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Author: Grafiati

Published: 7 July 2024

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1

Saleil, Jean, Marc Mantel, and Jean Le Coze. "La production des aciers inoxydables: Histoire de son développement et des procédés de fabrication. Partie III. Évolutions des méthodes de coulée et de mise en forme des aciers inoxydables." Matériaux & Techniques 108, no. 1 (2020): 105. http://dx.doi.org/10.1051/mattech/2020016.

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La coulée des aciers inoxydables, autrefois en lingots, s’effectue aujourd’hui par coulée continue. Ce mode de coulée a permis une considérable simplification de la gamme de fabrication (suppression du dégrossissage au blooming). La généralisation de la coulée continue aux aciers inoxydables fut assez tardive car il fallait satisfaire à deux impératifs qualitatifs essentiels : l’état de surface et la propreté inclusionnaire du métal déjà largement pris en compte par les affinages AOD et VOD. La complexité de la séquence de solidification des aciers inoxydables, notamment celle des aciers austénitiques, a aussi pesé sur le choix du mode de coulée. Le choix des outils de la filière coulée continue/mise en forme à chaud, pour les produits plats, est largement conditionné par le volume de production et par la proximité d’un train à bandes. Le laminoir Steckel a eu son utilité pour des productions de faibles volumes. Aujourd’hui les grandes usines en produits plats en aciers inoxydables ont des capacités suffisamment importantes pour leur dédier un train à bande (TAB) ; d’autres utilisent, en association, un train à bande pour aciers au carbone. La résolution des problèmes particuliers posés par la mise en forme à chaud des aciers inoxydables, notamment ceux liés au trou de ductilité à chaud des austénites, est décrite. Les cas particuliers de la mise en forme à chaud des tubes, des produits forgés sont évoqués. Les questions concernant la mise en forme à froid : laminage, emboutissage, écrouissage… sont abordées.

2

Semmler, Josef. "Hermann Jakobs, Eugen III. und die Anfänge europäischer Stadtsiegel nebst Anmerkungen zum Bande IV der Germania Pontificia." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte: Kanonistische Abteilung 71, no. 1 (August 1, 1985): 364–66. http://dx.doi.org/10.7767/zrgka.1985.71.1.364.

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3

Xu, Jie, and R. L. Conner. "Intravarietal variation in satellites and C-banded chromosomes of Agropyron intermedium ssp. trichophorum cv. Greenleaf." Genome 37, no. 2 (April 1, 1994): 305–10. http://dx.doi.org/10.1139/g94-042.

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A high amount of intravarietal variation in satellites and C-banded chromosomes was observed in the hexaploid wheatgrass synthetic cultivar 'Greenleaf' (Agropyron intermedium ssp. trichophorum (Link) A. &Gr., 2n = 6x = 42, genome E1E1E2E2SS). The cultivar is an open-pollinated perennial that shows extensive interplant polymorphism for many biological characters. Maximum number of satellites detected varied among plants from zero to six. In 61% of the plants, we observed two large satellites in association with zero, one, or two small ones. Chromosome constitution differed significantly among plants as revealed by analysis of variance based on the total number of banded chromosomes and the number of banded chromosomes with telomeric bands at either one or both ends. Heteromorphism in C-banding patterns between homologues was found in most of the chromosomes and was classified into four types: (i) difference in band size, (ii) difference in presence/absence of one or two bands, (iii) completely different banding patterns, and (iv) banded versus unbanded. Homologous chromosomes having types iii and iv heteromorphism could only be matched by their relative length and arm ratio instead of C-banding patterns. Deletions were detected in two chromosomes. Overall, C-banded chromosomes of this cultivar were characterized by the presence of large telomeric bands and were quite different from the previously reported karyotypes of the supposed diploid ancestor Agropyron elongatum (Host) P. Beauv. (genome EE) and an Ag. intermedium (Host) P. Beauv. accession (E1E1E2E2SS) The results suggest that dramatic chromosome modifications have occurred in this species during the course of evolution. The study sheds light on the extent of intrapopulation polymorphism present in the karyotypes of outcrossing polyploids and synthetic cultivars and has implications regarding strategies for chromosomal manipulation involving open-pollinated species.Key words: Agropyron intermedium ssp. trichophorum, intravarietal variation, satellites, C-banded karyotype.

