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See detailLower airway dysfunction in athletic horses
Votion, Dominique ULiege; Art, Tatiana ULiege; Lekeux, Pierre ULiege

in In Proceedings: Journées Vétérinaires Suisses (1996, September)

During the last decade, research in exercising horses provided growing evidence that the respiratory system may be a limiting factor for maximal performance, even in healthy animals. Therefore, any ... [more ▼]

During the last decade, research in exercising horses provided growing evidence that the respiratory system may be a limiting factor for maximal performance, even in healthy animals. Therefore, any pulmonary dysfunction, even subclinical or moderate, may significantly impair the aerobic metabolism and consequently performance of exercising horses. This paper briefly presents the main respiratory troubles of lower airway as well as the main pulmonary function tests used to diagnose these diseases. [less ▲]

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See detailLower airway function: response to exercise and training
Art, Tatiana ULiege; Bayly, Warwick

in Hinchcliff, Kenneth W.; Kaneps, Andris J.; Geor, Raymont J. (Eds.) Equine Sports Medicine and Surgery. Basic and clinical Sciences of the Equine Athlete. 2d Edition (2014)

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See detailLower and Middle Devonian miospore-based stratigraphy in Libya and its relation to the megafloras and faunas
Streel, Maurice ULiege; Fairon-Demaret, Muriel ULiege; Gerrienne, Philippe ULiege et al

in Review of Palaeobotany and Palynology (1990), 66(3), 229--242

Detailed reference viewed: 34 (9 ULiège)
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See detailLower and Middle Famennian (Upper Devonian) rugose corals from southern Belgium and northern France
Denayer, Julien ULiege; Poty, Edouard ULiege; Marion, Jean-Marc ULiege et al

in Geologica Belgica (2012), 15(4), 273-283

Detailed reference viewed: 52 (14 ULiège)
See detailLower Carboniferous corals from the Zonguldak Area (Black Sea, Northwestern Turkey).
Denayer, Julien ULiege

in PPMB-MVP meeting abstract book (2009, December 04)

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See detailLower Carboniferous ramp sedimentation of the Central Alborz Basin, northern Iran: Integrated sedimentological and rock-magnetic studies
Sardar Abadi, Mehrdad ULiege; Da Silva, Anne-Christine ULiege; Mosaddegh, hossein et al

in Geological Society Special Publication (2015), 414

The Lower Carboniferous Mobarak Formation in the Alborz Basin (northern Iran) was deposited along the northeastern margin of Gondwana in a carbonate ramp setting. This paper focuses on the Tournaisian ... [more ▼]

The Lower Carboniferous Mobarak Formation in the Alborz Basin (northern Iran) was deposited along the northeastern margin of Gondwana in a carbonate ramp setting. This paper focuses on the Tournaisian stratigraphic interval of this formation that crops out at the Jaban section in the southwestern Central Alborz Basin. The following facies associations, representing different ramp palaeoenvironments, have been identified: (1) mudstone–wackestone outer-ramp facies; (2) crinoidal to skeletal grainstone–packstone mid-ramp facies; (3) peloidal to crinoidal grainstone–packstone inner-ramp facies; and (4) coastal facies, which include a variety of microbial laminated to oncoidal grainstones and mudstones with evaporitic pseudomorphs. This ramp profile was affected by frequent storms that were responsible for the formation of several skeletal to non-skeletal shoals in the distal mid-ramp to the most proximal inner-ramp areas. The development of the skeletal to non-skeletal shoals along the sea side of the ramp formed a semi-enclosed lagoon sensitive to the influence of both high tides and storm surges.The magnetic susceptibility (xin) of all the samples was measured and compared with that of the facies from which the sample was taken. There is a clear link between xin and the facies; the average xin values were higher for the distal facies than for the proximal facies. The xin profile of this Lower Carboniferous carbonate sequence reflects stratigraphic variations in response to relative changes in sea level and the input of detrital materials. In the context of the sequence stratigraphic framework, the average xin values for lowstand and transgressive systems tract deposits are higher than for the highstand systems tract deposits. The clear link between xin and facies indicates at least a partly preserved primary xin signal related to the detrital inputs. However, to obtain a better understanding of the nature and origin of the minerals carrying the xin, we performed hysteresis measurements on selected samples. It appears that the xin signal is mainly carried by lowcoercivity ferromagnetic minerals such as magnetite, with a mixture of relatively coarse grains (detrital fraction) and ultra-fine grains (probably formed during diagenesis). [less ▲]

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See detailLower Carboniferous Rugose corals from the Arabian Plate: an insight from the Hakkari area (SE Turkey)
Denayer, Julien ULiege; Hoşgör

in Journal of Asian Earth Sciences (2014), 79(1), 345-357

Detailed reference viewed: 38 (3 ULiège)
See detailLower Carboniferous Rugose corals from the Zonguldak area (Northwestern Turkey)
Denayer, Julien ULiege

in Aldridge, R.; Harper, D. (Eds.) Abstracts volume of the Third International Palaeontological Congress (IPC3) (2010)

