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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| Formáid: | Artigo |
| Teanga: | Inglês |
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MDPI AG
2022-06-01
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| Sraith: | Geosciences |
| Ábhair: | |
| Rochtain ar líne: | https://www.mdpi.com/2076-3263/12/7/266 |
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Níl clibeanna ann, Bí ar an gcéad duine le clib a chur leis an taifead seo!
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