Cathodoluminescence and metamorphism in rudist shells from the Upper Cretaceous marbles of Menderes Massif (Western Turkey)
Radiolitid rudist shells from the Upper Cretaceous marbles in the southern sector of Menderes Massif (Turkey) have been studied under cathodoluminescence microscopy (CL). The background ofequant calcite mosaic appears non-luminescent, and only some scarce relicts of growth lines and walls are red an...
| Autores: | , , |
|---|---|
| Tipo de recurso: | artículo |
| Fecha de publicación: | 2004 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | inglés |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/8919 |
| Acceso en línea: | http://hdl.handle.net/10272/8919 |
| Access Level: | acceso abierto |
| Palabra clave: | Rudist shells Upper Cretaceous Menderes Massif Turkey Metamorphism Cathodoluminescence Conchas de rudistas Cretácico Superior Macizo de Menderes Turquía Metamorfismo Catodoluminiscencia |
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Cathodoluminescence and metamorphism in rudist shells from the Upper Cretaceous marbles of Menderes Massif (Western Turkey)Catodoluminiscencia y metamorfismo en conchas de rudistas de los mármoles del Cretácico Superior del Macizo de Menderes (W de Turquía)García Garmilla, FranciscoÓzer, SacitSari, BilalRudist shellsUpper CretaceousMenderes MassifTurkeyMetamorphismCathodoluminescenceConchas de rudistasCretácico SuperiorMacizo de MenderesTurquíaMetamorfismoCatodoluminiscenciaRadiolitid rudist shells from the Upper Cretaceous marbles in the southern sector of Menderes Massif (Turkey) have been studied under cathodoluminescence microscopy (CL). The background ofequant calcite mosaic appears non-luminescent, and only some scarce relicts of growth lines and walls are red and yellow-luminescent. CL observations allow us to think that the Upper Cretaceous marbles of the Menderes Massif were completely homogeneized through high-pressure metamorphism during the Alpine history that led to a strong recrystallization to non-luminescent ferroan calcite. After this process, the "honeycomb" microstructure still remains ill-preserved as some isolated patchs. From our previous observations in bivalve shells from the Middle-to-Upper Cretaceous of the Basque-Cantabrian Region (northern Spain) we think that, in spite of metamorphism, luminiscence survives restricted to the shell parts which originally could host a more dense concentration in organic matterSociedad Geológica de España20042004-01-0120042004-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/8919reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelvainstname:Universidad de Huelva (UHU)Inglésengopen accesshttp://purl.org/coar/access_right/c_abf2Atribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/info:eu-repo/semantics/openAccessoai:ariasmontano.uhu.es:10272/89192026-06-02T14:58:11Z |
| dc.title.none.fl_str_mv |
Cathodoluminescence and metamorphism in rudist shells from the Upper Cretaceous marbles of Menderes Massif (Western Turkey) Catodoluminiscencia y metamorfismo en conchas de rudistas de los mármoles del Cretácico Superior del Macizo de Menderes (W de Turquía) |
| title |
Cathodoluminescence and metamorphism in rudist shells from the Upper Cretaceous marbles of Menderes Massif (Western Turkey) |
| spellingShingle |
Cathodoluminescence and metamorphism in rudist shells from the Upper Cretaceous marbles of Menderes Massif (Western Turkey) García Garmilla, Francisco Rudist shells Upper Cretaceous Menderes Massif Turkey Metamorphism Cathodoluminescence Conchas de rudistas Cretácico Superior Macizo de Menderes Turquía Metamorfismo Catodoluminiscencia |
| title_short |
Cathodoluminescence and metamorphism in rudist shells from the Upper Cretaceous marbles of Menderes Massif (Western Turkey) |
| title_full |
