1,767,966 research outputs found
God KAL of Karahna - CTH 517
No full textAnalytical text on the inventory related to god KAL of Karahna based on tablet concordances listed in CTH 517. Emmanuel Laroche translated this text as "Dieu KAL de Karahna,” and classified the concordance in the category of religious administration in inventory texts of cults (Catalogue des textes Hittites, No. 517).Paper (4 sheets
Quaternary planktonic foraminifera of DSDP Hole 72-517
No full textQuaternary sediments were recovered at all four Sites at Leg 72. Planktonic foraminifers were abundant and well preserved, especially in the holes shielded from Antarctic Bottom Water (AABW) influence. The fauna belonged to the subtropical province marked by Globigerinoides ruber and to a lesser extent by Globorotalia inflata. Thirty planktonic foraminiferal species were distinguished, and a detailed study of the Site 517 stratigraphy was made.
The Quaternary sequence of the Rio Grande Rise was subdivided slightly differently from the Bolli and Premoli Silva (1973) pattern. Five subzones were identified but some difficulties arose when a precise correlation became necessary in the subzones of the tropical provinces. Correlations could nevertheless be made, particularly with respect to the earliest Quaternary.
Quaternary faunal data have been dated by isotopic stratigraphy (Vergnaud Grazzini et al.,1983) and partially contradict results previously published for this part of the Atlantic (Williams and Ledbetter, 1979).
By studying the occurrence of planktonic foraminifers, we obtained more information about hydrologic variations during the Quaternary sequence of Hole 517; two broad periods were recognized. Finally, we identified the interaction between the Brazil Current and the subtropical convergenc
Resolución UNRN N° 517/2009. Aprobar la designación del personal docente universitario
No full textFil: Universidad Nacional de Río Negro (U). Universidad Nacional de Río Negro. Río Negro, ArgentinaResolución UNRN N° 517/2009. Aprobar la designación del personal docente universitariofals
Going Beyond Counting First Authors in Author Co-citation Analysis
Full text linkThe 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
Automatic weather station buoy data PS81/517 from Weddell Sea, Antarctica, 2013
No full textAutomatic weather station buoy data PS81/517 from Weddell Sea, Antarctica, 2013. The buoy was deployed together with an ice mass balance buoy (see under related) on sea ice station PS81/517 from Research Vessel Polarstern in the Antarctic Weddell Sea in austral winter 2013 (cruise leg ANT-XXIX/6, AWECS campaign). The automatic weather station provides data between 2013-07-30T19:00 and 2013-11-10T12:00. Time is in UTC
Band 5, 517 (Sammlung Friedlaender)
No full textBAND 5, 517 (SAMMLUNG FRIEDLAENDER)
Band 5, 517 (Sammlung Friedlaender) (Public Domain) (1
Band 6, 517 (Sammlung Friedlaender)
No full textBAND 6, 517 (SAMMLUNG FRIEDLAENDER)
Band 6, 517 (Sammlung Friedlaender) (Public Domain) (1
(Table 2) Duration of the polarity change process at DSDP Holes 72-515A and 72-517
No full textA study has been made of downhole declination changes of the horizontal component of the natural remanent magnetization of unopened whole-core sections recovered by use of the hydraulic piston corer at DSDP Sites 515, 517, and 518. There is clear evidence that polarity reversal boundaries can be detected by this preliminary paleomagnetic technique. The Quaternary through late Neogene sediments studied reveal a record of the magnetostratigraphy over the past 4.5 Ma, although the quality of this record is better defined by the terrigenous sediments of the Brazil Basin than the biogenous oozes of the Rio Grande Rise
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