Clay mineral composition and biogenic opal content in upper Miocene to Quaternary drift sediments, ODP Site 178-1095
Cobertura |
LATITUDE: -66.985400 * LONGITUDE: -78.487867 * DATE/TIME START: 1998-02-13T00:00:00 * DATE/TIME END: 1998-02-13T00:00:00 * MINIMUM DEPTH, sediment/rock: 1.04 m * MAXIMUM DEPTH, sediment/rock: 561.60 m |
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Data(s) |
15/11/2005
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Formato |
text/tab-separated-values, 3782 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.218251 doi:10.1594/PANGAEA.218251 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
doi:10.1594/PANGAEA.735191 Hillenbrand, Claus-Dieter; Ehrmann, Werner (2005): Late Neogene to Quaternary environmental changes in the Antarctic Peninsula region: evidence from drift sediments. Global and Planetary Change, 45, 165-191, doi:10.1016/j.gloplacha.2004.09.006 |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #178-1095; Age model; Calculated, see reference(s); Chlorite; COMPCORE; Composite Core; Depth, composite; DEPTH, sediment/rock; Grain size, sieving/settling tube; Illite; Intercore correlation; interpolated; Joides Resolution; Kaolinite; Leg178; Lithogenic material; Ocean Drilling Program; ODP; ODP sample designation; Opal, auto analysis (Müller & Schneider, 1993); Opal, biogenic silica; Sample code/label; Sedimentation rate; Size fraction < 0.002 mm, > 9 phi, clay; Smectite; South Pacific Ocean; X-ray diffraction TEXTUR, clay fraction |
Tipo |
Dataset |