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Registros recuperados: 38 | |
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Bougault, Henri; Joron, Jean-louis; Treuil, Michel. |
.-Alkali metals prove to be very sensitive to alteration process even if this process is moderate. It is very difficult to use these elements to trace magmatic processes since their concentration may Vary within an homogeneous "unaltered" unit. From all the basaltic units investigated, a classification of "low partition coefficient" elements is presented (Sc, Ti, V, Y, Zr, Nb, La-Tb , Hf, Ta, Th) . The incompatible elements ratios (Y/Tb, Zr/Hf, Nb/Ta) are constant in the samples studied and are nearly equal to the same ratios in chondrites. This is consistent with the existence of an homogeneous primordial mantle at the scale of the North Atlantic, compatible with a chondritic composition of the earth. [NOT CONTROLLED OCR] |
Tipo: Text |
Palavras-chave: Histoire Ifremer. |
Ano: 1979 |
URL: http://archimer.ifremer.fr/doc/1979/publication-5253.pdf |
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Bougault, Henri; Cande, S; Mills, W; Curtis, D; Neuser, R; Christie, D; Rideout, M; Etoubleau, Joel; Drake, N; Brannon, J; Weaver, B; Echols, D; Clark, M; Khan, Mj; Hill, I. |
Tipo: Text |
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Ano: 1983 |
URL: http://archimer.ifremer.fr/doc/00311/42189/41490.pdf |
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Bougault, Henri; Appriou, P; Bienvenu, P; Cambon, Pierre; Charlou, Jean-luc; Collette, B; Donval, Jean-pierre; Dosso, Laure; Floch, G; Fouquet, Yves. |
Tipo: Text |
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Ano: 1990 |
URL: http://archimer.ifremer.fr/doc/00070/18105/15653.pdf |
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Bougault, Henri; Saget, Philippe. |
Amas sulfurés hydrothermaux, nodules et encroûtements ferromanganésifères constituent en l’état des connaissances les trois ressources minérales potentielles des « grands fonds » marins. L’évolution du contexte international pour l’accès aux matières premières depuis quelques années conduit naturellement à porter une attention à ces ressources potentielles sous-marines. Bien que les encroûtements ferromanganésifères puissent présenter la plus grande valeur en métal contenu [Ifremer, 2011], principalement en raison de leur concentration en cobalt, l’étude de ces encroûtements et de leur contexte n’ont pas fait l’objet, en France, d’autant d’investigations que les nodules de manganèse ou les amas sulfurés hydrothermaux. On se propose de résumer les... |
Tipo: Text |
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Ano: 2011 |
URL: http://archimer.ifremer.fr/doc/00069/18029/15560.pdf |
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Bougault, Henri; Treuil, M.; Joron, J.l.. |
From a study of first-transition series trace elements and low-partition-coefficient trace elements or so-called hygromagmatophyle elements (Treuil and Varet, 1973; Treuil and Joron, 1976), we will try to define the relative importance of the three fundamental parameters- mantle source composition, extent of partial melting, and crystal fractionation-which bear on the formation of basalts recovered during Leg 45.We relate the presented data to the results of shipboard study (Chapters 7 and 8, this volume) and then give a tentative interpretation, taking into account our present knowledge of the behavior of trace elements during magmatic processes of FAMOUS and Leg 37 results. [NOT CONTROLLED OCR] |
Tipo: Text |
Palavras-chave: Histoire Ifremer. |
Ano: 1978 |
URL: http://archimer.ifremer.fr/doc/1978/publication-5204.pdf |
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Wood, D.a.; Varet, J.; Bougault, Henri; Corre, O.; Joron, J.l.; Treuil, M.; Bizouard, H.; Norry, M.j.; Hawkesworth, C.j.; Roddick, J.c.. |
Whole-rock geochemical data were obtained for 178 samples selected from the petrologically freshest parts of most of the flow units recovered from the nine holes. These data include 170 major element analyses (XRF) and 174 trace-element analyses (XRF and INAA). We include representative microprobe analyses of the primary minerals and fresh basaltic glasses (where present) in 40 selected samples. We also present 87Sr/88Sr ratios for 14 samples selected from the holes at 63"N. These analytical data, together with petrographic data obtained from the study of some 500 thin sections, have enabled us to establish a detailed lithostratigraphy for each basement section. [NOT CONTROLLED OCR] |
Tipo: Text |
Palavras-chave: Histoire Ifremer. |
Ano: 1979 |
URL: http://archimer.ifremer.fr/doc/1979/publication-5238.pdf |
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Bougault, Henri; Appriou, P; Birolleau, A; Charlou, Jean-luc; Crane, K; Etoubleau, Joel; Fouquet, Yves; Gente, P; Harmegnies, Francois; Landure, Jean-yves; Le Noac'H, A; Pelle, Henri; Sichler, Bertrand; Voisset, Michel; Watremez, Pierre; Vaslet, N; Jean Baptiste, P. |
Tipo: Text |
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Ano: 1990 |
URL: http://archimer.ifremer.fr/doc/00070/18104/15652.pdf |
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Bougault, Henri; Joron, J.l.; Treuil, M.. |
Large-scale heterogeneities in the mantle are investigated through trace elements measured in oceanic basalts from different locations in the Atlantic and Pacific oceans.The study relies upon the physico-chemical properties of the elements and their classification according to their partition coefficients. High partition coefficient elements (Co, Ni; Cr) have concentrations in peridotite that are not sensitive to solidliquid equilibrium (partial melting); the mantle should therefore be homogeneous with respect to these elements.The ratios of elements that have equal or very similar low partition coefficients (Y/Tb, Zr/Hf and Nb/Ta) are constant in all samples studied, despite their large concentration range.These ratios are equal to chondritic ratios and... |
