Greater Antilles: Northern Caribbean Plate Kinematics

Fault Plane Solutions and Seismic Zones

Interpretation of Fault Plane Solutions

  • Fault plane solution A, located in eastern Jamaica, indicates compression by an east-dipping reverse fault.

  • Fault plane solution B, located in the southern Cayman Trough, indicates extension by an east-dipping normal fault.

  • Fault plane solution C, located on the NPRSFZ, indicates both compression and strike-slip movement on an oblique reverse fault with some right lateral slip dipping to the east.

  • Fault plane solutions D and E, located along the Puerto Rico Trench and the Oriente Fault Zone, respectively, indicate left-lateral strike-slip faulting with movement of the Caribbean Plate to the east.

Three Major Zones of Seismicity

  1. The first zone is composed of the south dipping slab beneath Puerto Rico and the Virgin Islands, which seems to be continuous with the slab of the Atlantic oceanic crust that is being subducted beneath the Lesser Antilles island arc (to the east),

  2. This zone is composed of a northwest-striking, almost vertical, zone of earthquakes below Mona Passage and eastern Hispaniola.  These earthquakes have virtually vertical T-axes and extend from 75-210 km deep, and

  3. This zone is made of a gently dipping plane which is part of the northward under-thrust of the Caribbean plate below Hispaniola and Puerto Rico along the Los Muertos trough.  The focal points of earthquakes near the upper portion of the Caribbean slab are indicative of shallow, north-dipping thrust faulting (Dolan et al., 1998).

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