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Active Triclinic Transtension in a Volcanic Arc: A Case of the El Salvador Fault Zone in Central America

The El Salvador Fault Zone (ESFZ) is part of the Central American Volcanic Arc and accommodates the oblique separation movement between the forearc sliver and the Chortis block (Caribbean Plate). In this work, a triclinic transtension model was applied to geological (fault-slip inversion, shape of v...

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Principais autores: Jorge Alonso-Henar, Carlos Fernández, José Antonio Álvarez-Gómez, Carolina Canora, Alejandra Staller, Manuel Díaz, Walter Hernández, Ángela Valeria García, José Jesús Martínez-Díaz
Format: Artigo
Sprog:Inglês
Udgivet: MDPI AG 2022-06-01
Serier:Geosciences
Fag:
El Salvador Fault Zone
active volcanic arc
triclinic transtension
Central America
Online adgang:https://www.mdpi.com/2076-3263/12/7/266
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