Deformation of the Juan de Fuca Plate Beneath the Central Cascadia Continental Margin (44°-45°N) in Response to an Upper Plate Load

A 3D crustal model for the central Cascadia continental shelf and Coast Range between 44°N and 45°N shows that the crystalline crust of the forearc wedge beneath the coastline is characterized by a NW-trending, vertical slab of high-velocity rock interpreted to represent the dike complex that fed th...

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Egile Nagusiak:	Anne M. Tréhu, Kathy Davenport, Christopher B. Kenyon, Suzanne M. Carbotte, John L. Nabelek, Douglas R. Toomey, William S. D. Wilcock
Formatua:	Artigo
Hizkuntza:	Inglês
Argitaratua:	Geological Society of London 2023-12-01
Saila:	Earth Science, Systems and Society
Gaiak:	forearc structure Cascadia earthquake hazards subduction zone structure controlled source seismic imaging
Sarrera elektronikoa:	https://www.lyellcollection.org/doi/10.3389/esss.2023.10085
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