Las ignimbritas del complejo volcánico Coranzuli (Puna Argentina-Andes Centrales)

Authors

  • R. Seggiaro Catedra de Petrología. Facultad de Ciencias. Universidad Nacional de Salta
  • S. A. Gorustovich Comisión Nacional de Energía Atómica. Facultad de Ciencias. Universidad Nacional de Salta.
  • J. Martí Instituto de Geología "Jaime Almera" (CSIC).

DOI:

https://doi.org/10.3989/egeol.87435-6605

Keywords:

Ignimbrites, Cª Coranzulí, Central Andes, Puna Argentina

Abstract


The Coranzulí is a large Upper Miocene volcanic complex located on a NE-SW and NW-SE regional faults intersection, at 66º 15' W 23º S, in the Northwest of Argentina in Jujuy province. It corresponds to one of four large volcanic complexes which represent the end of Transversal Volcanic Chaines in La Puna Argentina in the Central Andes. The volcanic activity was characterized by at least four separate ignimbrite eruptions which produced four different ignimbrite sheets. These are well welded, very crystal-rich, lithie poor ignimbrites and have a moderate to high pumice content. The total volume of the Coranzuli ignimbrites exeededs 650 Km3. Preliminary data indicate that the eruption oeeurred from a homogeneous magmatic chamber without zoning. The emplacement characteristics of the ignimbrites and the lack of basal or interbedded plinian fall deposits suggest that the eruptions developed quickly to massive proportions.

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Published

1987-12-30

How to Cite

Seggiaro, R., Gorustovich, S. A., & Martí, J. (1987). Las ignimbritas del complejo volcánico Coranzuli (Puna Argentina-Andes Centrales). Estudios Geológicos, 43(5-6), 345–358. https://doi.org/10.3989/egeol.87435-6605

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Articles