Éditeur(s) : HAL CCSD Springer Verlag (Germany) Springer Verlag
Résumé : International audience
Peridotite xenoliths erupted by alkali basaltic volcanoes in the western Pannonian Basin can be divided into two fundamentally contrasting groups. Geochemical characteristics of the abundant protogranular, porphyroclastic and equigranular nodules suggest that these samples originate from an old consolidated and moderately depleted lithospheric mantle domain. In contrast, the geochemical features of the worldwide rare, but in the Pannonian Basin relatively abundant, poikilitic xenoliths attest to a more complex evolution. It has been argued that the origin of the peculiar texture and chemistry may be intimately linked to melt/rock reactions at successively decreasing liquid volumes in a porous melt flow system. The most likely site where such reactions can take place is the asthenosphere-lithosphere boundary. In this context, poikilitic xenoliths may provide petrological and geochemical evidence for reactions between magmatic liquids issued from the uprising asthenosphere and the solid mantle rocks of the lithosphere. These reactions are important agents of the thermal erosion of the lithosphere; thus, they could have considerably contributed to the thinning of the lithosphere in the Pannonian region. We suggest that in the Pannonian Basin, there could be a strong relation between the unusual abundance of poikilitic mantle xenoliths and the strongly eroded lithosphere.
ISSN: 0010-7999

hal-01107421
https://hal.archives-ouvertes.fr/hal-01107421
DOI : 10.1007/s00410-014-1054-y

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : International audience
A dense network of seismic stations has been deployed on the Kaapvaal craton (South Africa) to investigate the upper mantle seismic structures. In order to bring independent petrophysical constraints, we analyze a direct sampling of the cratonic upper mantle and determine the seismic properties of 48 mantle nodules brought up to the Earth's surface by kimberlite eruptions. Seismic properties of these nodules are calculated from the olivine and pyroxene crystal preferred orientations and the single crystal elastic constants. Despite variations in the nodules compositions, microstructures and crystallographic preferred orientations, seismic anisotropy is rather homogeneous throughout the craton. Mean S-wave anisotropy is weak (2.64 %), which is compatible with the small measured SKS wave splitting (mean delay time of 0.62 s).
ISSN: 0094-8276

hal-01389119
http://hal.univ-reunion.fr/hal-01389119
http://hal.univ-reunion.fr/hal-01389119/document
http://hal.univ-reunion.fr/hal-01389119/file/BenIsmail_GRL_kaapvaal_GRL2001.pdf
DOI : 10.1029/2000GL012419

Éditeur(s) : Archives départementales de la Martinique
21Fi5/5
Rue Victor Hugo (Saint-Pierre)
Saint-Pierre

Droits : Reproduction soumise à autorisation
http://www.patrimoines-martinique.org/ark:/35569/a011273060476UeAvQE

Éditeur(s) : Archives départementales de la Martinique
2Fi758
Jardin des plantes (Saint-Pierre)
Saint-Pierre

Droits : Reproduction soumise à autorisation
http://www.patrimoines-martinique.org/ark:/35569/a011273060198MvMBXx

Éditeur(s) : HAL CCSD Universidad de Barcelona
Résumé : Tens of Surtseyan tuff cones are exposed in the Rio Coichel valley, between Nireguao and Estancia Bano Nuevo (Southern Chilean Andes). The Early Cretaceous products of the submarine eruptions rest on, or are interbedded with, shallow marine sandstones of the Hauterivian-early Aptian Apeleg Formation. The Early Cretaceous rocks typically contain large amphibole phenocrysts, clinopyroxene and plagioclase, and have compositions that range from relatively primitive basalts to andesites. The basalts are slightly enriched in LREE and incompatible trace elements. They have low Ti-contents and negative anomalies in Nb and Ta, characteristic of subduction-related magmas. Centimetre-sized amphibole megacrysts and an amphibole-bearing clinopyroxenite xenolith have been found in one of the tuff cones located near Estancia Bano Nuevo. The amphibole megacrysts are pargasite (low Si and Ti, high Mg). The xenolith has diopsidic clinopyroxene with abundant inclusions, and pargasite veins enclosing smaller clinopyroxene neoblasts. Geochemical data show that the megacrysts and the xenolith have the same origin and correspond to underplated igneous bodies crystallized at high pressure.
ISSN: 1695-6133

hal-00512829
https://hal.archives-ouvertes.fr/hal-00512829
DOI : 10.1344/105.000001530