4

Becet, Jean-Marie. "2. Construction dans la bande des cent mètres. Article L. 146-4-III du Code de l'urbanisme. Notion d'espace urbanisé. Tribunal administratif de Rennes, 25 octobre 1990 Epoux Jooris (Req. n° 86-2866). Avec note." Revue Juridique de l'Environnement 16, no. 3 (1991): 396–400. http://dx.doi.org/10.3406/rjenv.1991.2735.

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5

Favre, Justine. "Raconter l’expérience du sujet plurilingue, biographies langagières en bande dessinée." FLE: français langue en expérience(s) 323 (2024): 83–108. http://dx.doi.org/10.4000/11qej.

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De quelles manières des étudiants francophones et des apprenants de FLE de niveau avancé se sont-ils servis du potentiel graphique et narratif de la bande dessinée pour mettre en récit leur expérience du plurilinguisme? Cet article propose le compte rendu d’un atelier donné dans le cadre d’un séminaire universitaire et l’analyse de trois des bandes dessinées qui y ont été produites. Le concept de métaphore graphique développé ici montre, aux côtés d’outils plus classiques d’analyse, en quoi la bande dessinée offre des ressources pour exprimer de façon créative et réflexive un vécu entre plusieurs langues.

6

Dey, Monojit, Sourav Bhattacharjee, Aniket Chakrabarty, Roger H. Mitchell, Supriyo Pal, Supratim Pal, and Amit Kumar Sen. "Compositional variation and genesis of pyrochlore, belkovite and baotite from the Sevattur carbonatite complex, India." Mineralogical Magazine 85, no. 4 (April 14, 2021): 588–606. http://dx.doi.org/10.1180/mgm.2021.37.

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AbstractPyrochlore-group minerals are common in the Neoproterozoic Sevattur carbonatite complex. This complex is composed of dolomite-, calcite-, banded- and blue carbonatite together with pyroxenite, albitite and diverse syenites. This work reports the paragenetic-textural types and compositional variation of pyrochlore hosted by dolomite carbonatite, banded carbonatite and albitite together with that of alteration assemblages containing belkovite and baotite. On the basis of composition, five different types of pyrochlore are recognised and termed Pcl-I through to Pcl-V. The Pb-rich Pcl-I are present exclusively as inclusions in U-rich Pcl-IIa in dolomite carbonatite. The alteration assemblages of Pb-poor Pcl-IIb + Ba-rich or Ba–Si- rich Pcl-IV + belkovite (dolomite carbonatite) and Si-rich Pcl-V + baotite (banded carbonatite) formed after Pcl-IIa differ in these carbonatites. The albitite hosts extremely U-Ti-rich Pcl-III, mantled by Ba-rich potassium feldspar. In common with the banded carbonatite, Pcl-V is formed by alteration of Pcl-III where this mantle is partially, or completely broken. The Ba-Si-enrichment of Pcl-IV and Pcl-V together with the ubiquitous presence of baryte in all Sevattur lithologies suggests late-stage interaction with a Ba-Si-rich acidic hydrothermal fluid. This fluid was responsible for leaching silica from the associated silicates and produced Pcl-V in the silicate-rich lithologies of the banded carbonatite and albitite. The absence of Pcl-V in dolomite carbonatite is a consequence of the low modal abundance of silicates. The complex compositional diversity and lithology specific pyrochlore alteration assemblages suggest that all pyrochlore (Pcl-I to Pcl-IV) were formed initially in an unknown source and transported subsequently in their respective hosts as altered antecrysts.

