Back to results
Bibliographic record · Consultation and access
Artículo

New hints on the evolution of the Eastern Magmatic Belt, Puna Argentina. SW Gondwana margin: Zircon U-Pb ages and Hf isotopes in the Pachamama Igneous-Metamorphic Complex

Ortiz Yañez, Agustín et al · Pergamon-Elsevier Science Ltd · 2019

Open-access full text
Quick overview. Review the resource’s basic details, then access the content using the main button. This page shows only the information needed to identify, cite, and open the work.

Resource access

Open the content from the main option or choose another available source.

CONICET Digital CONICET Digital OAI-PMH
Entrar por CONICET Digital
Main access

Open-access full text

Texto completo identificado como acceso abierto.
Open text

Summary

Descripción general del contenido del recurso.

There are various geotectonic interpretations of the origin of the Eastern Magmatic Belt as part of the Lower Paleozoic Orogen at the Southwestern Gondwana margin in the Puna, NW Argentina. In this research paper, we obtained zircon U-Pb and Lu-Hf in key rocks from the Pachamama Igneous Metamorphic Complex in order to further constrain the evolution of the Eastern Magmatic Belt. We contribute to the understanding of magmatic sources, processes, and the emplacement of magmas during Lower Paleozoic times in this sector of the Puna. These will allow improving the reconstruction of the geotectonic setting that controlled the Eastern Magmatic Belt. A monzogranite from the mentioned complex yielded concordant zircon U-Pb ages from ∼530 Ma and ∼490 Ma, with the magmatic activity summit at ∼515-510 Ma. In addition to the monzogranite, the wall rocks (schist and gneiss), revealed zircon isotope ɛHf(t) values between +2 and −3 and whole rock ɛNd(t) values between +2 and −5, with TDM ages between 1.3 and 1.6 Ga. These indicate that the rocks from the Pachamama Igneous Metamorphic Complex, derived from a mixture of a reworked Mesoproterozoic crustal source and juvenile mantle-derived magmas. The combined data obtained in this contribution together with previous work, allow us to suggest that a long-lived magmatic event formed the granitoids in the Eastern Magmatic Belt from ∼540 Ma until ∼440 Ma. This event was represented by periods of low-level magmatic activity, interrupted periodically by short bursts of high-volume magmatism, triggered by repeated magmatic underplating. Fil: Ortiz Yañez, Agustín. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Bio y Geociencias del Noroeste Argentino. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Instituto de Bio y Geociencias del Noroeste Argentino; Argentina. Universidade do Brasília; Brasil Fil: Suzaño, Nestor Omar. Universidad Nacional de Jujuy; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Investigaciones en Energía no Convencional. Universidad Nacional de Salta. Facultad de Ciencias Exactas. Departamento de Física. Instituto de Investigaciones en Energía no Convencional; Argentina

How to cite

Elegí el formato que necesitás y copiá la referencia al portapapeles.

APA 7

Ortiz Yañez, A. E. A. (2019). New hints on the evolution of the Eastern Magmatic Belt, Puna Argentina. SW Gondwana margin: Zircon U-Pb ages and Hf isotopes in the Pachamama Igneous-Metamorphic Complex. http://hdl.handle.net/11336/120672

MLA

Ortiz Yañez, Agustín et al. "New hints on the evolution of the Eastern Magmatic Belt, Puna Argentina. SW Gondwana margin: Zircon U-Pb ages and Hf isotopes in the Pachamama Igneous-Metamorphic Complex." 2019. http://hdl.handle.net/11336/120672.

Chicago

Ortiz Yañez, Agustín et al. 2019. "New hints on the evolution of the Eastern Magmatic Belt, Puna Argentina. SW Gondwana margin: Zircon U-Pb ages and Hf isotopes in the Pachamama Igneous-Metamorphic Complex.". http://hdl.handle.net/11336/120672.

Harvard

Ortiz Yañez, A. E. A. 2019, New hints on the evolution of the Eastern Magmatic Belt, Puna Argentina. SW Gondwana margin: Zircon U-Pb ages and Hf isotopes in the Pachamama Igneous-Metamorphic Complex, Pergamon-Elsevier Science Ltd, available at: http://hdl.handle.net/11336/120672 [Accessed 9 Aug. 2026].

Share and print

Save the record, copy its permanent link, or print it as a PDF.

Export reference

You can export the record in common formats for use in a reference manager.

Resource details

Bibliographic information to help confirm that this is the correct material.

Title
New hints on the evolution of the Eastern Magmatic Belt, Puna Argentina. SW Gondwana margin: Zircon U-Pb ages and Hf isotopes in the Pachamama Igneous-Metamorphic Complex
Author / contributors
Ortiz Yañez, Agustín et al
Publisher
Pergamon-Elsevier Science Ltd
Publication year
2019
ISSN
0895-9811
ISSN
0895-9811
Language
English

Subjects

Explore related resources through these subjects.

Copied