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Relevant bibliographies by topics / Le Nain

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Journal articles

Academic literature on the topic 'Le Nain'

Author: Grafiati

Published: 4 June 2021

Last updated: 5 February 2022

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Journal articles on the topic "Le Nain"

1

de Lovinfosse, Marie. "Naïn ou Naïm (Lc 7.11) : une différence révélatrice." New Testament Studies 64, no. 1 (2017): 20–32. http://dx.doi.org/10.1017/s0028688517000224.

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This study investigates spelling variants of the name of the city where Jesus raises the only son of a widow, in Lk 7.11: Nain or Naim. The study develops along three lines: textual critic, Hebraic etymology, ancient geography. The investigation eventually raises the question of the theological significance of the miracle of Nain.

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2

Dronskowski, Richard. "In2.24(NCN)3 and NaIn(NCN)2: Synthesis and Crystal Structures of New Main Group Metal Cyanamides." Zeitschrift für Naturforschung B 50, no. 8 (1995): 1245–51. http://dx.doi.org/10.1515/znb-1995-0819.

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Single crystals of In2.24(NCN)3 and NaIn(N CN)2 can be synthesized from a reaction between InBr and NaCN at 400 °C, followed by chemical transport at 400-500 °C. The X-ray crystal structure determinations of In2.24(NCN)3 (rhombohedral R3̄c, a = 606.09(4), c = 2884.4(2) pm, Z = 6) and NaIn(NCN)2 (orthorhombic Cmcm, a = 961.30(6), b = 716.84(5), c = 603.65(4) pm, Z = 4) reveal ionic layer structures built from sheets of cationic and anionic (cyanamide) motifs. While NaIn(NCN)2 contains In3+ and Na+ ions, In2.24(NCN)3 is a mixedvalence compound, incorporating a monovalent In+ ion besides trivalen

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3

Connelly, J. N., and B. Ryan. "Late Archean evolution of the Nain Province, Nain, Labrador: imprint of a collision." Canadian Journal of Earth Sciences 33, no. 9 (1996): 1325–42. http://dx.doi.org/10.1139/e96-100.

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Archean gneisses of the Nain Province in the Nain area, Labrador, comprise narrow septa between intrusions of the Mesoproterozoic Nain Plutonic Suite. This region occupies a critical position between the northern (Saglek) and southern (Hopedale) blocks of the Nain Province, which experienced distinct thermotectonic histories until the late Archean. Field and geochronological evidence are indicative of a strong late Archean thermotectonic overprint that is absent from most of the remainder of the Nain Province. Archean gneisses were intruded by granites and mafic dykes at 2578 ± 3 and [Formula:

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4

Bertrand, Anne. "frères Le Nain." Vacarme 26, no. 1 (2004): 48. http://dx.doi.org/10.3917/vaca.026.0048.

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5

Schaduw, Joshian Nicolas William. "Struktur Komunitas Dan Keberlanjutan Pengelolaan Ekosistem Mangrove Pulau-Pulau Kecil (Kasus Pada Pulau Nain Kabupaten Minahasa Utara Provinsi Sulawesi Utara)." Jurnal Ilmu Lingkungan 16, no. 2 (2018): 120. http://dx.doi.org/10.14710/jil.16.2.120-129.

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ABSTRAKKajian ini bertujuan untuk menganalisa struktur komunitas dan keberlanjutan pengelolaan ekosistem mangrove di Pulau Nain Kecamatan Wori, Kabupaten Minahasa Utara, Provinsi Sulawesi Utara. Pulau Nain adalah salah satu pulau yang masuk dalam kawasan konservasi Taman Nasional Bunaken dan memiliki kawasan budidaya rumput laut yang masih produktif. Penelitian ini menggunakan data sekunder dan primer. Data yang dibutuhkan dalam kajian ini meliputi data dimensi ekologi, sosial ekonomi, dan kelembagaan. Analisis yang digunakan dalam kajian ini adalah RAPMECS (Rapid Appraisal for Mangroves Ecosy

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6

Thaning, Kaj. "Enkens søn fra Nain." Grundtvig-Studier 41, no. 1 (1989): 32–45. http://dx.doi.org/10.7146/grs.v41i1.16017.

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The Son of the Widow from Nain.By Kaj ThaningThis article intends to elucidate the distinctions that Grundtvig made in his world of ideas in the course of the years from 1824 to 1834, first between spirit and letter, church and church-school (1826-1830), and then between natural life and Christian life (in 1832). In His "Literary Testament" (1827), Grundtvig himself admits that there was a "Chaos" in his writings, due to the youthful fervour that pervaded his literary works and his sermons in the years 1822-1824. But not until 1832 does he acknowledge that "when I speak or write as a citizen,

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7

Canning, Patricia M. "The Nain Daycare Project." Canadian Journal of Education / Revue canadienne de l'éducation 11, no. 1 (1986): 1. http://dx.doi.org/10.2307/1494611.

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8

Hordijk, Arie, and Ger Koole. "The µc-rule is not optimal in the second node of the tandem queue: a counterexample." Advances in Applied Probability 24, no. 01 (1992): 234–37. http://dx.doi.org/10.1017/s0001867800024290.

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In this note we give a counterexample which shows that the µc-rule is not optimal in the second node of the tandem queue. This counterexample contradicts the interchange argument in Nain [1] and Nain et al. [2].

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9

Hordijk, Arie, and Ger Koole. "The µc-rule is not optimal in the second node of the tandem queue: a counterexample." Advances in Applied Probability 24, no. 1 (1992): 234–37. http://dx.doi.org/10.2307/1427742.

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In this note we give a counterexample which shows that the µc-rule is not optimal in the second node of the tandem queue. This counterexample contradicts the interchange argument in Nain [1] and Nain et al. [2].

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10

Wardle, Richard J., Donald T. James, David J. Scott, and Jeremy Hall. "The southeastern Churchill Province: synthesis of a Paleoproterozoic transpressional orogen." Canadian Journal of Earth Sciences 39, no. 5 (2002): 639–63. http://dx.doi.org/10.1139/e02-004.

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The Paleoproterozoic southeastern Churchill Province (SECP) is located in the northeastern Canadian Shield of Labrador and Quebec. The SECP formed through the oblique collisions of the Archean Nain and Superior cratons with a third intervening Archean block, the core zone. The belt has a tripartite structure, comprising the Torngat Orogen (TO) formed by Nain craton core zone collision in the east, the core zone in the centre, and the New Quebec Orogen (NQO) formed by Superior craton core zone collision in the west. The SECP thus records transpressional development on the flanks of the Supe

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