An overview of Precambrian rocks in Sonora

The oldest stratified rock recognized in NW Sonora (and in Mexico) are deformed muscovite-quartz schists, quartzites, and biotite-quartzofeldspathic gneisses near Caborca, which are cut by calcalkaline intrusives ranging from 1,710 to 1,750 m.y. in age. Southwest of Caborca, upper amphibolite facie...

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Main Authors: Thomas H. Anderson, Leon T. Silver
Format: Article
Language:English
Published: Universidad Nacional Autónoma de México 2019-03-01
Series:Revista Mexicana de Ciencias Geológicas
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Online Access:https://rmcg.unam.mx/index.php/rmcg/article/view/1318
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author Thomas H. Anderson
Leon T. Silver
author_facet Thomas H. Anderson
Leon T. Silver
author_sort Thomas H. Anderson
collection DOAJ
description The oldest stratified rock recognized in NW Sonora (and in Mexico) are deformed muscovite-quartz schists, quartzites, and biotite-quartzofeldspathic gneisses near Caborca, which are cut by calcalkaline intrusives ranging from 1,710 to 1,750 m.y. in age. Southwest of Caborca, upper amphibolite facies layered quartzofeldspathic and amphibolitic gneisses were apparently deformed and metamorphosed at about 1,660 ± 15 m.y. ago, concealing original lithologies and ages. In northeastern Sonora, a younger belt of eugeosynclinal strata, about 1,680 ± 20 m.y. old was tightly folded and metamorphosed to greenschist facies about 1,650 m. y. ago. Numerous granitic plutons intruded into the older Precambrian crust about 1,410 to 1,440 m.y. ago. These major intrusive masses are not known to have been accompanied by regional sedimentation or deformation. Rare, small plutons of micrographic granite added to the Precambrian crystalline complexes about 1,100 m.y. ago, are the youngest Precambrian igneous rocks recognized... In order to continue, download the full paper in PDF.
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spelling doaj-art-aef5d2e82768496596c6d5bafafb92022025-08-20T03:44:51ZengUniversidad Nacional Autónoma de MéxicoRevista Mexicana de Ciencias Geológicas1026-87742007-29022019-03-0152An overview of Precambrian rocks in SonoraThomas H. Anderson0Leon T. Silver1Department of Geology and Planetary Sciences, University of Pittsburgh, Pittsburg, Pennsylvania 15260, U.S.A.Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, U.S.A. The oldest stratified rock recognized in NW Sonora (and in Mexico) are deformed muscovite-quartz schists, quartzites, and biotite-quartzofeldspathic gneisses near Caborca, which are cut by calcalkaline intrusives ranging from 1,710 to 1,750 m.y. in age. Southwest of Caborca, upper amphibolite facies layered quartzofeldspathic and amphibolitic gneisses were apparently deformed and metamorphosed at about 1,660 ± 15 m.y. ago, concealing original lithologies and ages. In northeastern Sonora, a younger belt of eugeosynclinal strata, about 1,680 ± 20 m.y. old was tightly folded and metamorphosed to greenschist facies about 1,650 m. y. ago. Numerous granitic plutons intruded into the older Precambrian crust about 1,410 to 1,440 m.y. ago. These major intrusive masses are not known to have been accompanied by regional sedimentation or deformation. Rare, small plutons of micrographic granite added to the Precambrian crystalline complexes about 1,100 m.y. ago, are the youngest Precambrian igneous rocks recognized... In order to continue, download the full paper in PDF. https://rmcg.unam.mx/index.php/rmcg/article/view/1318tectonic, Precambrian, Sonora, Mexico
spellingShingle Thomas H. Anderson
Leon T. Silver
An overview of Precambrian rocks in Sonora
Revista Mexicana de Ciencias Geológicas
tectonic, Precambrian, Sonora, Mexico
title An overview of Precambrian rocks in Sonora
title_full An overview of Precambrian rocks in Sonora
title_fullStr An overview of Precambrian rocks in Sonora
title_full_unstemmed An overview of Precambrian rocks in Sonora
title_short An overview of Precambrian rocks in Sonora
title_sort overview of precambrian rocks in sonora
topic tectonic, Precambrian, Sonora, Mexico
url https://rmcg.unam.mx/index.php/rmcg/article/view/1318
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