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    Resolución UNRN N° 536/2009. Designar docente interina.

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    Fil: Universidad Nacional de Río Negro (U). Universidad Nacional de Río Negro. Río Negro, ArgentinaResolución UNRN N° 536/2009. Designar docente interina.fals

    Inclination of the two main components of magnetization and 87Sr/86Sr ratios for dolomites at DSDP Hole 77-536

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    Site 536 terminated in a shallow-water dolomite of unknown age. Paleomagnetic measurements combined with strontium isotope analyses suggest that the dolomite was deposited in the Middle Jurassic to Early Cretaceous time interval. However, the assumptions required to reach this determination make these results less than conclusive

    Going Beyond Counting First Authors in Author Co-citation Analysis

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    The present study examines one of the fundamental aspects of author co-citation analysis (ACA) - the way co-citation counts are defined. Co-citation counting provides the data on which all subsequent statistical analyses and mappings are based, and we compare ACA results based on two different types of co-citation counting - the traditional type that only counts the first one among a cited work's authors on the one hand and a non-traditional type that takes into account the first 5 authors of a cited work on the other hand. Results indicate that the picture produced through this non-traditional author co-citation counting contains more coherent author groups and is therefore considerably clearer. However, this picture represents fewer specialties in the research field being studied than that produced through the traditional first-author co-citation counting when the same number of top-ranked authors is selected and analyzed. Reasons for these effects are discussed

    Philosophy [536]

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    Philosophy. This manuscript is now IO Islamic 1866 in the India Office collections. [metadata: Otto Loth, A Catalogue of the Arabic Manuscripts in the Library of the India Office, (volume 1), no. 536 here with further notations and hyperlinks]. 536. 1866. Size 91/4 in. by 5 in.; foll. 23. Seven lines in a page. The same work, well written in Nasta’lîḳ

    UMNH:Mamm:536

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    UMNH:Mamm:536 Voucher Specimen Study Ski

    Verlustliste Nr. 536. (Nr. 536. /1917)

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    VERLUSTLISTE NR. 536. Verlustliste (-) Verlustliste Nr. 536. (Nr. 536. /1917) ([1]) Belehrung (2) Offiziere. (3) A, B, C, D, E, F, G, H, I, J, K, L (3) M (3) N, O, P, R, S, T, U, V (4) W (4) Z (5) Einjährig-Freiwillige. (5) Mannschaft. (6) A (6) B (7) C (12) D (13) E (15) F (16) G (18) H (20) I (23) J (23) K (24) L (30) M (32) N (36) O (38) P (39) R (43) S (45) T (50) U (52) V (53) W (54) Z (55) Berichtigungen zu den Verlustlisten: (57) Nr. 21. Nr. 24. Nr. 93. Nr. 122. Nr. 131. Nr. 137. Nr. 161. Nr. 249. Nr. 387. Nr. 391. Nr. 412. Nr. 434. Nr. 451. Nr. 480. Nr. 482. Nr. 518. (57

    Porosity, permeability, trace elements, and carbon-oxygen isotopes at DSDP Hole 77-536

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    Talus deposits recovered from Site 536 show evidence of aragonite dissolution, secondary porosity development, and calcite cementation. Although freshwater diagenesis could account for the petrographic features of the altered talus deposits, it does not uniquely account for isotopic or trace-element characteristics. Also, the hydrologic setting required for freshwater alteration is not easily demonstrated for the Campeche Bank. A mixing-zone model does not account for the available trace-element data, but does require somewhat less drastic assumptions about the size of the freshwater lens. Although a seawater (bottom-water) alteration model requires no hydrologic difficulties, unusual circumstances are required to account for the geochemical characteristics of the talus deposits using this model

    Band 5, 536 (Sammlung Friedlaender)

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    BAND 5, 536 (SAMMLUNG FRIEDLAENDER) Band 5, 536 (Sammlung Friedlaender) (Public Domain) (1

    Band 6, 536 (Sammlung Friedlaender)

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    BAND 6, 536 (SAMMLUNG FRIEDLAENDER) Band 6, 536 (Sammlung Friedlaender) (Public Domain) (1
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