Código QR

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...

Descrición completa

Gardado en:
Principais autores: Anne M. Tréhu, Kathy Davenport, Christopher B. Kenyon, Suzanne M. Carbotte, John L. Nabelek, Douglas R. Toomey, William S. D. Wilcock
Formato: Artigo
Idioma:Inglês
Publicado: Geological Society of London 2023-12-01
Series:Earth Science, Systems and Society
Assuntos:
forearc structure
Cascadia
earthquake hazards
subduction zone structure
controlled source seismic imaging
Acceso en liña:https://www.lyellcollection.org/doi/10.3389/esss.2023.10085
Tags: Engadir etiqueta
Sen Etiquetas, Sexa o primeiro en etiquetar este rexistro!

Títulos similares