1,764,462 research outputs found

    Astral signs [Signes astraux] - CTH 535

    No full text
    Accompanied with interpretive commetary, translation of the oracle texts related to the reading of astral signs and astrology based on the tablet concordances listed in the CTH 535. Emmanuel Laroche translated this text as "Signes astral,” and classified the concordance in the category of divination texts among treatises (Catalogue des textes Hittites, No. 535).Paper (1 sheet

    Astrological texts [Textes astrologiques] - CTH 535

    No full text
    Interpretive commetary on the oracle texts related to the reading of astral signs and astrology based on the tablet concordances listed in the CTH 535. Emmanuel Laroche translated this text as "Signes astral,” and classified the concordance in the category of divination texts among treatises (Catalogue des textes Hittites, No. 535).Paper (1 sheet

    Astrological texts [Textes astrologiques] - CTH 535

    No full text
    Interpretive commetary on the oracle texts related to the reading of astral signs and astrology based on the tablet concordances listed in the CTH 535. Emmanuel Laroche translated this text as "Signes astral,” and classified the concordance in the category of divination texts among treatises (Catalogue des textes Hittites, No. 535).Paper (1 sheet

    Geochemistry and pyrolysis at DSDP Hole 77-535

    No full text
    There are substantial differences in the character of organic matter contained in the Pleistocene and Cretaceous sedimentary sequences of DSDP Site 535. The argillaceous Pleistocene section contains type III, gas-prone organic matter whereas the calcareous Cretaceous section is dominated by type II, oil-prone organic matter. A more detailed investigation of the Cretaceous section reveals that the finely laminated limestones of Valanginian to Barremian age are of good to excellent source quality. The indigenous organic matter contained within this organically rich section is thermally immature, not having undergone sufficient thermal diagenesis for the generation and expulsion of hydrocarbons. Within this stratigraphic section, however, staining by mature hydrocarbons was detected. These stains are associated with a fractured interval. These fractures may in turn represent potential migration pathways

    Going Beyond Counting First Authors in Author Co-citation Analysis

    Get PDF
    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

    UMNH:Mamm:535

    No full text
    UMNH:Mamm:535 Voucher Specimen Study Ski

    Geochemistry and petrography of organic matter at DSDP Hole 77-535

    No full text
    Organic geochemical and organic petrographic methods were used to study three Lower to middle Cretaceous sediment samples from Hole 535 in the southeastern Gulf of Mexico for organic matter contents and origin and level of maturation. All three samples contain mixed kerogen Type II/III organic matter with a maturity corresponding to about 0.4% vitrinite reflectance. The marine component increases with stratigraphic age, and microbial reworking of the organic matter is significant in each age. The lower two samples of Hauterivian to Valanginian age appear to be impregnated (or contaminated) with soluble polar organic compounds, but there is only a weak indication for the presence of more mature, nonindigenous hydrocarbons

    Band 2, 535 (Sammlung Friedlaender)

    No full text
    BAND 2, 535 (SAMMLUNG FRIEDLAENDER) Band 2, 535 (Sammlung Friedlaender) (Public Domain) (1

    Band 6, 535 (Sammlung Friedlaender)

    No full text
    BAND 6, 535 (SAMMLUNG FRIEDLAENDER) Band 6, 535 (Sammlung Friedlaender) (Public Domain) (1
    corecore