7

Lemay, Sylvain, and Jean-François Boulé. "Le personnage féminin dans les bandes de l’Action catholique (1935-1938)." ALTERNATIVE FRANCOPHONE 1, no. 9 (February 22, 2016): 93–107. http://dx.doi.org/10.29173/af25711.

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Les années 1930 ont constitué un terreau fertile pour l’éclosion d’œuvres qui sont devenues des classiques de la bande dessinée et ce, tant américaine que franco-belge. Au Québec, le marché est surtout occupé par des traductions de bandes américaines. De 1935 à 1938, L’Action catholique publiera 11 récits, totalisant plus de 700 bandes. Il s’agit, pour la majorité, d’adaptations de romans québécois du terroir faisant l’apologie des racines canadiennes-françaises et de la religion catholique, tels L’appel de la race de Lionel Groulx. Ces adaptations sont livrées sous la forme d’image d’Épinal. Nous étudions ici ces bandes dessinées et, plus précisément le rôle du personnage féminin dans ces histoires, notamment dans Son chemin de Damas qui est aussi le seul récit à utiliser le phylactère.

8

Samsuri, Alya, and Salma Khansa. "APPLICATION OF THE PROJECT BASED LEARNING MODEL TO IMPROVE STUDENT LEARNING OUTCOMES IN CLASS IIB FRACTIONAL MATERIAL OF SD NEGERI 4 BANDA ACEH." Jurnal Ilmiah Teunuleh 3, no. 2 (June 28, 2022): 187–201. http://dx.doi.org/10.51612/teunuleh.v3i2.111.

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This study aims to describe student activities by applying the Project Based Learning learning model to improve student learning outcomes in class IIB fractional material SD Negeri 4 Banda Aceh. This type of research is Classroom Action Research (PTK) which aims to improve the quality of learning in the classroom. The subjects in this study amounted to 22 grade IIB students of SD Negeri 4 Banda Aceh City. Data collection techniques are carried out by observation and learning outcome tests. Based on the results of research in cycles I, II, and III obtained the following data: (1) the results of observations on student activities in learning observed for three cycles, increased each cycle, namely: student activity in cycle I reached 85.22%, cycle II reached 87.37%, and cycle III reached 93.45%. (2) the learning outcomes of students in fractional material have increased in cycle I of classical completeness criteria reaching 50% with an average value of 73.63, in cycle II classical completeness criteria of 81.81% with an average value of 85, while cycle III of classical completeness criteria 95.43% with an average value of 93.63. From the results of the study, it can be concluded that the application of the Project Based Learning learning model on fractional material can improve the learning outcomes of grade IIB students of SD Negeri 4 Banda Aceh.

9

Kuna Raj, John. "Characterizing a weathering profile over quartz-mica schists in undulating terrain in Peninsular Malaysia." Warta Geologi 48, no. 3 (December 30, 2022): 153–63. http://dx.doi.org/10.7186/wg483202202.

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The weathering profile can be differentiated into an upper, 4.8 m thick, pedological soil (zone I) and a lower, >16.2 m thick, saprock (zone II). Zone I comprises thin IA and IB soil horizons of firm, clayey sand with lateritic concretions, and a IC soil horizon of stiff, clayey silt with quartz clasts and lateritized core-stones. Zone II comprises steeply dipping to vertical, bands of pinkish to grey, stiff silt with distinct relict foliation (highly weathered schist) inter-fingering with bands of reddish yellow, firm clayey silt with indistinct foliation (completely weathered schist) towards its top, and bands of white to light grey, hard silt with distinct foliation (moderately weathered schist) towards its bottom. Lateral variations in abundance of differently weathered schist and preservation of fracture planes allow zone II to be separated into IIA, IIB and IIC sub-zones. The pedological soil (zone I) can be correlated with Class VI of standard rock mass weathering classifications, whilst the saprock sub-zones IIA, IIB and IIC are correlated with Classes V, IV and III, respectively. Silt fractions in the profile consist predominantly of sericite flakes, whilst the sand fractions are mostly of quartz grains and the clay fractions of mainly illite and kaolinite. Decreasing densities, unit weights and silt contents up the profile, but increasing porosities and clay contents, indicate increasing in situ alteration of the schist bedrock. Lowering of an unconfined groundwater table as a result of down-cutting by rivers in adjacent valleys is considered responsible for development of the weathering profile.

