Otú Norte Fault
Falla de Otú Norte
Otú-Pericos Fault
Map showing the location of Otú Norte Fault
Map showing the location of Otú Norte Fault
Map showing the location of Otú Norte Fault
Map showing the location of Otú Norte Fault
EtymologyOtú
Named byFeininger et al.
Year defined1972
Coordinates07°09′18.6″N 74°47′05.5″W / 7.155167°N 74.784861°W / 7.155167; -74.784861
Country Colombia
RegionAndean
StateAntioquia
CitiesRemedios, Segovia, Zaragoza
Characteristics
RangeCentral Ranges, Andes
Part ofAndean strike-slip faults
Length144.4 km (89.7 mi)
Strike346.4 ± 8
DipEast
Dip angleHigh
Displacement66 km (41 mi)
Slip rate <0.2 mm (0.0079 in)/yr
Tectonics
PlateNorth Andean
StatusInactive
TypeSlightly oblique strike-slip fault
MovementReverse sinistral
Rock unitsCajamarca Complex, Santa Isabel Stock, Antioquia Batholith & Segovia Batholith, San Lucas Complex
AgeQuaternary
OrogenyAndean

The Otú Norte or Otú-Pericos Fault (Spanish: Falla de Otú Norte) is an inactive sinistral oblique strike-slip fault in the department of Antioquia in northern Colombia. The fault has a total length of 144.4 kilometres (89.7 mi) and runs along an average north-northwest to south-southeast strike of 346.4 ± 8, cross-cutting the northern part of the Central Ranges of the Colombian Andes. Together with the parallel Bagre Norte Fault the fault separates the Central Ranges from its northeasternmost continuation, the Serranía de San Lucas.

Etymology

The fault was by Feininger et al. in 1972 named after Otú Airport in vereda Otú in Remedios, Antioquia.[1]

Description

The Otú Norte Fault crosses the northern part of the Central Ranges of the Colombian Andes. The fault strikes north-northwest to south-southeast and appears to branch off the Palestina Fault. The Otú Fault extends in a northwest direction to near Nechí, where it is covered by young Quaternary deposits. The sinistral oblique reverse fault separates blocks of totally dissimilar geology and lithology; the metamorphic Precambrian San Lucas Complex and Jurassic igneous rocks (diorites) of the Segovia Batholith on the east are juxtaposed against the Cretaceous Santa Isabel Stock and Paleozoic quartz-feldspar gneisses and quartzitic arc rocks of the Cajamarca Complex on the west.[2][3] Just west of Remedios, the fault forms the contact between the Cretaceous Antioquia and Jurassic Segovia Batholiths.[4] The northern end apparently splays into several faults that cross the Nechí River.[5]

Activity

A rate of less than 0.2 millimetres (0.0079 in) per year is estimated for the fault, considered inactive. Displaced Quaternary terraces as high as 140 metres (460 ft) are reported and the fault offsets the Tertiary erosion surface of the Central Ranges.[6] A total displacement of the fault has been estimated at 66 kilometres (41 mi).[7]

Economic importance

The fault separates two major gold mining areas in Antioquia; the Segovia-Remedios mining district and La Ye mine in the east,[8][9] and the placer deposits of Gramalote and Cisneros in the west.[10][11] North of Zaragoza, the fault underlies the El Limón mine.[12] Antioquia produces 50% of all gold in Colombia.[13]

The ductile zone of the fault produced mylonites in mainly the amphibolite facies of the Segovia Batholith.[14] This ductile behavior was later overprinted by fragile tectonics, leaving cataclasis and fault breccias in the fault zone as well as striations in the quartz of the batholith. These deformations are interpreted as second grade Riedel shears.[15]

See also

References

  1. ↑ Consorcio GSG, 2015, p.168
  2. ↑ Fonseca et al., 2011, p.40
  3. ↑ Fonseca et al., 2011, p.64
  4. ↑ Geological Map of Antioquia, 1999
  5. ↑ Paris et al., 2000, p.28
  6. ↑ Paris et al., 2000, p.29
  7. ↑ Álvarez et al., 2007, p.49
  8. ↑ Segovia-Remedios mining district
  9. ↑ Mining Atlas - La Ye
  10. ↑ Mining Atlas - Gramalote
  11. ↑ Mining Technology - Cisneros
  12. ↑ Mining Atlas - El Limón
  13. ↑ Fonseca et al., 2011, p.126
  14. ↑ Álvarez et al., 2007, p.47
  15. ↑ Álvarez et al., 2007, p.48

Bibliography

Maps

Further reading

  • Page, W.D. 1986. Seismic geology and seismicity of Northwestern Colombia, 1–200. San Francisco, California, Woodward-Clyde Consultants Report for ISA and Integral Ltda., Medellín.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.