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Blanco Fracture Zone
Wmawa ES
This Report Is Preliminary and Has Not Bee Reviewed for Conformity with US
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Recent Tectonics of the Blanco Ridge, Eastern Blanco Transform Fault Zone
Topographic Form of the Coast Ranges of the Cascadia Margin in Relation to Coastal Uplift Rates and Plate Subduction
Rethinking Turbidite Paleoseismology Along the Cascadia Subduction Zone
Mineralogy and Chemistry
Structure and Tectonics of Cascadia Segment. Central Blanco Transform Fault Zone Abstract Approved
Duncanjohnrussell1968
The Official Magazine of The
SEATTLE, UNIVERSITY of WASHINGTON DEPARTMENT of OCEANOGRAPHY Seattle, Washington 98105
Quaternary Fault and Fold Database of the United States
Subduction of Fracture Zones Controls Mantle Melting and Geochemical Signature Above Slabs
Petrological Constraints on Magma Plumbing Systems Along Mid-Ocean Ridges
Axial Seamount' an Active Ridge Axis Volcano on the Central Juan De Fuca Ridge
Shallow Crustal Structure of the Caldera of Axial Seamount, Juan De Fuca Ridge
Implicationscenozoic, Atwater (1970)
DOGAMI Open-File Report O-92-04, Neotectonic Map of the Oregon Continental Margin and Adjacent Abyssal Plain
Top View
TOPOGRAPHY and TECTONICS OP the INTERSECTIONS of FRACTURE ZONE with CENTRAL RIFTS by Norman Harvey Sleep B.S., Michigan State Un
Segmentation of the Blanco Transform Fault Zone from Earthquake Analysis
The STRUCTURE and TECTONICS of the BLANCO FRACTURE ZONE
Marine Transform Faults and Fracture Zones: a Joint Perspective Integrating Seismicity, Fluid Flow and Life
Internal Structure of Uppermost Oceanic Crust Along the Western Blanco Transform Scarp: Implications for Subaxial Accretion
Article Size Measurements, Down-Core X- Bathymetry
Hydrothermal Temperature Changes at the Southern Juan De Fuca Ridge