59,310 research outputs found

    Les maréchaux en Savoie au bas Moyen Age

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    Ville et féodalité dans la Catalogne du bas Moyen-Age

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    L'Ă©lite du pouvoir a Murcie au Bas Moyen-Age.

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    Isotope geochemistry and petrogenesis of peralkaline Middle Miocene ignimbrites from central Sonora: relationship with continental break-up and the birth of the Gulf of California

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    Middle Miocene peralkaline ignimbrites constitute a specific geodynamic marker of the early stage of opening of the Gulf of California, preserved either in central Sonora or the Puertecitos area, in Baja California. Very uniform ages (12-12.5 Ma) obtained on these rocks show that this volcanic episode corresponds to a specific stage in the tectonic evolution of the proto-gulf area. Field observations and slightly different Sr and Nd isotopic signatures support eruptions from several small volume magma batches rather than from a large-volume caldera forming event. Isotopic ratios help to constrain the petrogenesis of the peralkaline liquids by fractional crystallization of transitional basalts in a shallow reservoir, with slight contamination by Precambrian upper crustal material. Less differentiated glomeroporphyritic icelandites erupted at about 11 Ma, mark an increase in the magma production rate and highlight an easier access to the surface, illustrating an advanced stage in the weakening of the continental crust. The tilting of the Middle Tertiary sequences results from a major change in the tectonic regime, from E-W extension giving rise to N-S grabens, to NNW-SSE strike-slip motion that can be related to the transfer of Baja California from North America to the Pacific plate. The location of peralkaline volcanism coincides with the southern edge of the Precambrian crust and the southernmost extension of the California slab window at 12.5 Ma

    Villars-les-Dombes – Rue Carnot

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    Identifiant de l'opĂ©ration archĂ©ologique : 9889 Date de l'opĂ©ration : 2008 (EX) Un diagnostic a Ă©tĂ© rĂ©alisĂ© dans l’emprise (1 500 m2 ) d’un futur immeuble d’habitation, situĂ© Ă  une cinquantaine de mĂštres au sud d’une butte remarquable, monument mĂ©diĂ©val dĂ©nommĂ© la Poype, (classĂ© au titre des Monuments Historiques en 1905), Ă©picentre du bourg castral mĂ©diĂ©val. La Poype Ă©tant siĂšge de pouvoir militaire et/ou religieux entre la fin du haut Moyen Age et le bas Moyen Age, il s’agissait d’identifi..

    Villars-les-Dombes – Rue Carnot

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    Identifiant de l'opĂ©ration archĂ©ologique : 9889 Date de l'opĂ©ration : 2008 (EX) Un diagnostic a Ă©tĂ© rĂ©alisĂ© dans l’emprise (1 500 m2 ) d’un futur immeuble d’habitation, situĂ© Ă  une cinquantaine de mĂštres au sud d’une butte remarquable, monument mĂ©diĂ©val dĂ©nommĂ© la Poype, (classĂ© au titre des Monuments Historiques en 1905), Ă©picentre du bourg castral mĂ©diĂ©val. La Poype Ă©tant siĂšge de pouvoir militaire et/ou religieux entre la fin du haut Moyen Age et le bas Moyen Age, il s’agissait d’identifi..

    Changes to commercial topography in late medieval Brussels

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    In this essay I will focus on changes to the commercial topography of late medieval Brussels and its correlation with urban development. Since the work of Henri Pirenne, trade has been considered as an essential factor in the growth of late medieval towns. As a result commercial activities have left traces in urban space. Market places and guild halls are well known examples

    Revolt and the Manipulation of Sacral and Private Space in 12th-Century Laon and Bruges

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