10

Hong, Yong-Eui, Chi-Woo Lee, Gi-Ho Kim, Myo-Geun Yang, and Won-Mo Seong. "Triple-band Antenna Using PCB for T-DMB(Band III)/DAB(L-Band)/WiBro." Journal of Korean Institute of Electromagnetic Engineering and Science 18, no. 2 (February 28, 2007): 227–32. http://dx.doi.org/10.5515/kjkiees.2007.18.2.227.

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11

Lundsteen, Claes, and Erik Granum. "Microphotometry of banded human chromosomes III." Clinical Genetics 10, no. 1 (April 23, 2008): 33–40. http://dx.doi.org/10.1111/j.1399-0004.1976.tb00006.x.

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12

Frémont, P., P. M. Charest, C. Côté, and P. A. Rogers. "Carbonic anhydrase III in skeletal muscle fibers: an immunocytochemical and biochemical study." Journal of Histochemistry & Cytochemistry 36, no. 7 (July 1988): 775–82. http://dx.doi.org/10.1177/36.7.3133407.

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The objectives of the present study were to determine if carbonic anhydrase III (CA III) demonstrated a specific association for any particular organelle or structure of the skeletal muscle cell and to quantify the activity and content of this enzyme in different types of skeletal muscle fibers. Ultrastructural localization of CA III in the soleus (SOL), deep vastus lateralis (DVL), and superficial vastus lateralis (SVL), composed of predominantly type I, IIa, and IIb fibers, respectively, was performed using a high-resolution immunocytochemical technique and antibody specific for CA III on ultra-thin sections of skeletal muscle embedded in the water-soluble medium polyvinyl alcohol (PVA). The results indicated a uniform distribution of CA III within the sarcomere. Mitochondria, nuclei, triads, Z-, and M-bands were not specifically labeled. Immunoblotting of washed myofibril preparations did not show any detectable CA III associated with this structure. In addition to quantification of the immunogold labeling, CA III activity and content were assayed in the post-mitochondrial supernatant of the three muscles. In the SOL, these values were found to be 3.6-7.6 times higher than in the DVL. The SVL showed a labeling intensity slightly higher than background level, while the enzyme activity and content were indistinguishable from background levels. We therefore conclude that CA III is randomly distributed in the cytoplasm of the three muscle fiber types and that the relative CA III content and activity in the three muscles studied is SOL greater than DVL greater than SVL approximately equal to 0.

13

Barker, G. M. "Pasture renovation: interactions of vegetation control with slug and insect infestations." Journal of Agricultural Science 115, no. 2 (October 1990): 195–202. http://dx.doi.org/10.1017/s0021859600075122.

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SUMMARYIn a field trial at Rukuhia, New Zealand, ryegrass (Lolium perenne L.) and white clover (Trifolium repens L.) seed was direct drilled into pasture (i) without herbicide suppression of the resident sward, (ii) with banded application of glyphosate or paraquat herbicide at drilling to remove 50% of the resident sward and (iii) after complete removal of the grass and weed components of the old sward with glyphosate or paraquat before drilling. These treatments were compared with the untreated old swards. Where the old sward was removed by herbicide before drilling, pests moved onto the drilled seedling rows, but, where herbicide was sprayed in bands over the drill rows, the pests remained in or moved into the residual bands of the old sward. Significant beneficial interactions between herbicide use and in-furrow applications of molluscicides and insecticides resulted in reductions in the numbers of pests on the seedling rows. The influence of vegetation control on the pest burden is discussed in the context of current pasture renovation practices.

