Otú Norte Fault

Otú Norte Fault
Otú Norte Fault
Falla de Otú Norte; Otú-Pericos Fault
Age	Quaternary
Orogeny	Andean

The Otú Norte or Otú-Pericos Fault (

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

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

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]

References

^ Consorcio GSG, 2015, p.168
^ Fonseca et al., 2011, p.40
^ Fonseca et al., 2011, p.64
^ Geological Map of Antioquia, 1999
^ Paris et al., 2000, p.28
^ Paris et al., 2000, p.29
^ Álvarez et al., 2007, p.49
^ Segovia-Remedios mining district
^ Mining Atlas - La Ye
^ Mining Atlas - Gramalote
^ Mining Technology - Cisneros
^ Mining Atlas - El Limón
^ Fonseca et al., 2011, p.126
^ Álvarez et al., 2007, p.47
^ Álvarez et al., 2007, p.48

Bibliography

Álvarez Galindez, Milton; Oswaldo Ordóñez Carmona; Mauricio Valencia Marín, and Antonio Romero Hernández. 2007. Geología de la zona de influencia de la Falla Otú en el Distrito Minero Segovia-Remedios - Geology of the influence zone of the Otú Fault in the Segovia-Remedios mining district. Dyna 74. 41–51. Accessed 2018-06-05.
Consorcio, GSG. 2015. Memoria Plancha 94 - El Bagre - 1:100,000, 1–196.
Servicio Geológico Colombiano
.
Fonseca P. et al, Héctor Antonio. 2011. Memoria Plancha 133 - Puerto Berrío - 1:100,000, 1–145.
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

González, Humberto; Ubaldo Cossio; Mario Maya; Edgar Vásquez, and Magdalí Holguín. 1999. Mapa Geológico de Antioquia 1:400,000, 1.
INGEOMINAS
. Accessed 2017-09-21.
Paris, Gabriel; Michael N. Machette; Richard L. Dart, and Kathleen M. Haller. 2000b. Map of Quaternary Faults and Folds of Colombia and Its Offshore Regions, 1. USGS. Accessed 2017-09-18.