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  • 1
    ISSN: 1520-510X
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Acta neuropathologica 32 (1975), S. 169-172 
    ISSN: 1432-0533
    Keywords: Polyneuritis ; Myelin ; Peripheral Nerve ; Chronic Lymphoid Leukemia
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Summary A 75 years old man had a chronic lymphoid leukemia for 5 years. Within a period of three months he developed a polyneuritis. The biopsy of a peripheral nerve showed a large cellular infiltration by lymphocytes. The ultrastructural study shows in some Schwann cells disruption of the myelin. Their cytoplasm is invaded by a lymphocyte process as in Guillain-Barré. But in this case some of these invading lymphocytes show polygonal structures in their cytoplasm; that is sometimes seen in the proliferating cells of the chronic lymphoid leukemia.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Mineralium deposita 15 (1980), S. 201-210 
    ISSN: 1432-1866
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The SEM investigations on some chromite crystals show significant morphological differences between cumulate chromites (from stratiform complexes and from ophiolites) and chromites from podiform deposits (ophiolites). The later exhibit a rounded habit and abundant pits which are both the result of dissolution processes. Accordingly, the interpretation of the silicate inclusions within these chromites and the interpretration of the trace-elements distribution need great care. The nodules, a typical structure of the podiform chromites, are explained by a magmatic growth followed by a progressive recrystallization. The accessory chromites which define the mineral lineation in the tectonite peridotites from ophiolites have been deformed by processes of intracrystalline gliding, stretching and dissolution. In the harzburgites, the orthopyroxene has progressively exsolved at sub-solidus (symplektites) vermicular to massive chromite displaying euhedral forms. In the dunitic lenses, the idiomorphic chromites which are aligned parallel to the lineation may have also recrystallized in a solid state.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Mineralium deposita 21 (1986), S. 129-136 
    ISSN: 1432-1866
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Résumé Le gisement d'Alous (4 à 6 Mt à 0,8% Cu) est un exemple apparemment fort rare, de dépôt de cuivre dans un appareil ignimbritique. Celui dans lequel il est installé appartient à une formation volcanique post-orogénique de la fin du Précambrien. Les sulfures de cuivre (chalcocite, bornite avec accessoirement chalcopyrite et pyrite) et les minéraux accompagnateurs (chlorites, séricite, albite, épidote, quartz) ont cristallisé dans des pyromérides au cours du refroidissement de l'ignimbrite. La minéralisation cuprifère est localisée le long de failles radiales et l'on observe une diminution centrifuge des rapports Cu/Fe des sulfures et Mg/Fe des chlorites. Un modèle de circulations hydrothermales associées au volcanisme ignimbritique est proposé: le cuivre aurait été lessivé à partir des laves basiques sous-jacentes puis redéposé sous forme de sulfures le long des failles radiales au cours du refroidissement des ignimbrites.
    Notes: Abstract The Alous deposit (from 4 to 6 Mt at 0.8% Cu) is apparently a rare example of copper deposit in ignimbrite volcanos. The volcano from which it comes belongs to a post-orogenic volcanic formation of late Proterozoic age (Anti-Atlas, Morocco). The copper sulphides (chalcocite, bornite with accessory chalcopyrite and pyrite) and associated minerals (chlorites, sericite, albite, epidote, quartz) crystallized during the cooling of the ignimbrite and were included in pyromeride textures. The mineralization is distributed along radial faults and displays, outwards from the volcano center, a decrease of sulphides Cu/Fe ratio and chlorites Mg/Fe ratio. A model of small-scale hydrothermal circulations linked to the volcanic activity is proposed: copper was leached from the underlaying basic lavas then redeposited along radial faults during the ignimbrite cooling.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Mineralium deposita 16 (1981), S. 269-282 
    ISSN: 1432-1866
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Résumé Les orbicules de chromites, structures typiques des corps podiformes de chromite des ophiolites, sont décrites en détail. Elles correspondent à des concrétions magmatiques en milieu turbulent soumises en fin de cristallisation à un allongement et un cisaillement contemporains de la déformation plastique de l'olivine. Les autres types de minerai des corps podiformes sont affectés d'un plan de "pull-apart" marqué par des feuillets lenticulaires et parallèles à remplissage d'olivine. Ultérieurement, un réseau de diaclases à remplissage serpentineux se développera. Ces observations sont cohérentes avec l'hypothèse de la formation des corps podiformes dans des conduits magmatiques au sein des péridotites mantelliques.