14

Gómez-Vivo, David, Fernando Gervilla, Rubén Piña, Rebeca Hernández-Díaz, and Antonio Azor. "Gold in the Farallones Block of the Shale-Hosted, Clastic-Dominated Castellanos Zinc-Lead Deposit (Northwest Cuba)." Minerals 11, no. 4 (April 14, 2021): 414. http://dx.doi.org/10.3390/min11040414.

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The Zn-Pb ores of the Castellanos shale-hosted, clastic-dominated deposit in northwest Cuba average nearly 1 g/t Au, with local maximum concentrations up to 34 g/t Au. This deposit is stratiform with respect to the bedding in the host black shales and shows a bottom to top zoning of ore assemblages made up of a stockwork underlying the main orebody, a basal pyrite-rich zone and a disseminated to massive Zn-Pb ore zone capped by a discontinuous, thin barite-rich zone. Petrographic data and textural relations allow distinguishing five textural types of pyrite (framboidal Py I, colloform Py IIa, euhedral Py IIb, massive Py IIc and banded colloform Py III) successively formed during ore deposition. The main Zn-Pb ore formed after the crystallization of disseminated, sedimentary framboidal pyrite (Py I) in black shales by the superimposition of several crystallization events. The crystallization sequence of the main ore-forming stage evolved from the precipitation of colloform sphalerite and pyrite (Py IIa) with skeletal galena and interstitial dolomite-ankerite to similar ore assemblages but showing subhedral to euhedral crystal habits (Py IIb) and interstitial calcite-rich carbonates. This stage ended with the development of massive pyrite (Py IIc), mainly occurring at the base of the stratiform orebody. A late fracturing stage gave way to the development of a new generation of colloform banded pyrite (Py III) just preceding the crystallization of early barite. Au is mainly concentrated in pyrite showing variable contents in the different textural types of pyrite and a bottom to top enrichment trend. Minimum contents occur in massive pyrite (Py IIc) from the basal pyrite-rich zone (0.18 ppm Au average), increasing in pyrite IIa (from 0.29 to 2.86 ppm Au average) and in euhedral pyrite (Py IIb) (from 0.82 to 9.02 ppm Au average), reaching maxima in colloform banded pyrite (Py III) formed just before the crystallization of early barite at the top of the orebody. Au enrichment in pyrite correlates with that of Sb (0.08–4420 ppm), As (0.7–35,000 ppm), Ag (0.03–1560 ppm) and to a lesser extent Cu (3–25,000 ppm), Ni (0.02–1600 ppm) and Mn (0.6–5030 ppm). Au deposition should have taken place by oxidation and, probably cooling, of reduced (H2S-dominated) fluids buffered by organic matter-rich black shales of the host sedimentary sequence. The input of such reduced fluids in the ore-forming environment most probably occurred alternating with that of the main oxidized fluids which leached Zn and Pb from the large volume of sandstones and siltstones making up the enclosing sequence, thus being responsible for the precipitation of the majority Zn-Pb ore. Supply of Au-carrying reduced fluids might progressively increase over the course of ore formation, reaching a maximum at the beginning of the late fracturing stage. This evolution of Au supply is consistent with the early crystallization of barite since Ba can also only be transported at low temperature by highly reduced fluids. These results highlight the potential of medium-sized, shale-hosted, clastic-dominated deposits to contain economic (by product) Au amounts and show that ore-forming fluids can change from oxidized (SO42+ dominated) to reduced (H2S-dominated), and vice versa, throughout the evolutionary history of a single deposit.

15

Cohen, Martin, A. G. G. M. Tielens, Jesse Bregman, Fred C. Witteborn, David M. Rank, L. J. Allamandola, Dianne Wooden, and M. Jourdain de Muizon. "The infrared emission bands. III - Southern IRAS sources." Astrophysical Journal 341 (June 1989): 246. http://dx.doi.org/10.1086/167489.

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16

CONSTANTINOU, Georgia. "Interjections et onomatopées : quelle richesse pour la bande dessinée ?" Langues & Cultures 3, no. 01 (June 20, 2022): 43–60. http://dx.doi.org/10.62339/jlc.v3i01.141.

