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Brothers Fault Zone
Hazard Annex Earthquake
Tectonic Alteration of a Major Neogene River Drainage of the Basin and Range
The Origin of the Columbia River Flood Basalt Province: Plume Versus Nonplume Models
B2158 Pt 15 Text Copy
PDF Linkchapter
The Case for NE-SW Extension in Northeast Oregon
Heat Flow and Energy Loss in the Western United States
Controls on Fault Geometry During Early Stages of Extension
Probabilistic Estimates of Maximum Seismic Horizontal Ground Motion on Rock in the Pacific Northwest and the Adjacent Outer Continental Shelf
Pierceof 00-498
Geological and Geophysical Perspectives on the Magmatic and Tectonic Development, High Lava Plains and Northwest Basin and Range
Open-File Report 99-31 I Paper Edition
Slip Rates and Kinematics of Active Crustal Faults in the Central Oregon Cascades
Map and Data for Quaternary Faults and Folds in Oregon
Stratocone Persistence, Mafic Lava Shields, and Pyroclastic Volcanism Associated with Intra-Arc Rift Propagation
Long-Term Fault Slip Rates, Distributed Deformation Rates, and Forecast of Seismicity in the Western United States from Joint Fi
Stratigraphic and Geochemical Evolution of the Glass Buttes Complex, Oregon
Geologic and Tectonic History of the Western Snake River Plain, Idaho and Oregon
Top View
Geology and Structure of the Brothers Fault Zone in the Central Part of the Millican SE Quadrangle, Deschutes County, Oregon by Elizabeth Ruth Tucker
Quaternary Faulting of Deschutes County, Oregon
Geological Survey Circular 838 HIGH LAVA PLAINS, BROTHERS FAULT ZONE to HARNEY BASIN, OREGON
Structural Analysis of the John Day and Mitchell Fault Zones, North-Centralgegon
Geologic Criteria for Siting Nuclear Power Plants in Oregon
TWO-STAGE OPENING of the NORTHWESTERN BASIN and RANGE in EASTERN OREGON: Evidence from the Miocene Crane Basin