The origin and petrologic evolution of the Ordovician Famatinian-Puna arc

M. N. Ducea, J. E. Otamendi, G. W. Bergantz, D. Jianu, L. Petrescu

Research output: Chapter in Book/Report/Conference proceedingChapter

25 Scopus citations

Abstract

Elemental chemistry, radiogenic isotopic data, and zircon U-Pb inheritance patterns for the Famatinian-Puna arc suggest that the primary petrogenetic process operating in the arc was mixing between subarc mantle-derived gabbroic magmas and metasedimentary materials without a substantial component of lower-crustal continental basement rocks. This mixing is observable in the field and evident in variations of chemical elemental parameters and isotopic ratios, revealing that hybridization coupled with fractionation of magmas took place in the upper 25 km of the crust. Intermediate and silicic plutonic rocks of the Famatinia-Puna arc formed in a subduction setting where the thermal and material input of mantle-derived magmas promoted fusion of fertile metasedimentary rocks and favored mixing of gabbroic and dioritic magmas with crustal granitic melts. Whole-rock geochemical and isotopic data for the Famatinian-Puna magmatic belt as a whole demonstrate that the petrologic model studied in detail in the Sierra Valle Fértil-La Huerta section has the potential to explain generation of plutonic and volcanic rocks across the Early Ordovician western Gondwanan proto-Pacific margin. This example further underscores the significance of passive-margin sedimentary accumulations in generating continental arcs.

Original languageEnglish (US)
Title of host publicationGeodynamics of a Cordilleran Orogenic System
Subtitle of host publicationThe Central Andes of Argentina and Northern Chile
EditorsMihai N. Ducea, Mihai N. Ducea, Peter G. DeCelles, Paul A. Kapp, Barbara Carrapa
PublisherGeological Society of America
Pages125-138
Number of pages14
ISBN (Electronic)9780813712123
DOIs
StatePublished - Jan 1 2015

Publication series

NameMemoir of the Geological Society of America
Volume212
ISSN (Print)0072-1069

ASJC Scopus subject areas

  • Geology

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    Ducea, M. N., Otamendi, J. E., Bergantz, G. W., Jianu, D., & Petrescu, L. (2015). The origin and petrologic evolution of the Ordovician Famatinian-Puna arc. In M. N. Ducea, M. N. Ducea, P. G. DeCelles, P. A. Kapp, & B. Carrapa (Eds.), Geodynamics of a Cordilleran Orogenic System: The Central Andes of Argentina and Northern Chile (pp. 125-138). (Memoir of the Geological Society of America; Vol. 212). Geological Society of America. https://doi.org/10.1130/2015.1212(07)