Textural and genetic relationships between glauconite and celadonite at the nanoscale: two different structural-compositional fields

Glauconite and celadonite coexist at the nanometre scale in Early Jurassic\nsubmarine volcanic rocks of the Betic Cordillera (southern Spain) as a\nresult of microbial activity. Samples from the limit between the two micas, \nrecognizable in scanning electron microscopy, have been extracted using th...

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Detalles Bibliográficos
Autores: Nieto, Fernando, Abad, Isabel, Bauluz, Blanca, Reolid, Matías
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2021
País:España
Institución:Universidad de Zaragoza
Repositorio:Zaguán. Repositorio Digital de la Universidad de Zaragoza
OAI Identifier:oai:zaguan.unizar.es:109426
Acceso en línea:http://zaguan.unizar.es/record/109426
Access Level:acceso abierto
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spelling Textural and genetic relationships between glauconite and celadonite at the nanoscale: two different structural-compositional fieldsNieto, FernandoAbad, IsabelBauluz, BlancaReolid, MatíasGlauconite and celadonite coexist at the nanometre scale in Early Jurassic\nsubmarine volcanic rocks of the Betic Cordillera (southern Spain) as a\nresult of microbial activity. Samples from the limit between the two micas, \nrecognizable in scanning electron microscopy, have been extracted using the\nfocussed ion beam technique and studied by high-resolution analytical\nelectron microscopy. Both micas are present as randomly oriented\ndifferentiated small crystals in the boundary area. They define clearly\ndistinct compositional fields with gaps affecting to Fe, Mg and K. At the\nlattice scale, celadonite shows a high degree of order, with homogeneous\norientation of the visible lattice parameters being a difference from\nglauconite, formed by packets no more than 10-layers thick. Smectite layers\nwere also detected alongside glauconite packets, in accordance with X-ray\ndiffractograms which indicate that glauconite is a mica-smectite\ninterstratification being more than 90\u2009% mica layers. The compositional\ngap indicates that celadonite is not the endmember of the glauconitic series\nand the two micas represent two different structural tendencies of mica, \nwith glauconite having more distorted octahedral sheets, indicated by\nsystematically higher b parameters than celadonite.2021info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttp://zaguan.unizar.es/record/109426reponame:Zaguán. Repositorio Digital de la Universidad de Zaragozainstname:Universidad de ZaragozaInglésinfo:eu-repo/grantAgreement/ES/DGA/E18-17Rinfo:eu-repo/grantAgreement/ES/MCIU-AEI-FEDER/PGC2018-094573-B-I00info:eu-repo/grantAgreement/ES/MCIU-AEI-FEDER/PID2019-104624RB-I00info:eu-repo/grantAgreement/ES/MCIU-AEI-FEDER/RTI2018-093419-B-I00info:eu-repo/semantics/openAccessoai:zaguan.unizar.es:1094262026-05-29T13:59:51Z
dc.title.none.fl_str_mv Textural and genetic relationships between glauconite and celadonite at the nanoscale: two different structural-compositional fields
title Textural and genetic relationships between glauconite and celadonite at the nanoscale: two different structural-compositional fields
spellingShingle Textural and genetic relationships between glauconite and celadonite at the nanoscale: two different structural-compositional fields
Nieto, Fernando
title_short Textural and genetic relationships between glauconite and celadonite at the nanoscale: two different structural-compositional fields
title_full Textural and genetic relationships between glauconite and celadonite at the nanoscale: two different structural-compositional fields
title_fullStr Textural and genetic relationships between glauconite and celadonite at the nanoscale: two different structural-compositional fields
title_full_unstemmed Textural and genetic relationships between glauconite and celadonite at the nanoscale: two different structural-compositional fields
title_sort Textural and genetic relationships between glauconite and celadonite at the nanoscale: two different structural-compositional fields
dc.creator.none.fl_str_mv Nieto, Fernando
Abad, Isabel
Bauluz, Blanca
Reolid, Matías
author Nieto, Fernando
author_facet Nieto, Fernando
Abad, Isabel
Bauluz, Blanca
Reolid, Matías
author_role author
author2 Abad, Isabel
Bauluz, Blanca
Reolid, Matías
author2_role author
author
author
description Glauconite and celadonite coexist at the nanometre scale in Early Jurassic\nsubmarine volcanic rocks of the Betic Cordillera (southern Spain) as a\nresult of microbial activity. Samples from the limit between the two micas, \nrecognizable in scanning electron microscopy, have been extracted using the\nfocussed ion beam technique and studied by high-resolution analytical\nelectron microscopy. Both micas are present as randomly oriented\ndifferentiated small crystals in the boundary area. They define clearly\ndistinct compositional fields with gaps affecting to Fe, Mg and K. At the\nlattice scale, celadonite shows a high degree of order, with homogeneous\norientation of the visible lattice parameters being a difference from\nglauconite, formed by packets no more than 10-layers thick. Smectite layers\nwere also detected alongside glauconite packets, in accordance with X-ray\ndiffractograms which indicate that glauconite is a mica-smectite\ninterstratification being more than 90\u2009% mica layers. The compositional\ngap indicates that celadonite is not the endmember of the glauconitic series\nand the two micas represent two different structural tendencies of mica, \nwith glauconite having more distorted octahedral sheets, indicated by\nsystematically higher b parameters than celadonite.
publishDate 2021
dc.date.none.fl_str_mv 2021
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dc.identifier.none.fl_str_mv http://zaguan.unizar.es/record/109426
url http://zaguan.unizar.es/record/109426
dc.language.none.fl_str_mv Inglés
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