Search results for "Structural basin"

showing 2 items of 292 documents

Late Quaternary marine ostracods of the Basque Basin (S Bay of Biscay): taxonomy and distribution

2018

Late Quaternary taxonomy and ecologic and age distributions of ostracods from the Basque Basin (S Bay of Biscay) are described. More than forty-four thousands ostracod specimens have been obtained from one hundred surface samples and core samples from six cores located in shelf and upper bathyal depths and other infrabathyal core as comparative deep reference. A total of 155 species have been taxonomically described, belonging to 67 genera. Most characteristic species (123) have been SEM figured, and ecologic-geographic distributions and ages have been provided for all species. The resulting database will be a useful help for palaeoceanographic and palaeoclimatologic studies of the region.

taxonomy and distribution. Artículo [Late Quaternary marine ostracods of the Basque Basin (S Bay of Biscay)]biologyUNESCO::CIENCIES DE LA VIDAPaleontologyStructural basinbiology.organism_classificationQE701-760Bathyal zonePaleontologyOstracodLate Quaternary marine ostracods of the Basque Basin (S Bay of Biscay): taxonomy and distribution. ArtículoTaxonomy (biology):CIENCIES DE LA VIDA [UNESCO]QuaternaryBayGeologySpanish Journal of Palaeontology
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Mise en évidence d'un Sénonien gypseux sous la série phosphatée du bassin des Ouled Abdoun: un nouveau point de départ pour l'origine des zones déran…

2013

In the Ouled Abdoun sedimentary basin (Morocco), the phosphatic series is composed of regular interbedded phosphatic and marly limestone layers. Exploitation of the phosphate in some deposits in this basin collides frequently with problems bound to the existence, in the phosphatic series, of disturbed areas (sterile bodies) qualified as derangements by the mining engineers of the Office Cherifian Phosphate Group (OCP). Their presence in the phosphatic layers causes two kinds of problems: (1) since the whole phosphatic sequence is overlain by a Quaternary cover, we do not know their volume proportion in the phosphatic layers, and therefore the reserves estimations can be wrong (2) they are g…

zone dérangéeGeochemistryBoreholeMineralogyStructural basin[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphydisturbed areaGroup (stratigraphy)Khouribgasérie phosphatéeQE1-996.5geographygeography.geographical_feature_categorylcsh:QE1-996.5SénonienSenonianGeologyOuled Abdoun BasinPhosphatic seriesSedimentary basinkarstKarstgypsumDiagenesislcsh:GeologyMarocMoroccogypseQuaternaryGeology
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