Estructura cortical y procesos activos en el margen septentrional de La Españolaaplicación a la caracterización de fuentes tsunamigénicas

  1. Rodríguez Zurrunero, Álvaro
Zuzendaria:
  1. José Luis Granja Bruña Zuzendaria
  2. Alfonso Muñoz Martín Zuzendaria

Defentsa unibertsitatea: Universidad Complutense de Madrid

Fecha de defensa: 2021(e)ko urtarrila-(a)k 22

Epaimahaia:
  1. Gerardo de Vicente Muñoz Presidentea
  2. José Antonio Álvarez Gómez Idazkaria
  3. José Martín Dávila Kidea
  4. Alberto López Venegas Kidea
  5. Albert Casas Ponsatí Kidea
Saila:
  1. Geodinámica, Estratigrafía y Paleontología

Mota: Tesia

Teseo: 155405 DIALNET lock_openDocta Complutense editor

Laburpena

The North American (NOAM) plate converges with the Caribbean (CARIB) plate at a rate of 20.0 ± 0.4 mm/yr. towards 254 ± 1°. Plate convergence is highly oblique (20–10°), resulting in a complex crustal boundary with along-strike segmentation, strain partitioning and microplate tectonics. The northern margin of Hispaniola records the oblique collision/underthrusting of the Bahamas Carbonate Province with the island-arc. Due to the collision, northern Hispaniola has suffered several natural disasters caused by major earthquakes and tsunamis, such as the historic earthquake of 1842, thet sunami caused by earthquake-driven slumping in 1918 in the Mona Passage, the seismic crisis of 1943–1953 with five events of M > 7.0 or the seismic crisis of 2003 with amain shock of M6.3 and a large aftershock of M5.3...