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See detailLower critical field and SNS-Andreev spectroscopy of 122-arsenides: Evidence of nodeless superconducting gap
Abdel-Hafiez, M.; Pereira, P.J.; Kuzmichev, S.A. et al

in Physical Review. B : Condensed Matter (2014), 90

Using two experimental techniques, we studied single crystals of the 122-FeAs family with almost the same critical temperature, Tc. We investigated the temperature dependence of the lower critical field ... [more ▼]

Using two experimental techniques, we studied single crystals of the 122-FeAs family with almost the same critical temperature, Tc. We investigated the temperature dependence of the lower critical field Hc1(T) of a Ca0.32Na0.68Fe2As2 (Tc ≈ 34 K) single crystal under static magnetic fields H parallel to the c axis. The temperature dependence of the London penetration depth can be described equally well either by a single anisotropic s-wave-like gap or by a two-gap model, while a d-wave approach cannot be used to fit the London penetration depth data. Intrinsic multiple Andreev reflection effect spectroscopy was used to detect bulk gap values in single crystals of the intimate compound Ba0.65K0.35Fe2As2, with the same Tc. We estimated the range of the large gap value L = 6–8 meV (depending on small variation of Tc) and its a k space anisotropy of about 30%, and the small gap Delta ≈ 1.7 ± 0.3 meV. This clearly indicates that the gap structure of our investigated systems more likely corresponds to a nodeless s-wave two gaps. [less ▲]

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See detailThe Lower Devonian around the "Lac de la Gileppe"
Steemans, Philippe ULiege; Gerrienne, Philippe ULiege

Conference (1994)

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See detailLower Devonian flora from Morocco and its palaeogeographical implications
Gerrienne, Philippe ULiege; Fairon-Demaret, Muriel ULiege; Galtier, J. et al

Conference (1997)

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See detailLower Devonian palynomorphs from the San Juan Precordillera, Argentina
Rubinstein, C. V.; Le Hérissé, A.; Steemans, Philippe ULiege

Conference (1996)

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See detailLower Devonian Palynomorphs from the Talacasto Formation, Cerro del Fuerte Section, San Juan Precordillera, Argentina
Le Hérissé, A; Rubinstein, CR; Steemans, Philippe ULiege

in Acta Universitatis Carolinae. Geologica (1996), 40(3-4), 497-515

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See detailLower Devonian plant mesofossils from Paraná Basin, Brazil: general introduction, description, age significance and correlation with floral succession from Laurussia and Gondwana.
Gerrienne, Philippe ULiege

in Rodrigues, M.A.C.; Pereira, E. (Eds.) : Ordovician-Devonian palynostratigraphy in Western Gondwana: update, problems and perspectives. (1999)

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See detailLower Devonian rhynchonellid brachiopods from the Ougarta area (western Sahara, Algeria)
Brice, Denise; Boumendjel, Kheira; Racheboeuf, Patrick R. et al

in Bulletin of Geosciences (2011), 86(1), 71-90

The description and study of rhynchonellid brachiopods recently collected from the Lower Devonian of the Ougarta area in western Algerian Sahara permitted the revision of previously described and/or ... [more ▼]

The description and study of rhynchonellid brachiopods recently collected from the Lower Devonian of the Ougarta area in western Algerian Sahara permitted the revision of previously described and/or listed taxa, mainly from Morocco. Palaeobiogeographically, the nine identified taxa share many similarities with the rhynchonellid fauna of the Ibarmaghian Domain. Five of the nine identified taxa belong to three genera of the Family Nucinulidae Sartenaer, 2004. Three of these are new taxa, namely Nucinulus orbignyanus crassicostus subsp. nov., Cuninulus ougartaensis sp. nov. and Palinulus saharaensis sp. nov. The our remaining taxa are assigned (one of them questionably) to the genera Lanceomyonia, Stenorhynchia and Glossinulus of the families Hebetoechiidae, Trigonirhynchiidae, and Glossinotoechiidae, respectively. [less ▲]

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See detailLower Devonian spores from South Wales.
Chaloner, W.G.; Streel, Maurice ULiege

in Argumenta Palaeobotanica (1968), 1

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See detailLower Devonian spores from the Ardennes-Rhine area
Steemans, Philippe ULiege

Conference (1984)

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See detailLower impact of blue light on non-visual brain functions in older subjects
Daneault, V; Vandewalle, Gilles ULiege; Hébert, M et al

Poster (2012, February)

Detailed reference viewed: 13 (3 ULiège)