Letteratura scientifica selezionata sul tema "Le Mas-d'Azil (Ariège ; région)"
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Articoli di riviste sul tema "Le Mas-d'Azil (Ariège ; région)":
Vialou, Denis. "L’art des grottes en Ariège magdalénienne". Gallia préhistoire. Suppléments 22, n. 1 (1986): 5–28. http://dx.doi.org/10.3406/galip.1986.2542.
Duhard, Jean-Pierre. "Les figurations humaines sculptées et gravées du Mas d'Azil (Ariège)". Gallia préhistoire 34, n. 1 (1992): 289–301. http://dx.doi.org/10.3406/galip.1992.2310.
Ferraro Júnior, Luiz Antonio, e Marcel Bursztyn. "DAS SESMARIAS À RESISTÊNCIA AO CERCAMENTO: razões históricas dos Fundos de Pasto". Caderno CRH 23, n. 59 (21 dicembre 2010). http://dx.doi.org/10.9771/ccrh.v23i59.19108.
Tesi sul tema "Le Mas-d'Azil (Ariège ; région)":
Pallier, Céline. "De l’enregistrement sédimentaire en milieu karstique à la taphonomie des sites archéologiques du Paléolithique supérieur (MIS 3-MIS 2) : les apports de la grotte du Mas d’Azil et de la vallée de l’Arize (Pyrénées, France)". Electronic Thesis or Diss., Toulouse 2, 2021. http://www.theses.fr/2021TOU20011.
The Mas d'Azil cave, crossed by the Arize river, has preserved evidence of the hydrosedimentary dynamics of the last glacial cycle, which conditioned both human occupation during the Upper Palaeolithic and the conservation of archaeological remains. Thus, how can the study of such a sedimentary recorder answer the question of the archaeological gaps of the last ice age?Hiatuses, either chronological or spatial, are observed in the cave's occupations. What significance can be attributed to them : absence of humans or differential conservation? At the transition MIS 3-MIS 2, a phase of sedimentary aggradation has constrained occupation in the cave, while playing a major role in the conservation or erosion of the remains. It allowed the partial conservation of the Aurignacian levels that it covers, but made the cave inaccessible for several millennia. Finally, the geomorphological study allows a very precise reflection on the organisation of space, access and movement of the populations inside the cave during the recent Middle Magdalenian.The cave also provides information on the hydrosedimentary dynamics and paleoclimatic conditions on the scale of the Arize valley. The phenomena observed inside the cave have been recorded outside in a degraded way, but correlation hypotheses remain possible between the recordings in the cave and in the Arize valley. The Mas d'Azil cave is therefore a very high-resolution recorder of hydrosedimentary responses resulting from climatic fluctuations, particularly during the last glacial cycle. Through the archaeological evidence inserted in its geomorphological context, this cave underlines the importance of the differential taphonomy of the archaeological remains and makes it possible to interpret them, from the scale of the site to that of the valleys of the northern Pyrenean foothills
Mereau, Anne-Laure. "Les dents animales perforées au Magdalénien : nouvelles perspectives fonctionnelles : étude de quatre sites pyrénéens : Isturitz, le Mas d'Azil, Arudy et Gourdan". Paris 1, 2012. http://www.theses.fr/2012PA010559.