield, Thomas F. / Late cenozoic uplift of Denali and its relation to relative plate motion and fault morphology. In: Science. 1993 ; Vol. 259, No. 5094. pp. 497-499.
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