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L’interjection et l’onomatopée ont longtemps été écartées des recherches linguistiques. Cependant, leur étude a préalablement permis d’établir des bases pragmatiques dont les approches révèlent leur richesse expressive. Dans le but d’analyser leur traduction et leur utilisation dans une bande dessinée, nous avons ici choisi une optique linguistico-musicale. Si l’interjection sert de marqueur d’oralité dans un texte écrit, comme en témoignent les bandes dessinées francophones, l’onomatopée, quant à elle, présente, grâce à son rapport mimétique avec la réalité extralinguistique, des caractéristiques musicales aidant à compléter et nuancer l’analyse d’un texte dans une bande dessinée. Abstract Interjection and onomatopoeia have long been excluded from linguistic research. However, their study has previously made it possible to establish pragmatic bases whose approaches reveal their expressive richness. To analyze their translation and use in a comic strip, we have chosen here a linguistic-musical perspective. If the interjection serves as a marker of orality in a written text, as evidenced by French-language comic strips, onomatopoeia, for its part, presents, thanks to its mimetic relationship with extralinguistic reality, musical characteristics that help to complete and nuance the analysis of a text in a comic strip.

17

Sorasaenee, Karn, Pouyan Taqavi, Lawrence M. Henling, Harry B. Gray, Elena Tkachenko, Atif Mahammed, and Zeev Gross. "Amphiphilic aluminium(III) and gallium(III) corroles." Journal of Porphyrins and Phthalocyanines 11, no. 03 (March 2007): 189–97. http://dx.doi.org/10.1142/s1088424607000242.

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The preparation and spectroscopic properties of a series of metallocorroles with polar head groups CHO and CH = C ( CN )( COOH ) are reported, as well as the X-ray crystal structure of 5,10,15-tris(pentafluorophenyl)corrolatoaluminium(III)bispyridine (triclinic space group (P-1) with unit cell parameters: a = 9.426(1) Å; b = 13.202(1) Å; c = 19.936(1) Å; α = 74.19(1)°; β = 78.47(1)°; γ = 75.75(1)°; V = 2289.57(8) Å3). Amphiphilic aluminium(III) and gallium(III) corroles exhibit electronic absorption (Soret peaks between 410 and 448 nm; Q-bands between 584 and 638 nm) and fluorescence (band maxima between 634 and 706 nm) at lower energies than their hydrophobic analogs.

18

Tuszynski, W., and E. Strauss. "Four emission bands from a quadrate chronium(III) complex." Journal of Luminescence 40-41 (February 1988): 276–77. http://dx.doi.org/10.1016/0022-2313(88)90192-5.

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19

Hobbs, L. M., D. G. York, J. A. Thorburn, T. P. Snow, M. Bishof, S. D. Friedman, B. J. McCall, et al. "STUDIES OF THE DIFFUSE INTERSTELLAR BANDS. III. HD 183143." Astrophysical Journal 705, no. 1 (October 7, 2009): 32–45. http://dx.doi.org/10.1088/0004-637x/705/1/32.

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20

Kumar, C. K. "Diffuse interstellar bands in low color excess stars. III." Astrophysical Journal 306 (July 1986): 38. http://dx.doi.org/10.1086/164318.

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21

Coquart, B., and D. A. Ramsay. "High-resolution studies of the near-ultraviolet bands of oxygen: III: the system." Canadian Journal of Physics 64, no. 6 (June 1, 1986): 726–32. http://dx.doi.org/10.1139/p86-132.

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Ten bands of the [Formula: see text] system of oxygen have been observed in absorption using longer path lengths than in the earlier work of Herzberg (1953). Rotational analysis of the bands confirms that the A′ 3Δu state is an inverted state as expected from electron-configuration arguments. Rotational assignments are given for the [Formula: see text] and [Formula: see text] sub-bands with ν′ = 2–11; weaker [Formula: see text] sub-bands are identified for ν′ = 5–11. Sub-band origins and rotational constants are given for all the bands. The following derived molecular constants are obtained:[Formula: see text]A comparison of the frequencies of the diffuse bands of oxygen with the sub-band origins of the [Formula: see text] bands shows convincingly that the diffuse bands can be assigned to a weak (O2)2 complex in which one of the O2 molecules is excited to the A′ 3Δu state.

