Abriaquí Fault

Abriaquí Fault
Falla de Abriaquí
Map showing the location of Abriaquí Fault
Map showing the location of Abriaquí Fault
EtymologyAbriaquí
Coordinates06°40′09″N 76°06′38″W / 6.66917°N 76.11056°W / 6.66917; -76.11056
Country Colombia
RegionAndean
StateAntioquia
Characteristics
RangeWestern Ranges, Andes
Part ofAndean oblique faults
Length33.8 km (21.0 mi)
Strike311 ± 2
DipNortheast
Dip angleHigh
Displacement0.2–1 mm (0.0079–0.0394 in)/yr
Tectonics
PlateNorth Andean
StatusInactive
TypeOblique thrust fault
MovementReverse sinistral
AgeQuaternary
OrogenyAndean

The Abriaquí Fault (Spanish: Falla de Abriaquí) is an oblique thrust fault in the department of Antioquia in northwestern Colombia. The fault has a total length of 33.8 kilometres (21.0 mi) and runs along an average northwest to southeast strike of 311 ± 2 in the Western Ranges of the Colombian Andes.

Etymology

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The fault is named after Abriaquí.[1]

Description

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The Abriaquí Fault parallels the Cañasgordas Fault to the south, cutting Cretaceous oceanic volcanic rocks as well as Tertiary and Cretaceous sedimentary rocks. The fault has a well defined fault trace with scarps, saddles, and deflected streams. The slip rate is estimated at 0.2 to 1 millimetre (0.0079 to 0.0394 in) per year deduced from displaced geomorphologic features.[1]

See also

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References

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  1. ^ a b Paris et al., 2000, p.18

Bibliography

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  • Paris, Gabriel; Machette, Michael N.; Dart, Richard L.; Haller, Kathleen M. (2000a), Map and Database of Quaternary Faults and Folds in Colombia and its Offshore Regions (PDF), USGS, pp. 1–66, retrieved 2017-09-18

Maps

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Further reading

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  • Page, W.D (1986), Seismic geology and seismicity of Northwestern Colombia, San Francisco, California, Woodward-Clyde Consultants Report for ISA and Integral Ltda., Medellín, pp. 1–200