Éditeur(s) : HAL CCSD
Résumé : International audience
The "South-Dominica" archaeological mission of the French ministry of foreign affairs has started work in 2005. Designed to enlighten the archaeological terra incognita dominicana, this research has essentially been dedicated to the early ceramic occupation of the island. Our work has been based on the analysis of the few collections already existing, on systematic survey campaigns and on an important test pit program. This lecture will be concentrating on the presentation of the Soufrière site excavation. The Soufriere site, found in the seventies, is composed of an important early cedrosan saladoid occupation covered by volcanic deposits. The data obtained during this excavation, associated with other results of the "South Dominica" archaeological mission, incites us to think about a revision of the territories associated to the complexes in the Lesser Antilles.
La mission archéologique "Sud-Dominique" du ministère français des affaires étrangères a débuté ses travaux en 2005. Destinées à en finir avec la terra incognita dominicana archéologique, ces recherches sont essentiellement consacrées à l'étude du premier peuplement agro-céramique de l'île. Le travail de la mission archéologique repose sur l'étude de séries anciennes, des campagnes de prospections systématiques et un important programme de sondages. Notre présentation se concentrera sur la fouille que nous avons menée du site de Soufrière dans le sud de la Dominique. Ce gisement identifié dans les années 1970 correspond à une importante occupation saladoïde cedrosane ancienne qui a été recouverte par des dépôts volcaniques. Les données obtenues lors de cette fouille associées à l'ensemble des résultats obtenus en 3 années par la mission archéologique Sud-Dominique nous incitent à nous interroger sur la nécessité d'une révision des territoires associés à la notion de complexe dans les Petites Antilles.
XXII Conference of the International Association of Caribbean Archaeology
Kingston, Jamaica

Droits : info:eu-repo/semantics/OpenAccess
hal-00961335
https://hal.univ-antilles.fr/hal-00961335
https://hal.univ-antilles.fr/hal-00961335/document
https://hal.univ-antilles.fr/hal-00961335/file/soufriA_repaperfinal.pdf

Éditeur(s) : HAL CCSD Museum Nationale d'Histoire Naturelle Paris
Résumé : International audience
ISSN: 1280-9551

hal-01084016
https://hal-agroparistech.archives-ouvertes.fr/hal-01084016
DOI : 10.5252/z2009n4a8

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : International audience
Expeditions 304 and 305 of the Integrated Ocean Drilling Program cored and logged a 1.4 km section of the domal core of Atlantis Massif. Postdrilling research results summarized here constrain the structure and lithology of the Central Dome of this oceanic core complex. The dominantly gabbroic sequence recovered contrasts with predrilling predictions; application of the ground truth in subsequent geophysical processing has produced self-consistent models for the Central Dome. The presence of many thin interfingered petrologic units indicates that the intrusions forming the domal core were emplaced over a minimum of 100-220 kyr, and not as a single magma pulse. Isotopic and mineralogical alteration is intense in the upper 100 m but decreases in intensity with depth. Below 800 m, alteration is restricted to narrow zones surrounding faults, veins, igneous contacts, and to an interval of locally intense serpentinization in olivine-rich troctolite. Hydration of the lithosphere occurred over the complete range of temperature conditions from granulite to zeolite facies, but was predominantly in the amphibolite and greenschist range. Deformation of the sequence was remarkably localized, despite paleomagnetic indications that the dome has undergone at least 45 degrees rotation, presumably during unroofing via detachment faulting. Both the deformation pattern and the lithology contrast with what is known from seafloor studies on the adjacent Southern Ridge of the massif. There, the detachment capping the domal core deformed a 100 m thick zone and serpentinized peridotite comprises similar to 70% of recovered samples. We develop a working model of the evolution of Atlantis Massif over the past 2 Myr, outlining several stages that could explain the observed similarities and differences between the Central Dome and the Southern Ridge.
ISSN: 0148-0227

hal-00617528
https://hal.archives-ouvertes.fr/hal-00617528
https://hal.archives-ouvertes.fr/hal-00617528/document
https://hal.archives-ouvertes.fr/hal-00617528/file/2010JB007931.pdf
DOI : 10.1029/2010JB007931