22

SIMON, Justine. "Climat sous tension, un « récit climatique » interactif engagé mêlant bande dessinée, audiovisuel et jeu." Nouvelles écritures interactives audiovisuelles 6, no. 1 (February 12, 2018). http://dx.doi.org/10.25965/interfaces-numeriques.2809.

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L’analyse des dispositifs communicationnels numériques développant de nouvelles formes de narrations interactives représente un enjeu de recherche pour comprendre les différentes stratégies mises en œuvre pour toucher les publics. L’objectif de cet article est d’analyser un discours audiovisuel hypertextualisé interactif exploitant plusieurs récits présentés sous forme de bandes dessinées numériques, représentant différentes tribunes d’experts au format audiovisuel et structurés de manière ludique : il s’agit de Climat sous tension, pensé et réalisé dans le contexte socio-politique de la COP21 en 2015 par TV5 Québec Canada et TV5 Monde. Trois angles d’analyse sont proposés : (i) l’un concernant la composition multimédiatique du discours, (ii) le deuxième s’intéressant à la dynamique interdiscursive existant entre les récits et les discours audiovisuels liés, (iii) et le dernier étudiant les procédés interlocutifs mis en place. L’objectif est de comprendre la dimension argumentative du discours, cherchant implicitement à convaincre le lecteur de lutter contre le réchauffement climatique.

23

Daigneault, Robert-André, and Serge Occhietti. "Les moraines du massif Algonquin, Ontario, au début du Dryas récent, et corrélation avec la Moraine de Saint-Narcisse." 60, no. 2 (December 10, 2007): 103–18. http://dx.doi.org/10.7202/016823ar.

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Résumé La cartographie détaillée des moraines majeures et mineures de la région du parc Algonquin, à partir de l’interprétation de photographies aériennes à grande échelle et de levés de terrain, permet de corréler plus de 150 éléments discontinus de marge glaciaire qui peuvent être regroupés en trois alignements morainiques régionaux, nommés Algonquin I, II et III, disposés sur une bande orientée ONO-ESE d’une largeur de 20 km. Ces alignements sont antérieurs à la Moraine de Genesee, au sud-est du lac Nipissing, et aux déversements du Lac glaciaire Algonquin vers la Mer de Champlain, via les exutoires de White Partridge, Fossmill et Sobie-Guilmette. Ils sont corrélés latéralement avec les positions morainiques A, B et BC du lobe de l’Outaouais. L’alignement Algonquin III-Outaouais BC s’étend sur 250 km en Ontario. Il est associé vers l’est à la Moraine de Saint-Narcisse qui peut être suivie sur 750 km au Québec et dont l’âge se situe entre 10 700 et 10 500 BP (12,7-12,4 ka cal.). Vers l’ouest, au nord du lac Huron, il est probablement contemporain de la Moraine du lac Whiskey. Cette hypothèse permettrait de prolonger le tracé du front de l’Inlandsis laurentidien sur 400 kilomètres additionnels, pendant la halte majeure du début du Dryas récent correspondant à la Moraine de Saint-Narcisse au Québec.

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"Inhalt des 120. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte. Romanistische Abteilung 120, no. 1 (August 1, 2003): III—X. http://dx.doi.org/10.7767/zrgra.2003.120.1.iii.

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"Inhalt des 121. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte. Romanistische Abteilung 121, no. 1 (August 1, 2004): III—X. http://dx.doi.org/10.7767/zrgra.2004.121.1.iii.

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"Inhalt des 122. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte. Romanistische Abteilung 122, no. 1 (August 1, 2005): III—VIII. http://dx.doi.org/10.7767/zrgra.2005.122.1.iii.

