Stratigraphy and volcanic evolution of the middle Miocene to Pliocene La Grande–Owyhee eruptive axis in eastern Oregon
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Published:August 01, 2013
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CiteCitation
Mark L. Ferns, Jason D. McClaughry, 2013. "Stratigraphy and volcanic evolution of the middle Miocene to Pliocene La Grande–Owyhee eruptive axis in eastern Oregon", The Columbia River Flood Basalt Province, Stephen P. Reidel, Victor E. Camp, Martin E. Ross, John A. Wolff, Barton S. Martin, Terry L. Tolan, Ray E. Wells
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The La Grande–Owyhee eruptive axis in eastern Oregon is an ~300-km-long, north-northwest–trending, middle Miocene to Pliocene volcanic belt located along the eastern margin of the Columbia River flood basalt province. The eruptive axis extends from Elgin on the north to Jordan Valley on the south and is juxtaposed between the Chief Joseph dike swarm on the east and the Monument dike swarm and the middle Miocene Strawberry volcanics on the west. Numerous volcanic vents, from which a diverse assemblage of tholeiitic, silicic, calc-alkaline, and alkalic lavas erupted, are contained within or directly adjacent to the La Grande, Baker, and Oregon-Idaho...
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Contents
The Columbia River Flood Basalt Province

GeoRef
- andesites
- basalts
- calc-alkalic composition
- calderas
- Cenozoic
- Columbia River Basalt Group
- dacites
- eruptions
- fissures
- flood basalts
- grabens
- igneous rocks
- major elements
- middle Miocene
- Miocene
- Neogene
- olivine basalt
- Oregon
- Pliocene
- rhyolites
- spectra
- Tertiary
- tholeiite
- trace elements
- United States
- vents
- volcanic belts
- volcanic features
- volcanic rocks
- X-ray fluorescence spectra
- eastern Oregon
- Oregon-Idaho Graben
- Baker Graben
- La Grande-Owyhee eruptive axis
- La Grande Graben