Drake Peak — A structurally complex rhyolite center in southeastern Oregon

Professional Paper 1124-E
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Abstract

The Drake Peak volcanic center of middle Miocene age, located about 25 km northeast of Lakeview, Oreg., is a structurally complex eruptive center that resulted from several episodes of intrusion and extrusion of rhyolite. Two thousand meters of andesite and basalt flows, lahars, and volcaniclastic rocks of late Eocene age, and of basaltic andesite, tuff, and flood basalts of Eocene to middle Miocene age were structurally domed by the piston-like intrusion of a large body of rhyolite. The eruption of rhyolite flows at 14.3±2 million years followed the structural doming, and upper Miocene tuffs and basalt flows lapped against the dome and the rhyolite. A felsitic rhyolite ring intrusion 3 km in diameter, emplaced during the doming, is now exposed in the deeply eroded core of the dome. The rhyolites range in Si02 content from 69 to 76 percent and are peraluminous. The nonporphyritic ring intrusion is more silicic than the flows erupted later, which contain up to 23 percent phenocrysts of plagioclase, hypersthene, biotite, clinopyroxene, and quartz. The progressive depletion of Mg, Ca, Sr, Fe, Ti, and Al and the enrichment in silicon and rubidium are compatible with the generation of the observed rhyolite types by tapping a compositionally zoned magma chamber.

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Publication type Report
Publication Subtype USGS Numbered Series
Title Drake Peak — A structurally complex rhyolite center in southeastern Oregon
Series title Professional Paper
Series number 1124
Chapter E
DOI 10.3133/pp1124E
Year Published 1980
Language English
Publisher U.S. Geological Survey
Contributing office(s) Geology, Minerals, Energy, and Geophysics Science Center
Description iii, 16 p.
Larger Work Type Report
Larger Work Subtype USGS Numbered Series
Larger Work Title Shorter contributions to mineralogy and petrology, 1979
Country United States
State Oregon
Other Geospatial Drake Peak
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