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"Inhalt des 123. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte. Romanistische Abteilung 123, no. 1 (August 1, 2006): III—X. http://dx.doi.org/10.7767/zrgra.2006.123.1.iii.

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"Inhalt Des 124. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte. Romanistische Abteilung 124, no. 1 (August 1, 2007): III—XII. http://dx.doi.org/10.7767/zrgra.2007.124.1.iii.

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"Inhalt des 125. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte. Romanistische Abteilung 125, no. 1 (August 1, 2008): III—X. http://dx.doi.org/10.7767/zrgra.2008.125.1.iii.

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"Inhalt des 126. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte. Romanistische Abteilung 126, no. 1 (August 1, 2009): III—VII. http://dx.doi.org/10.7767/zrgra.2009.126.1.iii.

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"Inhalt des CII. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte: Kanonistische Abteilung 71, no. 1 (August 1, 1985): III—VI. http://dx.doi.org/10.7767/zrgka.1985.71.1.iii.

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"Inhalt des CHI. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte: Kanonistische Abteilung 72, no. 1 (August 1, 1986): III—VII. http://dx.doi.org/10.7767/zrgka.1986.72.1.iii.

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"Inhalt des CIV. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte: Kanonistische Abteilung 73, no. 1 (August 1, 1987): III—V. http://dx.doi.org/10.7767/zrgka.1987.73.1.iii.

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"Inhalt des CVIII. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte: Kanonistische Abteilung 77, no. 1 (August 1, 1991): III—VIII. http://dx.doi.org/10.7767/zrgka.1991.77.1.iii.

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"Inhalt des CX. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte: Kanonistische Abteilung 79, no. 1 (August 1, 1993): III—VII. http://dx.doi.org/10.7767/zrgka.1993.79.1.iii.

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"Inhalt des CXI. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte: Kanonistische Abteilung 80, no. 1 (August 1, 1994): III—VI. http://dx.doi.org/10.7767/zrgka.1994.80.1.iii.

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"Inhalt des CXII. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte: Kanonistische Abteilung 81, no. 1 (August 1, 1995): III—VI. http://dx.doi.org/10.7767/zrgka.1995.81.1.iii.

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"Inhalt des CXIII. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte: Kanonistische Abteilung 82, no. 1 (August 1, 1996): III—V. http://dx.doi.org/10.7767/zrgka.1996.82.1.iii.

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"Inhalt des 115. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte: Kanonistische Abteilung 84, no. 1 (August 1, 1998): III—V. http://dx.doi.org/10.7767/zrgka.1998.84.1.iii.

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"Inhalt des 116. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte: Kanonistische Abteilung 85, no. 1 (August 1, 1999): III—VI. http://dx.doi.org/10.7767/zrgka.1999.85.1.iii.

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"Inhalt des 117. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte: Kanonistische Abteilung 86, no. 1 (August 1, 2000): III—VIII. http://dx.doi.org/10.7767/zrgka.2000.86.1.iii.

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"Inhalt des 118. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte: Kanonistische Abteilung 87, no. 1 (August 1, 2001): III—VI. http://dx.doi.org/10.7767/zrgka.2001.87.1.iii.

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"Inhalt des 119. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte: Kanonistische Abteilung 88, no. 1 (August 1, 2002): III—V. http://dx.doi.org/10.7767/zrgka.2002.88.1.iii.

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"Inhalt des 120. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte: Kanonistische Abteilung 89, no. 1 (August 1, 2003): III—VI. http://dx.doi.org/10.7767/zrgka.2003.89.1.iii.

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"Inhalt des 121. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte: Kanonistische Abteilung 90, no. 1 (August 1, 2004): III—VIII. http://dx.doi.org/10.7767/zrgka.2004.90.1.iii.

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"Inhalt des 122. Bandes." Zeitschrift der Savigny-Stiftung für Rechtsgeschichte: Kanonistische Abteilung 91, no. 1 (August 1, 2005): III—VI. http://dx.doi.org/10.7767/zrgka.2005.91.1.iii.

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