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Actividad tectónica del Holoceno tardío a lo largo de los márgenes de la subplaca Sinaí
Science (New York, N.Y.)
|October 27, 1978
Resumen
La actividad tectónica del Holoceno superior, incluido el plegamiento y la elevación, se produjo a lo largo del margen occidental de la subplaca del Sinaí (Laguna de Bardawil) y el margen oriental (Golfo de Elat). Estos movimientos se analizan dentro del marco tectónico regional.
Área de la Ciencia:
- Geología Geología Geología.
- La tectónica es la tectónica.
- Ciencia Cuaternaria La ciencia cuaternaria es la ciencia cuaternaria.
Sus antecedentes:
- La subplaca del Sinaí es tectónicamente activa.
- Los eventos geológicos del Holoceno superior son cruciales para comprender la deformación regional.
Objetivo del estudio:
- Para investigar los movimientos tectónicos del Holoceno Superior a lo largo de la subplaca del Sinaí.
- Analizar las actividades de plegado y elevación en los márgenes occidental y oriental.
- Para contextualizar estas actividades dentro del marco tectónico regional más amplio.
Principales métodos:
- Observaciones geológicas de campo.
- Análisis de la geomorfología costera.
- Interpretación del marco tectónico.
Principales resultados:
- Se identificaron movimientos de plegado y elevación significativos a lo largo del margen occidental de la subplaca del Sinaí, específicamente alrededor de la laguna de Bardawil.
- El levantamiento también se documentó en las costas del margen oriental, en el área del Golfo de Elat.
- Estos eventos tectónicos ocurrieron durante el período del Holoceno Superior.
Conclusiones:
- Los márgenes occidental y oriental de la subplaca del Sinaí experimentaron una actividad tectónica sustancial durante el Holoceno Superior.
- El plegamiento y elevación observados son consistentes con los procesos tectónicos regionales que afectan a la subplaca del Sinaí.
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