Oca-Ancón Fault System

The Oca-Ancón Fault System (Spanish: Falla Oca-Ancón) is a complex of geological faults located in the northeastern Colombia and northwestern Venezuela near the Caribbean Sea. The fault system is of right-lateral strike-slip type and runs an approximate length of 650 km (400 mi).[1][2] The Oca-Ancón Fault System is part of the diffuse boundary between the Caribbean Plate and the South American Plate.[3] The movement rate of the Oca-Ancón Fault System is estimated at 2 millimeters each year, more than most Venezuelan faults.[1]

References

  1. 1 2 Audemard M., Franck A.; Singer P., André; Soulas, Jean-Pierre (2006). "Quaternary faults and stress regime of Venezuela" (PDF). Revista de la Asociación Geológica Argentina. Asociación Geológica Argentina. 61 (4): 480–491. Retrieved 24 November 2015.
  2. ↑ Audemard M., Franck A. (1996). "Paleoseismicity studies on the Oca-Ancón fault system, northwestern Venezuela". Tectonophysics. 259: 67–80.
  3. ↑ Audemard M., Franck A.; Singer P., André (1996). "Active fault recognition in northwestern Venezuela and its seismogenic characterization: Neotectonic and paleoseismic approach". Geofísica Internacional. 35 (3): 245–255.


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