Cathodoluminescence and metamorphism in rudist shells from the Upper Cretaceous marbles of Menderes Massif (Western Turkey) |
| title_fullStr |
Cathodoluminescence and metamorphism in rudist shells from the Upper Cretaceous marbles of Menderes Massif (Western Turkey) |
| title_full_unstemmed |
Cathodoluminescence and metamorphism in rudist shells from the Upper Cretaceous marbles of Menderes Massif (Western Turkey) |
| title_sort |
Cathodoluminescence and metamorphism in rudist shells from the Upper Cretaceous marbles of Menderes Massif (Western Turkey) |
| dc.creator.none.fl_str_mv |
García Garmilla, Francisco Ózer, Sacit Sari, Bilal |
| author |
García Garmilla, Francisco |
| author_facet |
García Garmilla, Francisco Ózer, Sacit Sari, Bilal |
| author_role |
author |
| author2 |
Ózer, Sacit Sari, Bilal |
| author2_role |
author author |
| dc.contributor.none.fl_str_mv |
|
| dc.subject.none.fl_str_mv |
Rudist shells Upper Cretaceous Menderes Massif Turkey Metamorphism Cathodoluminescence Conchas de rudistas Cretácico Superior Macizo de Menderes Turquía Metamorfismo Catodoluminiscencia |
| topic |
Rudist shells Upper Cretaceous Menderes Massif Turkey Metamorphism Cathodoluminescence Conchas de rudistas Cretácico Superior Macizo de Menderes Turquía Metamorfismo Catodoluminiscencia |
| description |
Radiolitid rudist shells from the Upper Cretaceous marbles in the southern sector of Menderes Massif (Turkey) have been studied under cathodoluminescence microscopy (CL). The background ofequant calcite mosaic appears non-luminescent, and only some scarce relicts of growth lines and walls are red and yellow-luminescent. CL observations allow us to think that the Upper Cretaceous marbles of the Menderes Massif were completely homogeneized through high-pressure metamorphism during the Alpine history that led to a strong recrystallization to non-luminescent ferroan calcite. After this process, the "honeycomb" microstructure still remains ill-preserved as some isolated patchs. From our previous observations in bivalve shells from the Middle-to-Upper Cretaceous of the Basque-Cantabrian Region (northern Spain) we think that, in spite of metamorphism, luminiscence survives restricted to the shell parts which originally could host a more dense concentration in organic matter |
| publishDate |
2004 |
| dc.date.none.fl_str_mv |
2004 2004-01-01 2004 2004-01-01 |
| dc.type.none.fl_str_mv |
journal article http://purl.org/coar/resource_type/c_6501 |
| dc.type.openaire.fl_str_mv |
info:eu-repo/semantics/article |
| format |
article |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/10272/8919 |
| url |
http://hdl.handle.net/10272/8919 |
| dc.language.none.fl_str_mv |
Inglés eng |
| language_invalid_str_mv |
Inglés |
| language |
eng |
| dc.rights.none.fl_str_mv |
open access http://purl.org/coar/access_right/c_abf2 Atribución-NoComercial-SinDerivadas 3.0 España http://creativecommons.org/licenses/by-nc-nd/3.0/es/ |
| dc.rights.openaire.fl_str_mv |
info:eu-repo/semantics/openAccess |
| rights_invalid_str_mv |
open access http://purl.org/coar/access_right/c_abf2 Atribución-NoComercial-SinDerivadas 3.0 España http://creativecommons.org/licenses/by-nc-nd/3.0/es/ |
| eu_rights_str_mv |
openAccess |
| dc.format.none.fl_str_mv |
application/pdf |
| dc.publisher.none.fl_str_mv |
Sociedad Geológica de España |
| publisher.none.fl_str_mv |
Sociedad Geológica de España |
| dc.source.none.fl_str_mv |
reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelva instname:Universidad de Huelva (UHU) |
| instname_str |
Universidad de Huelva (UHU) |
| reponame_str |
Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| collection |
Arias Montano. Repositorio Institucional de la Universidad de Huelva |
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15,223283 |