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...

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Detalles Bibliográficos
Autores: García Garmilla, Francisco, Ózer, Sacit, Sari, Bilal
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
Descripción
Sumario: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