Complex Crustal Deformation Controlled by the 3D Geometry of the Chile Subduction Zone (vol 113, pg 2479, 2023)

Cembrano, Jose

Abstract

The authors of Herrera et al. (2023) note the following errors in their original article: Location of Error Original Text Revised Text Third key point The upper plate deformation is consistent with radially from fault-oriented normal and strike-slip faults Crustal faults representing upper plate deformation form an arcuate pattern around persistent rupture zones Abstract N20°W–50° W/N60°SW N20°W–50° W/60° SW Abstract N30°E–80° E/N60°NW N30°E–80° E/60° NW Page 6 of Herrera et al. (2023), first column N30°W–N80°W/N60°SW N30°W–N80°W/60° SW Page 8 of Herrera et al. (2023), second column N54°W/N55°SW N54°W/55° SW Page 8 of Herrera et al. (2023), second column N65°W/N74°SW N65°W/74° S. © Seismological Society of America.

Más información

Título según WOS: Complex Crustal Deformation Controlled by the 3D Geometry of the Chile Subduction Zone (vol 113, pg 2479, 2023)
Título según SCOPUS: Erratum to Complex Crustal Deformation Controlled by the 3D Geometry of the Chile Subduction Zone (Bull. Seismol. Soc. Am. 113, no. 6, 2479–2491, doi: 10.1785/0120230062)
Título de la Revista: Bulletin of the Seismological Society of America
Volumen: 114
Número: 1
Editorial: Seismological Society of America
Fecha de publicación: 2024
Página de inicio: 612
Idioma: English
DOI:

10.1785/0120230286

Notas: ISI, SCOPUS