Universidad Complutense de Madrid
E-Prints Complutense

Late Cambrian – Early Ordovician magmatism in the Sierra de Pie de Palo, Sierras Pampeanas (Argentina): implications for the early evolution of the proto-Andean margin of Gondwana

Impacto

Downloads

Downloads per month over past year

Ramacciotti, Carlos and Casquet, César and Baldo, Edgardo G. and Alasino, Pablo H. and Galindo Francisco, Mª del Carmen and Dahlquist, Juan A. (2020) Late Cambrian – Early Ordovician magmatism in the Sierra de Pie de Palo, Sierras Pampeanas (Argentina): implications for the early evolution of the proto-Andean margin of Gondwana. Geological Magazine, 157 (2). pp. 321-339. ISSN 0016-7568, ESSN: 1469-5081

[img] PDF
Restringido a Repository staff only

3MB

Official URL: https://www.cambridge.org/core/journals/geological-magazine/article/late-cambrian-early-ordovician-magmatism-in-the-sierra-de-pie-de-palo-sierras-pampeanas-argentina-implications-for-the-early-evolution-of-the-protoandean-margin-of-gondwana/7EF5E27526E5AF



Abstract

The Sierra de Pie de Palo, in the Argentinean Sierras Pampeanas (Andean foreland), consists of a Mesoproterozoic basement and an Ediacaran – upper Cambrian sedimentary cover that underwent folding, thrusting and metamorphism during the Ordovician Famatinian orogeny. Mafic rocks and granitoids of the easternmost Sierra de Pie de Palo provide information about the magmatic activity at the proto-Andean margin of Gondwana during late Cambrian – Early Ordovician time. Magmatic activity began in the Sierra de Pie de Palo as dykes, sills and small intrusions of tholeiitic gabbros between 490 and 470 Ma, before shortening and regional metamorphism. Variable mantle sources (Nd depleted mantle age, TDM between 1.7 and 1.3 Ga) were involved in the mafic magmatism. Nd-isotope signatures were probably inherited from a Mesoproterozoic subcontinental mantle. Mafic magmatism was coincident with collapse of a Cambrian carbonate-siliciclastic platform that extended along SW Gondwana, and was probably coeval with the beginning of subduction. After mafic magmatism, peraluminous granitoids were emplaced in the Sierra de Pie de Palo along ductile shear zones during a contractional tectonic phase, coeval with moderate to high P/T metamorphism, and with the Cordilleran-type magmatic arc that resulted from a flare-up at c. 470 Ma. Granitoids resulted mainly from partial melting of metasedimentary rocks, although some hybridization with juvenile magmas and/or rocks cannot be ruled out. The evidence shown here further implies that the Pie de Palo block was part of the continental upper plate during the Famatinian subduction, and not an exotic block that collided with the Gondwana margin.


Item Type:Article
Uncontrolled Keywords:Famatinian magmatism, U–Pb SHRIMP geochronology, active continental margin, SW Gondwana margin
Subjects:Sciences > Geology > Geodynamics
Sciences > Geology > Geochemistry
Sciences > Geology > Petrology
ID Code:59417
Deposited On:05 Mar 2020 17:15
Last Modified:06 Mar 2020 08:22

Origin of downloads

Repository Staff Only: item control page