    Notes: Abstract The chromite orbicules, a typical ore from chromite pods of ophiolites, are described. These are considered as magmatic concretions having suffered deformations at the end of the crystallization state, during the plastic deformation of olivine. Other ore textures display a pull-apart plane marked by lenticular olivine sheets. Later joint planes, with serpentine filling up, are developped. Our observations are in good agreement with the hypothesis of the generation of the chromite pods within magmatic pipes in the mantle peridotites.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Mineralium deposita 30 (1995), S. 211-224 
    ISSN: 1432-1866
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The Amesmessa gold prospect is located along a vertical N-S-trending crustal-scale ductile shear zone; stretching lineations are subhorizontal. This major shear zone is a Late Pan African dextral strike-slip fault of the Pharusian Belt of the Tuareg Shield (Algeria). The Amesmessa shear zone is asymmetric: strong thermal and deformational gradients are present along its western border where biotitic ultramylonites are in contact with a rigid Archean complex (In Ouzzal block), whereas there is a progressive gradation, through mylonite then protomylonite, to the Proterozoic gneiss of the Eastern block which displays co-axial Pan African structures. The Amesmessa shear zone is characterized by the presence of a felsic dike complex emplaced during shearing, and forming the most important parent material for ultramylonites. Basic magmas and carbonatites also intruded within the shear zone. The gold-rich quartz veins are located within the ultramylonitic western part of the shear zone. These N-S-trending laminated quartz veins formed during the late increments of shearing (plastic/brittle transition), by repeated syntectonic hydraulic fracturing along zones of rheological contrast parallel to foliation. The ore mineral association (pyrite, galena, native gold, sphalerite) crystallized in the deformed quartz matrix along late shear planes. Undeformed E-W trending banded quartz veins are present in the mylonitic eastern part of the shear zone; their gold content is low and no native gold has been observed. A strong hydrothermal alteration resulted in the development (along the walls of the N-S gold-bearing quartz veins) of a 5-m-wide carbonate-sericite-albite-pyrite secondary mineral association which implies an important CO2 supply and moderate temperature conditions. There is no alteration halo around the E-W quartz veins. Ultramylonites, hydrothermally altered rocks and quartz veins display similar REE patterns characterized by strong LREE enrichments. Shear-related fluids could be likely parental fluids for the Amesmessa gold mineralization and the associated hydrothermal alteration. Hydrothermal fluids were drawn into dilation zones and filled opening fractures along the main planar discontinuity of the most deformed rocks. The supply of CO2 may come from a deep-seated source as suggested by the presence of carbonatite dikes in the shear zones and the existence of CO2-H2O-rich fluid inclusions in quartz. The location of the gold-bearing quartz veins in the western part of the shear zone can be explained by the presence of strong thermal and rheological gradients.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Mineralium deposita 24 (1989), S. 123-123 
    ISSN: 1432-1866
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Intensive care medicine 25 (1999), S. 1169-1172 
    ISSN: 1432-1238
    Keywords: Key words Myoglobin ; Hemofiltration ; Clearance ; Removal ; Creatinine kinase ; Acute renal failure
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Abstract Myoglobin has a relatively high molecular weight of 17,000 Da and is poorly cleared by dialysis (diffusion). However, elimination of myoglobin might be enhanced by an epuration modality based on convection for solute clearances. We present a single case of myoglobin-induced renal failure (peak creatine kinase level: 313,500 IU/l) treated by continuous venovenous hemofiltration (CVVH). Our purpose was to evaluate the efficiency of such a modality using an ultrafiltration rate of 2 to 3 l/h for myoglobin removal and clearance. The hemofilter was a 0.9 m2 polyacrylonitrile (AN69) membrane Multiflow-100 (Hospal-Gambro, St-Leonard, Canada) and the blood flow rate was maintained at 150 ml/min by an AK-10 pump (Hospal-Gambro, St-Leonard, Canada). The ultrafiltration bag was placed 60 cm below the hemofilter and was free of pump control or suction device. Serum myoglobin concentration was 92,000 μg/l at CVVH initiation and dropped to 28,600 μg/l after 18 h of the continuous modality. The mean sieving coefficient for myoglobin was 0.6 during the first 9 h of therapy and this decreased to 0.4 during the following 7 h. Mean clearance of myoglobin was 22 ml/min, decreasing to 14 ml/min during corresponding periods, while the mean ultrafiltration rates were relatively stable at 2,153 ± 148 ml/h and 2,074 ± 85 ml/h, respectively. In contrast to myoglobin, the sieving coefficeint for urea, creatinine, and phosphorus remained stable at 1.0 during the first 16 h of CVVH. More than 700 mg of myoglobin were removed by CVVH during the entire treatment.¶In conclusion, considerable amounts of myoglobin can be removed by an extracorporeal modality allowing important convective fluxes and middle molecule clearances, such as CVVH at a rate of 2 to 3 l/h using an AN69 hemofilter. If myoglobin clearance had been maintained at 22 ml/min, 32 l of serum would have been cleared per day. However, the sieving coefficient of myoglobin decreased over time, probably as a consequence of protein coating and/or blood clotting of the hemofilter. Whereas myoglobin can be removed by CVVH, it remains unknown at this point if such a modality, applied early, can alter or shorten the course of myoglobinuric acute renal failure.
