1,810,744 research outputs found
Core-section summary from IODP Hole 317-U1354C
No full textCore-section summary from IODP Hole 317-U1354
(Supplement) Oedometer test results for samples from IODP Sites 317-U1351, 317-U1352, 317-U1353 and 317-U1354
No full text(Supplement) Oedometer test results for samples from IODP Sites 317-U1351, 317-U1352, 317-U1353 and 317-U135
Bulletin No. 317 - Marketing Western Feeder Cattle
No full textBulletin No. 317 - Marketing Western Feeder Cattl
IODP Expedition 317: Exploring the Record of Sea-Level Change Off New Zealand
No full textExpedition 317 investigated the record of global sea-level change (eustasy) within continental margin sedimentary to produce preserved sedimentary architectures. The Canterbury Basin, on the eastern margin of the South Island because of high rates of Neogene sediment supply from the uplifting Southern Alps. This sediment input results in a high-frequency (~0.1–0.5 My periods) record of depositional cyclicity that is modulated by the presence of strong ocean currents. The expedition recovered sediments as old as Eocene but focused on the sequence stratigraphy of the late Miocene to Recent, when global sea-level change was dominated by glacioeustasy. A transect of three sites was drilled on the continental shelf (Sites U1353, U1354, and U1351), plus one on the continental slope (Site U1352). The transect samples the shallow-water environment most directly affected by relative sea-level change. Lithologic boundaries, provisionally correlative with seismic sequence boundaries, have been identified in cores from each site. Continental slope Site U1352 provides a record of ocean circulation and fronts during the last ~35 My. The early Oligocene (~30 Ma) Marshall Paraconformity was the deepest target of Expedition 317 and is hypothesized to represent intensified current erosion or non-deposition associated with the initiation of thermohaline circulation in the region. Expedition 317 involved operational challenges for JOIDES Resolution, including shallow-water, continental-shelf drilling and deep penetrations. Despite these challenges, Expedition 317 set a number of records for scientific ocean drilling penetration and water-depth.ArticleScientific Drilling. 12:4-14 (2011)journal articl
Participant 317 Community Conversations Animation
No full textIn this graphics/digital artwork and original music composition by Participant 317 from the group MLP Artists, titled "Fine Line," the participant describes their work: " 'Fine Line' is an animation that symbolizes a story that everyone has experienced; No matter how different their story may be from one another. This quarantine has been rough for us all, and this animation displays a story that can be looked at in many different ways. This animation was made so that everyone could experience a connection with it, on how their story of quarantine went."New Jersey Department of Healt
Resolución UNRN Nº 317/2009. Designar docente interino.
No full textFil: Universidad Nacional de Río Negro (U). Universidad Nacional de Río Negro. Río Negro, ArgentinaResolución UNRN Nº 317/2009. Designar docente interino.fals
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
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