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The Armorica ‘microplate’: fact or fiction? Critical review of the concept and contradictory palaeobiogeographical data
The problem of an ‘Armorica microplate’, detached from Gondwana and having had during part of the Palaeozoic an independent latitudinal evolution, is reconsidered in terms of a critical review of theExpand
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Alternative approach to the Variscan Belt in southwestern Europe: Preorogenic paleobiogeographical constraints
Most of the models proposed for the Variscan Belt of southwestern Europe have been based on structural, metamorphic, and magmatic data. An alternative approach is proposed here, based onExpand
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Late Ordovician glaciation in southern Turkey
ABSTRACT We present a new survey of several Palaeozoic sections in both the Taurus range and the Border Folds that documents typical glacial features including a glacial pavement and striatedExpand
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Deciphering ``temperature'' and ``salinity'' from biogenic phosphates: the δ18O of coexisting fishes and mammals of the Middle Miocene sea of western France
Abstract This study examines the possibility of estimating the oxygen isotopic composition and temperature of seawater by using a combination of δ18O values of phosphate from coexisting fishes andExpand
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Early Palaeozoic palaeobiogeography of the Variscan regions
Abstract The palaeobiogeographic method appears to be an attractive alternative for reconstruction of the palaeogeography of the Variscan regions during the Palaeozoic. The evolution of faunalExpand
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Las rocas sedimentarias del Ordovícico, Silúrico y Devónico de la Zona de Ossa Morena (SO Península Ibérica, España)
Se revisa el registro sedimentario del Ordovicico, Silurico y Devonico de la Zona de Ossa Morena del Macizo Hesperico (o Iberico), referido esencialmente a la parte espanola, pero complementado conExpand
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Terranes within the Iberian Massif: Correlations with West African Sequences
The Iberian Peninsula consists of two very different parts: (1) the eastern half which constitutes the westernmost extension of the Alpine orogen; and (2) the western half (Iberian Massif)Expand
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δ18O and REE contents of phosphatic brachiopods: a comparison between modern and lower Paleozoic populations
Abstract δ18O values of both carbonate (18.7–25.1‰) and phosphate (15.1–16.7‰) components of the francolite from the fossil brachiopod shells are interpreted as the result of a partial resetting ofExpand
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Silurian stratigraphy and paleogeography of the Iberian Peninsula (Spain and Portugal)
32 paginas.-- In: Gutierrez-Marco, J.C. and Rabano, I. (eds.), Proceedings of the Sith International Graptolite Conference of the GWG (IPA) and the 1998 Field Meeting of the InternationalExpand
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A reassessment of the Lochkovian (Lower Devonian) benthic faunas and palynomorphs from the Dornes region (southern Central Iberian Zone, Portugal)
A revision of benthic faunas and palynomorphs previously described from the Dornes syncline, southern Central Iberian Zone, Portugal, complemented with recent research, shows that the Serra de LuacaoExpand
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