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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Autors principals:	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
Idioma:	Inglês
Publicat:	MDPI AG 2022-06-01
Col·lecció:	Geosciences
Matèries:	El Salvador Fault Zone active volcanic arc triclinic transtension Central America
Accés en línia:	https://www.mdpi.com/2076-3263/12/7/266
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