Trapa-Trapa Formation

Trapa-Trapa Formation
Stratigraphic range: Miocene
Type Geological formation
Underlies Cola de Zorro Formation
Campanario Formation
Overlies Cura-Mallín Formation
Lithology
Primary Andesite lava, basaltic andesite lava, pyroclastic rocks, epiclastic rocks
Other Basalt lava, dacite lava, tuff
Location
Region Araucanía Region, Bío Bío Region, Maule Region
Neuquén Province
Country  Chile
 Argentina
Type section
Named for Estero Trapa-Trapa

Trapa-Trapa Formation (Spanish: Formación Trapa-Trapa) is a volcano-sedimentary formation of Miocene age in south-central Chile and nearby parts of Argentina. The largest outcrops lie in the Andes while the Chilean Central Valley host some of the smaller outcrops. The volcanic rocks of the formation are of calc-alkaline character, and are less silicic than contemporary volcanic rocks found further north in Farellones Formation.[1]

References

  1. Muñoz B., Jorge; Niemeyer R., Hans (1984). "Petrología de la formación Trapa-Trapa y consideraciones acerca del volcanismo mioceno entre los 36° y 39° lat. S (codillera principal)". Revista Geológica de Chile. 23: 53–67. Retrieved 23 August 2016.
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