The dykes in the western fringe of the Ybytyruzú Hills, central‑eastern Paraguay region

Authors

  • Celso de Barros Gomes Institute of Geosciences, Universidade de São Paulo ‑ USP
  • Ana Maria Castillo Clerici Clerici Technical Coordinator attached. Framework Program La Plata Basin, Buenos Aires, Argentina
  • Victor Velázquez Fernandez School of Arts, Sciences and Humanities, Universidade de São Paulo ‑ USP
  • Angelo De Min Department of Mathematics and Geosciences, University of Trieste, Trieste, Italy
  • Piero Comin‑Chiaramonti Department of Mathematics and Geosciences, University of Trieste, Trieste, Italy

DOI:

https://doi.org/10.11606/issn.2316-9095.v17-121977

Keywords:

Ybytyruzú, Eastern Paraguay, Potassic Alkaline Dykes.

Abstract

The Cordillera del Ybytyruzú region of central‑eastern Paraguay is predominantly formed by tholeiitic lava flows from the Early Cretaceous age (130–134 Ma) cut by K‑alkaline dykes and intrusive bodies aged between 125 and 127 Ma. Petrochemical studies focusing on 14 samples of dykes from the region show an apparent affinity to Roman Province Type rocks and total consistency with the overall petrographic association of the Asunción‑Sapucai‑Villarrica (ASV) graben. Two main potassic suites are distinguished: B‑P (basanite‑tephrite‑phonotephrite‑phonolite) and AB‑T (alkali basalt‑trachybasalt‑trachyandesite‑trachyphonolite/trachyte).The occurrence of lamproitic rocks in the area has so far not been confirmed.

Downloads

Download data is not yet available.

Published

2017-08-01

Issue

Section

Articles

How to Cite

Gomes, C. de B., Clerici, A. M. C. C., Fernandez, V. V., Min, A. D., & Comin‑Chiaramonti, P. (2017). The dykes in the western fringe of the Ybytyruzú Hills, central‑eastern Paraguay region. Geologia USP. Série Científica, 17(2), 131-141. https://doi.org/10.11606/issn.2316-9095.v17-121977