Geoquímica de rocas ígneas Permo-Triásicas del norte de Chile (28°-30°15‘S): Implicancias en la dinámica del margen pre-Andino

Translated title of the contribution: Geochemistry of permian to triassic igneous rocks from northern Chile (28°-30°15‘S): Implications on the dynamics of the proto-Andean margin

Felipe Coloma, Ximena Valin, Verónica Oliveros, Paulina Vásquez, Christian Creixell, Esteban Salazar, Mihai N. Ducea

Research output: Contribution to journalArticle

23 Scopus citations

Abstract

Permian to Triassic igneous rocks cropping out in the Coastal and Frontal cordilleras in northern Chile between 28°00‘S and 30°15‘S have long been interpreted to represent products of magmatism related to an extensional tectonic setting, either as the result of crustal anatexis or asthenospheric mantle decompression melting, in a passive continental margin. Eighty-six samples of plutonic (61) and volcanic (25) rocks from this region are characterized petrographically and geochemically. They are Permian to Early Jurassic in age, but the majority of the studied rocks correspond to the Lower to Middle Triassic Chollay Plutonic Complex, the volumetrically most important unit in the area. The rock samples have features typical of magmas derived from flux-induced melting of a depleted mantle such as: broad range of petrographic composition with predominance of intermediate to acid members, highly porphyrytic volcanic rocks, magnetite as the Fe-Ti oxide mineral phase, enrichment in LILE over HFSE, marked depletion in Nb, Ta, Ti, and P and moderate to no negative Eu anomalies. Few of the studied rock samples (<10%) have alkaline signature and trace element contents representative of anorogenic magmatism. In this work, we propose that subduction of an oceanic plate beneath the South American continent is responsible for the evolution of the margin from the Permian to Early Jurassic, at the studied latitudes. A preliminary interpretation of the margin architecture of the Andean margin from the Permian to the Triassic would be that the Chanchoquin and Chollay plutonic complexes represent the roots of a magmatic arc developed from the Permian to the Middle or early Late Triassic, whereas the Guanaco Sonso and Pastos Blancos formations would be the shallower parts of such arc. The La Totora Formation and some volumetrically minor Upper Triassic intrusive units represent magmatic products with alkaline signatures, which developed immediately before the establishment of the magmatic arc in the present-day Coastal Cordillera (during the Rhaetian to Early Jurassic).

Translated title of the contributionGeochemistry of permian to triassic igneous rocks from northern Chile (28°-30°15‘S): Implications on the dynamics of the proto-Andean margin
Original languageSpanish
Pages (from-to)147-178
Number of pages32
JournalAndean Geology
Volume44
Issue number2
DOIs
StatePublished - Jan 1 2017

Keywords

  • Frontal cordillera
  • Geochemistry
  • Pre-andean
  • Subduction
  • Triassic

ASJC Scopus subject areas

  • Geology
  • Geochemistry and Petrology
  • Stratigraphy
  • Palaeontology

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