Inoceramid shells from the Basque Arc Domain (Basque-Cantabrian Basin) have been studied to determine their behaviour under cathodoluminescence. The shells exhibit a luminescent zoning intimately related to their microstructure and the development of preferred paths of fluid circulation during diagenesis. The luminescent behaviour allows to establish a first classification of the shells according to their preservation degree that can be related to other geochemical and isotopic evidences. Due to the occurrence of nonluminescent areas in the inoceramid shells from Bidart they constitute a good candidate for their use as palaeoenvironmental and chemostratigraphic tool
Cathodoluminescence study of oyster shell growth modalities allows to propose a new method of invest...
Radiolitid rudist shells from the Upper Cretaceous marbles in the southern sector of Menderes Massif...
The detailed geochemical evolution along two transects of the shell of one specimen of Praeradiolite...
Inoceramid shells from the Basque Arc Domain (Basque-Cantabrian Basin) have been studied to determin...
Inoceramid shells (four individuals) from deep facies sediments of the Plentzia Formation) (Santonia...
The petrographic analysis of the inoceramid shells allows to identify some microstructures, which su...
The Quintanaloma Fm (Campanian-Maastrichtian) was deposited in a shallow marine environment and cont...
Inoceramid bivalve shells and host-rock samples from the mid-Maastrichtian carbonate rocks have been...
The cathodoluminescent behaviour of rudist shells and coral skeletal fragments from Ereño Urgonian l...
Lower Maastrichtian inoceramid shells from the Basque-Cantabrian Basin were deposited in a carbonate...
Upper Cretaceous inoceramid bivalves and belemnite rostra from three sections (Aquitaine, Pays de Ca...
Lower Maastrichtian inoceramid shells from the Basque-Cantabrian Basin were deposited in a carbonate...
Detailed petrographic and geochemical analyses of brachiopod shells from the Guadiato Carboniferous ...
The microstructural and cathodoluminescence (CL) study of Crassotrea sp. shells of Somocuevas, Canta...
Pycnodonte or “honeycomb-oysters” (Bivalvia: Gryphaeidea) is an extinct genus of calcite-producing b...
Cathodoluminescence study of oyster shell growth modalities allows to propose a new method of invest...
Radiolitid rudist shells from the Upper Cretaceous marbles in the southern sector of Menderes Massif...
The detailed geochemical evolution along two transects of the shell of one specimen of Praeradiolite...
Inoceramid shells from the Basque Arc Domain (Basque-Cantabrian Basin) have been studied to determin...
Inoceramid shells (four individuals) from deep facies sediments of the Plentzia Formation) (Santonia...
The petrographic analysis of the inoceramid shells allows to identify some microstructures, which su...
The Quintanaloma Fm (Campanian-Maastrichtian) was deposited in a shallow marine environment and cont...
Inoceramid bivalve shells and host-rock samples from the mid-Maastrichtian carbonate rocks have been...
The cathodoluminescent behaviour of rudist shells and coral skeletal fragments from Ereño Urgonian l...
Lower Maastrichtian inoceramid shells from the Basque-Cantabrian Basin were deposited in a carbonate...
Upper Cretaceous inoceramid bivalves and belemnite rostra from three sections (Aquitaine, Pays de Ca...
Lower Maastrichtian inoceramid shells from the Basque-Cantabrian Basin were deposited in a carbonate...
Detailed petrographic and geochemical analyses of brachiopod shells from the Guadiato Carboniferous ...
The microstructural and cathodoluminescence (CL) study of Crassotrea sp. shells of Somocuevas, Canta...
Pycnodonte or “honeycomb-oysters” (Bivalvia: Gryphaeidea) is an extinct genus of calcite-producing b...
Cathodoluminescence study of oyster shell growth modalities allows to propose a new method of invest...
Radiolitid rudist shells from the Upper Cretaceous marbles in the southern sector of Menderes Massif...
The detailed geochemical evolution along two transects of the shell of one specimen of Praeradiolite...