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Academic literature on the topic 'Points chauds (géologie) – Pacifique (océan ; sud)'
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Dissertations / Theses on the topic "Points chauds (géologie) – Pacifique (océan ; sud)"
Binard, Nicolas. "Les points chauds de la société, des Australes et de Pitcairn (Pacifique Sud) : approche volcanologique et pétrologique." Brest, 1991. http://www.theses.fr/1991BRES2050.
Full textLe, Faouder Antoine. "Caractérisation géochimique (déséquilibres 230Th/238U, isotopes Sr, Nd et Pb, éléments en traces) du volcanisme de dorsale en contexte d'interaction point chaud dorsale : Cas des bassins marginaux du Sud Ouest Pacifique et de la dorsale Centrale Indienne." Brest, 2006. http://www.theses.fr/2006BRES2039.
Full textStudying U series disequilibria in young lavas (<10kyr) is a powerful tool for understanding magma genesis and transfer such as time constraints of melt ascent or mantle porosity. Combined trace element geochemistry, isotope composition and U series data are able to indicate source heterogeneity due to the possible input of plume-derived enriched material. Input of additional mantle material can be carried out under two forms : melt or solid transport state. A major constrain to decipher between these two mechanisms is the duration of transport. Thus, U series disequilibria can provide information about the rate of the transfer process and therefore the transport mechanism of the process. The study presented here (on lavas from the North Fiji and Lau basins and the Central Indian Ridge) is probably one of the first to constrain ridge hotspot interaction using U series disequilibria and accentuates the peculiar interest of this method
Adam, Claudia. "Signature topographique et gravimétrique des panaches du manteau dans le Pacifique." Phd thesis, Institut de physique du globe de paris - IPGP, 2003. http://tel.archives-ouvertes.fr/tel-00350037.
Full textFontaine, Fabrice R. "Anisotropie et atténuation sismique en domaine océanique : application aux panaches mantelliques de la Polynésie française et des Galapagos." Montpellier 2, 2005. http://www.theses.fr/2005MON20002.
Full textJanin, Myriam. "Le plateau Amsterdam-St. Paul : caractérisation du point chaud éponyme et évolution de son interaction avec la dorsale Sud-est Indienne." Brest, 2010. https://tel.archives-ouvertes.fr/tel-00592036.
Full textThe Amsterdam-St Paul plateau (ASP) is an oceanic plateau built from the interaction between ASP hotspot and the Southeast Indian ridge. P volcanic chain, called the chain of the dead Poets (CDP), lies to its northward and related to the hotspot intraplate activity. Their study reveals that ASP plume composition comes from oceanic crust and pelagic sediments recycled in the mantle through a 1,5Ga subduction process, ASP plume activity is pulsatile and occurs preferentially on weakness zones. The CDP construction results thus from (1) the plume pulses and (2) the diffuse divergent boundary between the Capricorn and Australian plates. K-Ar datings reveal that this volcanic chain is made of two generations of seamounts: (1) an old one, of about 9Ma and made of large edifices which had probably a sub-aerial period and (2) a young one, younger than 2Ma, and made of small edifices related to some pounded plume pulse material. In addition, ASP plume has an own motion of about 1-2 cm/yr to the south-west. The ASP plateau lavas compositions (major and trace elements and Sr-Nd-Pb-Hf isotopes) show en important variability and reveal that the underlying mantle is heterogeneous. It is made of a depleted mantle with lower continental crust strips in the form of garnet-plagioclase granulites, probably delaminated during the Gondwana breakup. The lower continental crust s one of the hypotheses for DUPAL anomaly origin and our data support this assumption
Machado, Pessanha Ivo Bruno. "Évolution temporelle et spatiale du sytème d’interaction entre le point chaud de Tristan de Cunha et la Dorsale de l’Atlantique Sud." Brest, 2011. http://www.theses.fr/2011BRES2016.
Full textIn this work we have studied the space and time evolution of the Tristan hotspot and south Mid-Atlantic Ridge interaction system. The Tristan hotspot and its associated bathymetrical features (i. E. Walvis Ridge in the African plate and Rio Grande Rise in the South American plate) are one of the most significant features of the South Atlantic Ocean. However, this system is not as well studied as the systems in the North Atlantic (e. G. Azores and Iceland), and their origin and evolution is an open subject. Data compilation of the available surveys from the National Geophysical Data Center (NGDC) and satellite-derived bathymetry were treated to generate a Digital Elevation Model (DEM) for the entire South Atlantic Ocean. Satellite-derived free-air anomaly data and sediment thickness data were used to calculate the mantle Bouguer anomaly (MBA) and digital isochrons of the ocean floor were used to calculate the residual mantle Bouguer anomaly (RMBA), residual bathymetry and new poles for the South America and Africa relative plate motions. Satellite-derived geoid data and the Earth Gravitational Model - EGM2008 were used for the separation of the different components in the geoid data with the calculation of filters using different levels and degree of spherical harmonics. From kinematics reconstructions based on new rotation poles calculated in this work and using the most accepted hypothesis for the current position of the hotspot, as the volcanic island of Tristan da Cunha, the chronology of the emplacement of the volcanic structures could be detailed
Le, Saout Morgane. "Interaction dorsale-point chaud : relations entre les processus tectoniques et magmatiques à l'axe de la dorsale Est Pacifique, 16°N." Thesis, Brest, 2015. http://www.theses.fr/2015BRES0019/document.
Full textThe 16°N segment of the East Pacific Rise (EPR) is the most over-inflated and shallowest of this fast -spreading ridge, in relation with an important magma flux due to the proximity of the Mathematician hotspot. The goal of this thesis is to analyze in detail the magmatic and tectonic processes along this segment in regards to the influence of the hotspot. The study of these processes is based on a morpho-structural and chronological analysis of the segment between 15°36.N and 15°53.N using bathymetric data (1,10 and 40 m resolution) and Nautile dive photos and videos of the French PARISUB (.PAnach Ridge SUBmerssible.) cruise. The characterization of the faults and fissures geometry (e.g., vertical throw, dip, length, depth, width) and their orientation reveled that tectonic processes occur more than 750 m of the ridge axis. Lateral and abyssal grabens formed by fault, less developed than in other EPR segments would be the consequence of a warmer and thinner lithosphere. At the axis, the existence of two parallel and contiguous Axial Summit Troughs (ASTs) over a distance of about 20 km and above a wide magma lens, indicate a wide zone of diking and thus a poor localization of magmatic processes. This poor localization, and the highly segmented and global “en echelon” shift of the ASTs that progressively accommodate the bow shape of the axial dome in the direction of the hotspot, revealed the importance of the Mathematician hotspot influences on spreading processes. This hotspot also influences, although indirectly lava flows morphologies.Indeed, it is at the origin of the formation of a wide sub-horizontal plateau that results in the formation of inflated sheet and pillow flows. That flows covering about one third of the plateau allows us to develop theoretical and conceptual models to investigate lava flow dynamics. Models revealed that inflated sheet and pillow flows may emplace during the same long-live (few hours to 20 days) eruption, with sheet flows erupted at the end