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1432-1238
    Keywords: Key words Hemofiltration ; Hemodiafiltration ; Folic acid ; Vitamin B6 ; Clearances ; Micronutrient
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Abstract Objective: To determine to what extent hydrosoluble vitamins are removed by continuous renal replacement therapy (CRRT); to evaluate clearances, removal rates, and evolution of serum concentrations of folic acid and pyridoxal-5′-phosphate (P-5′-P), the active moiety of vitamin B6 during CRRT. Design: A prospective, non-interventional, descriptive study on vitamin losses induced by CRRT. Setting: Medical and surgical intensive care units in a tertiary university-affiliated hospital. Patients: A total of ten critically ill patients in oligoanuric acute renal failure (five treated by continuous venovenous hemofiltration and five by continuous venovenous hemodiafiltration) with a mean effluent rate of 1801 ± 468 ml/h. Nutritional support was not modified and additional vitamin supplements were not provided during study periods. Measurements and results: Concentrations of folic acid and P-5′-P were determined daily during CRRT. Samples for folic acid, P-5′-P, urea, and creatinine were taken simultaneously from the blood at the dialyzer inlet and from the effluent, at CRRT initiation, and daily thereafter over an average of 3.4 ± 1.2 days. Samples were processed by immunochemiluminescence for folic acid and by radioenzymatic assay for P-5′-P determinations with normal ranges above 6.8 nmol/l and from 11.5 to 179.3 nmol/l, respectively. Marked decreases in serum folic acid and P-5′-P concentrations were noticed over time with mean daily reductions of 12.6 and 13.7 %. Serum folic acid concentrations decreased from 42.7 to 16.0 nmol/l and serum P-5′-P decreased from 14.4 to 5.0 nmol/l in the blood coming in to the dialyzer over the study period. Clearances and removal rates were determined from the effluent side. During CRRT, mean (± SEM) folic acid and P-5′-P clearances were 20.5 ± 6.3 ml/min (n = 34) and 13.2 ± 10.6 ml/min (n = 22), whereas mean urea clearance was 27.1 ± 5.1 ml/min (n = 26). Folic acid and P-5′-P removal rates were 27.0 ± 34.2 and 3.4 ± 2.0 nmol/h, corresponding to mean daily losses of nearly 650 and 80 nmol/day respectively. Conclusion: Significant losses of folic acid and P-5′-P (and most likely of other hydrosoluble vitamins) occur during CRRT. Considering that stores of most hydrosoluble vitamins are relatively low in critically ill patients, supplementation should be provided to patients treated similarly.
    Type of Medium: Electronic Resource
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  • 10
    ISSN: 1469-7610
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Medicine , Psychology
    Notes: Abstract Three subgroups of kindergarten boys (Stable conduct disordered-hyperaetive (SCDH), Stable conduct disordered (SGD). Stable non deviat control(SC)) were- defined and Followed up three, four and five years later in primary schools. Using assessments From multiple informants (teachers, mothers peers, self), the results showed that SCDH boys were more hyperactive (i.e. overactive inattentive) and displayed a greater diversity of conduct problems in school and home at follow-up compared to other groups. These results, and the fact that during early adolescence SCDH boys tend to develop a worse prognosis than SCD boys suggest that they should be distinguished.
    Type of Medium: Electronic Resource
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