David L.S. Blackwell
University of Oregon, Eugene, OR
Activity
2021
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CENOZOIC EVOLUTION OF THE CASCADIA FOREARC: CONSTRAINTS FROM PALEOMAGNETISM AND ANISOTROPY OF MAGNETIC SUSCEPTIBILITY OF SEDIMENTARY ROCKS EXPOSED NEAR CAPE ARAGO, CENTRAL OREGON COAST
T162 Initiation and Evolution of Arc-Forearc Systems in Cascadia and Beyond (Posters)Tuesday, 12 October 20219:00 AM - 1:00 PMExhibit Hall A
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INITIATION AND CENOZOIC EVOLUTION OF THE CASCADIA FOREARC BASIN: MULTIDISCIPLINARY EVIDENCE FROM THE COOS BAY AREA CENOZOIC STRATIGRAPHY, SOUTHWESTERN OREGON
T168 Initiation and Evolution of Arc-Forearc Systems in Cascadia and BeyondTuesday, 12 October 20211:30 PM - 5:30 PMPortland Ballroom 257 (Hybrid Room)
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TECTONOSTRATIGRAPHIC EVOLUTION OF SW OREGON FROM EARLY EOCENE COLLISION OF SILETZIA TO THE MODERN CASCADIA CONVERGENT MARGIN
T168 Initiation and Evolution of Arc-Forearc Systems in Cascadia and BeyondTuesday, 12 October 20211:30 PM - 5:30 PMPortland Ballroom 257 (Hybrid Room)
2019
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TECTONIC HISTORY OF THE COOS BAY BASIN AND ITS RELATIONSHIP TO PACIFIC NORTHWEST ‘SILETZIA’ TECTONICS
17 Recent Advances in Cordilleran Tectonic Evolution—2: CenozoicThursday, 16 May 20198:00 AM - 12:00 PMRoom C124