Tipo: Text |
Palavras-chave: Histoire Ifremer. |
Ano: 1980 |
URL: http://archimer.ifremer.fr/doc/1980/publication-5281.pdf |
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Auzende, Jean Marie; Boespflug, X; Bougault, Henri; Dosso, Laure; Foucher, Jean-paul; Joron, J-l; Ruellan, Etienne; Sibuet, Jean-claude. |
Three cruises (POP 1, SEAPSO 3 and SEAPSO 4) carried out during the "Tour du Monde" of the R.V. Jean Charcot allow us to obtain new structural and geochemical data for the Okinawa, North Fiji and Lau basins. Taken together, the structural and geochemical data illustrate a difference in evolution stages of these sites. The less evolved stage is represented by the Okinawa basin, where accretion is evidence only by volcanic intrusion into a thinned continental crust. The most evolved stage is illustrated in the North Fiji basin, where the present-day accretion can be directly compared to the East Pacific Ridge. The Lau basin displays an intermediate stage with a complex system of accretionary ridges. This difference in the evolution stage is translated in the... |
Tipo: Text |
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Ano: 1990 |
URL: http://archimer.ifremer.fr/doc/00268/37893/35974.pdf |
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Bougault, Henri; Maury, R.c.; El Azzouzi, M.; Joron, J.l.; Cotten, J.; Treuil, M.. |
This chapter presents major oxide and trace element determinations of igneous whole-rock compositions from sites drilled during Leg 60 and electron microprobe mineral and glass analyses of samples from Sites 454 and 458. Interarc basin basalts from the Mariana Trough (Sites 454 and 456) are similar in all respects to depleted mid-ocean ridge basalts. Basaltic andesites and andesites from Site 458 (Mariana fore-arc region) are more depleted than mid-ocean ridge basalts and show different geochemical behavior for Zr-, Hf, and Ti when compared on an extended Coryell- Masuda plot. [NOT CONTROLLED OCR] |
Tipo: Text |
Palavras-chave: Histoire Ifremer. |
Ano: 1981 |
URL: http://archimer.ifremer.fr/doc/1981/publication-5308.pdf |
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Pignet, G.; Martin, G.; Bougault, Henri. |
Les eaux superficielles sont atteintes de plus en plus gravement par la pollution industrielle, alors que les besoins en eau pure augmentent. C'est pourquoi on est amené à utiliser pour la consommation des eaux de qualités variables contenant en particulier un certain nombre de micropolluants. Les essais présentés ici ont pour but de tester une méthode originale d'élimination de différents cations métalliques bivalents. [OCR NON CONTRÔLE] |
Tipo: Text |
Palavras-chave: Histoire Ifremer. |
Ano: 1979 |
URL: http://archimer.ifremer.fr/doc/1979/publication-5396.pdf |
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Vlastelic, Ivan; Dosso, Laure; Bougault, Henri; Aslanian, Daniel; Geli, Louis; Etoubleau, Joel; Bohn, Marcel; Joron, Jl; Bollinger, C. |
Axial bathymetry, major/trace elements, and isotopes suggest:that the Pacific-Antarctic Ridge (PAR) between 56 degrees S and 66 degrees S is devoid of any hotspot influence. PAR (56-66 degrees 5) samples have in-average lower Sr-87/Sr-86 and Nd-143/Nd-144 and higher Pb-206/(204)pb than northern Pacific midocean ridge basalts (MORB), and also than MORE from the other oceans. The high variability of Pb isotopic ratios (compared to Sr and Nd) can be due to either a;general high mu (HIMU) (high U/Pb) affinity of the southern Pacific upper mantle or to a mantle event first recorded in time by Pb isotopes. Compiling the results of this study with those from the PAR between 53 degrees S and 57 degrees S gives a continuous view of mantle characteristics from south... |
Tipo: Text |
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Ano: 2000 |
URL: https://archimer.ifremer.fr/doc/00000/10578/9396.pdf |
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Bougault, Henri. |
From a study of the first transition series elements we will try to define the pattern of fractional crystallization and partial melting. Results are discussed hole by hole in connection with lithological description and major element analysis. and element by element in term of fractional crystallization or partial melting using their partition coefficients. [NOT CONTROLLED OCR] |
Tipo: Text |
Palavras-chave: Histoire Ifremer. |
Ano: 1977 |
URL: http://archimer.ifremer.fr/doc/1977/publication-4992.pdf |
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Bougault, Henri; Treuil, Michel. |
The MAPCO cruise of the R.V. Jean-Charcot (October-November, 1979) sampled zero-age basalts along the Mid Atlantic Ridge from the Azores triple junction to 24°N. Preliminary shipboard geochemical analyses together with previOusly collected data show that hygromagmaphile elements are not randomly distributed along the ridge. North from Hayes transform, the chondrite normalised diagrams of these elements show flat to enriched distributions for the most hygromagmaphile elements. South from this transform, these diagrams are systematically depleted for the most hygromagmaphile elements. These data are interpreted in terms of regional upper mantle heterogeneity. [NOT CONTROLLED OCR] |
Tipo: Text |
Palavras-chave: Histoire Ifremer. |
Ano: 1980 |
URL: http://archimer.ifremer.fr/doc/1980/publication-5417.pdf |
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Registros recuperados: 38 | |
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