Éditeur(s) : Archives départementales de la Martinique
2Fi702
Montagne Pelée
Saint-Pierre

Droits : Reproduction soumise à autorisation
http://www.patrimoines-martinique.org/ark:/35569/a011273060198RTAWOc

Éditeur(s) : Archives départementales de la Martinique
2Fi1388
Mouillage (Saint-Pierre)
Saint-Pierre

Droits : Reproduction soumise à autorisation
http://www.patrimoines-martinique.org/ark:/35569/a011273060192UlviDS

Éditeur(s) : Archives départementales de la Martinique
2Fi1345
Saint-Pierre

Droits : Reproduction soumise à autorisation
http://www.patrimoines-martinique.org/ark:/35569/a011273060195qzVZoo

Éditeur(s) : Archives départementales de la Martinique
2Fi419
Pont de pierre (Saint-Pierre)
Rivière Roxelane (Saint-Pierre)
Centre (Saint-Pierre)
Saint-Pierre
Fort (Saint-Pierre)

Droits : Reproduction soumise à autorisation
http://www.patrimoines-martinique.org/ark:/35569/a011273060184xrwaS3

Éditeur(s) : Bibliothèque Schoelcher
80134550
Martinique
Saint-Pierre
Montagne Pelée

Droits : Reproduction soumise à autorisation de la Bibliothèque Schoelcher
http://www.patrimoines-martinique.org/ark:/35569/a011416928916FAxjfW

Éditeur(s) : HAL CCSD Elsevier
Résumé : We present new analytical data from lavas and associated rocks dredged and/or drilled from the South Fiji Basin, Northland Plateau, Colville Ridge and Havre Trough. These results provide much-needed ground truth about the geology, age and tectonic evolution of the Cenozoic submarine ridges and basins between the active intraoceanic Tonga–Kermadec arc, and rifted continental borderlands of New Zealand, the Norfolk Ridge and New Caledonia. Key results from this study include: (1) Ar–Ar dates on Minerva Abyssal Plain oceanic crust suggest that the ages of magnetic anomalies in the South Fiji Basin have been overestimated by earlier workers; (2) subduction-related lavas are widespread across the region, are not presently organised into arc-like chains, and cluster in the age range 22–18 Ma (Early Miocene); (3) the oldest subduction-related lavas occur in the western part of the region (32–26 Ma: Norfolk and Three Kings Ridge); (4) shoshonites, interpreted as rifted arc lavas, were erupted in a narrow 20–21 Ma interval over a wide area. Put together, these results indicate high magmatic flux and large and rapid horizontal tectonic translations and basin opening from 18–23 Ma in the region immediately north of New Zealand. We explain the Miocene tectonomagmatic development of the region by a model of rapid rollback of a single, east-facing Pacific arc–trench system that became established after Northland Allochthon emplacement. Critical testing of this, versus other, tectonic models must await drilling and dating of thus-far unsampled Kupe Abyssal Plain crust.
ISSN: 0025-3227

hal-00405803
https://hal.archives-ouvertes.fr/hal-00405803
DOI : 10.1016/j.margeo.2006.10.033

Éditeur(s) : Archives départementales de la Martinique
2Fi738
Saint-Pierre

Droits : Reproduction soumise à autorisation
http://www.patrimoines-martinique.org/ark:/35569/a011273060197yZz3Sf

Éditeur(s) : Archives départementales de la Martinique
21Fi5/8
Saint-Pierre

Droits : Reproduction soumise à autorisation
http://www.patrimoines-martinique.org/ark:/35569/a011273060476btcNui

Éditeur(s) : HAL CCSD
Résumé : International audience
Earthquake, volcanic eruption, cyclone, flood, tsunami, the Caribbean are particularly vulnerable to many natural hazards. Citizen Education to hazard mitigation is much more important in French West Indies than in Paris. With national, curriculum, evaluation and textbooks, how science education in French West Indies manage the challenge to take account this particularity of our territories? Based on this example and others, the aim of this communication is to present a science education theoretical background focus on contexts studies. During science teaching, learning effects due to different context like social, cultural or language could be described as contextual effects. But others micro-didactic effects of contexts could also be identified as linked with specificity of natural environment. These effects manifest a strain between a goal of teaching or learning and its implementation, when this stain is due in the educational process in different contexts involved.To ensure the quality of education, reference and quantify the effects of educational context seems to be necessary. it should be interested in the process leading to the emergence of these contexts. We propose a simplified model of these processes initially described as meetings of mechanisms operating within a network of transposition of designs. Then we question these processes by degree or forms of contextualization (low to high) and crossed these two approaches, giving an initial typology of contextualisation process. It then emerges the idea that these processes are constrained by resistances. We retain the following three: epistemological, social and educational. As these constraints are expressed in different ways according to disciplines, the data suggest the existence of disciplinary contextualization profiles. All these three approaches (network implementation, degree of contextualization, disciplinary profiles) are three tools for analyzing contextual phenomena which remain to test the robustness and operational character for the training analysis context.
Biennial Conference of Caribbean Academy of Sciences
Barbados, Barbados

