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Sismicidad Y Tectónica De La Región De Murcia

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Sismicidad Y Tectónica De La Región De Murcia Sismicidad y Tectónica de la Región de Murcia Actividad tectónica reciente de fallas Fallas neotectónicas y activas grandes fallas son estructuras tectónicas lineales que conforman una zona de deformación (zona de falla) de ancho variable, normalmente entre 1 y 5 km, que se reconoce en superficie por longitudes de al menos 30 km, si bien éstas superan con frecuencia los 50 km, llegando excepcionalmente a 100 km en algunos casos. Casi todas las grandes fallas se pueden compartimentar en segmentos tectónicos diferenciados, que pueden presentar longitudes desde los 10-15 km hasta unos 40 km en las fallas más continuas. Las grandes fallas de la Región de Murcia pueden clasificarse de modo sencillo en cinco grupos según su actividad tectónica reciente reconocida: “Muy Baja”, “Baja”, “Media”, “Alta” y “Muy Alta”. Las clases “Muy Baja” y “Baja” califican fallas en las que no se han reconocido deformaciones en depósitos del Cuaternario o posteriores al Pleistoceno Inferior, respectivamente, y, en los que los procesos geomorfológicos asociados indican una actividad muy baja o baja. Las fallas de clase “Media” presentan procesos geomorfológicos asociados a indicadores de cierta actividad y la edad de la última deformación reconocida es al menos Pleistoceno Medio. La clase “Alta” se corresponde con fallas que deforman depósitos de edad al menos Pleistoceno Superior y presentan tasas de deslizamiento entre 0,05-0,10 m/ka (1000 años). La clase “Muy alta” la forman fallas con tasas de deslizamiento superiores a 0,10 m/ka y con deformaciones reconocidas en materiales del Pleistoceno Superior y en algunos casos del Holoceno. Las fallas con mayor grado de actividad reciente en la Región de Murcia son las fallas de Alhama de Murcia y Carrascoy. Aunque estrictamente fuera del territorio murciano también hay que destacar la Falla del Bajo Segura y las fallas de San Miguel de Salinas y Torrevieja (Alicante). Figura. Grandes Fallas del sureste de España (Cordilleras Béticas Orientales). Se indican los diferentes segmentos tectónicos que componen cada gran falla, así como su grado de actividad tectónica reciente. 1: Pozohondo-Tobarra, 2: Socovos-Calasparra (a: Central, b: Línea Eléctrica), 3: Tíscar, 4: Crevillente (Sector Murcia) (a: Campo Coy-Bullas, b: Bullas-Sª Ricote), 5: Crevillente (Sector Alicante) (Abanilla-Río Vinalopó), 6: Alhama de Murcia (a: Puerto Lumbreras-Lorca, b: Lorca-Totana, c: Totana- Alhama, d: Alhama-Alcantarilla), 7: Jumilla (Sectores Murcia y Valencia) (a: Calasparra-Jumilla, b:Jumilla-Yecla, c: Yecla-Caudete, d: Caudete-Xátiva, e: Xátiva-Tavernes), 8: Carrascoy, 9: Bajo Segura (a: Hurchillos, b: Benjúzar, c: Guardamar), 10: Torrevieja, 11: San Miguel de Salinas, 12: Palomares (a: Almenara- Hinojar, b: Carboneras-Almenara), 13: Corredor de Las Alpujarras, 14: Alhamilla, 15: Carboneras (a: Rambla Morales, b: Serrata, c: El Argamasón, d: Carboneras), 16: Las Moreras-Escarpe de Mazarrón (a: Las Moreras, b: Puerto de Mazarrón-Este de Cabo Tiñoso, c: Este de Cabo Tiñoso-Este de Cabo de Palos). .
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