Vianí Fault

Coordinates: 04°52′37.4″N 74°33′23.6″W / 4.877056°N 74.556556°W / 4.877056; -74.556556
Source: Wikipedia, the free encyclopedia.
Vianí Fault
Falla de Vianí
Age
Quaternary
OrogenyAndean

The Vianí Fault (

strike of 055.5 ± 15 in the Eastern Ranges of the Colombian Andes
.

Etymology

The fault is named after Vianí, Cundinamarca.[1]

Description

The Vianí Fault is located on the western slope of the

Upper Cretaceous rocks of the Güagüaquí Group to the southeast.[1][2] In the southern area of the fault, the north–south oriented Vianí Fault thrusts the Seca Formation on top of the Hoyón Formation. Farther to the north at Vianí, the fault strike changes to northeast–southwest and the fault displaces the Bituima Fault.[2] The fault trace is characterised by offset spurs, degraded fault scarps, saddles, small pull-apart basins, aligned drainage, and deflected streams.[1] The fault borders the Guaduas Synclinal to the east and south.[3] It forms the northwestern boundary of the Bogotá savanna
.

A maximum moment magnitude earthquake is estimated to be 7.2 on the basis of probable rupture of entire fault length. The slip rate is estimated at 0.1 to 1 millimetre (0.0039 to 0.0394 in) per year based on offset morphologic and neotectonic features.[1]

See also

References

  1. ^ a b c d Paris et al., 2000a, p.48
  2. ^ a b c Plancha 227, 1998
  3. ^ Acosta & Ulloa, 2001, p.71

Bibliography

  • Acosta Garay, Jorge, and Carlos E Ulloa Melo. 2001. Geología de la Plancha 227 - La Mesa - 1:100,000, 1–80.
    INGEOMINAS
    .
  • Paris, Gabriel; Michael N. Machette; Richard L. Dart, and Kathleen M. Haller. 2000a. Map and Database of Quaternary Faults and Folds in Colombia and its Offshore Regions, 1–66. USGS. Accessed 2017-09-18.

Maps