hal-01539482
https://hal.univ-antilles.fr/hal-01539482

Éditeur(s) : Bibliothèque Schoelcher
Di-I 80151092
Morne-Rouge (Le)
Saint-Pierre
Montagne Pelée

Droits : Reproduction soumise à autorisation
http://www.patrimoines-martinique.org/ark:/35569/a011414681977aCbJFn

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
Island arc picrites and boninites are magnesian magmatic rocks believed to be generated by high degrees of melting of depleted mantle sources fluxed by subduction-derived, volatile-rich components. These magmas can be probes of both the mantle wedge protoliths and subduction components, but are rare among other, usually more evolved, types of arc lavas. Furthermore, many arc picrites and boninites show evidence for late-stage differentiation prior to or during eruption, masking their primary, mantle-derived geochemical signatures. We report textural and chemical data on spinel-hosted melt inclusions of mantle origin in amphibole-bearing websterite veins cross-cutting spinel harzburgite xenoliths from the active andesitic Avacha volcano (south Kamchatka, Russia). The data are used to constrain the composition and origin of melts that formed the websterite veins in the sub-arc lithospheric mantle. The melt inclusions typically contain euhedral orthopyroxene and clinopyroxene and occasionally minor amphibole in silicate glass. The melt inclusions were homogenized using heating stages and gas-mixing furnaces. The homogenized glasses range from subalkaline primitive silica-rich picrite and high-Ca boninite (>15 wt % MgO, 48–54 wt % SiO2) to rhyolite. High-Ca boninite glasses have moderate volatile and low heavy rare earth element contents and elevated Cs, Rb, Ba, U, Sr, and Li abundances, with extremely high U/Th. In turn, the glasses display no negative spikes in the high field strength elements Nb, Ta, Zr, Hf, and Ti. We show that the silica-rich picrite and high-Ca boninite liquids in this study formed by high degrees of melting (>25%), at volatile under-saturation, of hybrid melt-depleted but silica-rich mantle sources at ≥1·5 GPa. The hybrid sources formed in two stages: first, by extraction of ∼15% melt from the convecting mantle to form a refractory protolith, which was subsequently enriched in silica via interaction with subduction-derived components prior to or during remelting in the mantle wedge. The subduction-derived components were enriched in fluid-mobile elements and probably oxidized. Overall, our results suggest that silica-rich picrites and high-Ca boninites can be primary melts in mature subduction zones and differentiate within the mantle wedge and the deep arc crust to form more evolved andesite magmas.
ISSN: 0022-3530

hal-01553676
https://hal.archives-ouvertes.fr/hal-01553676
DOI : 10.1093/petrology/egw066

Éditeur(s) : Archives départementales de la Martinique
21Fi3/42
Saint-Pierre

Droits : Reproduction soumise à autorisation
http://www.patrimoines-martinique.org/ark:/35569/a011273060476aPmHIq

Éditeur(s) : Archives départementales de la Martinique
21Fi3/35
Place Bertin (Saint-Pierre)
Saint-Pierre

Droits : Reproduction soumise à autorisation
http://www.patrimoines-martinique.org/ark:/35569/a011273060476CxfNrr

Éditeur(s) : Archives départementales de la Martinique
2Fi52
Saint-Pierre

Droits : Reproduction soumise à autorisation
http://www.patrimoines-martinique.org/ark:/35569/a011273060199kmAqk2

Éditeur(s) : Archives départementales de la Martinique
2Fi1711
Rivière Roxelane (Saint-Pierre)
Saint-Pierre

Droits : Reproduction soumise à autorisation
http://www.patrimoines-martinique.org/ark:/35569/a011273060198vOrUzj