Clay mineral composition and biogenic opal content in upper Miocene to Quaternary drift sediments, ODP Site 178-1096
| Cobertura |
LATITUDE: -67.566817 * LONGITUDE: -76.963517 * DATE/TIME START: 1998-02-27T00:00:00 * DATE/TIME END: 1998-02-27T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 587.11 m |
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| Data(s) |
15/11/2005
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| Formato |
text/tab-separated-values, 3500 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.218252 doi:10.1594/PANGAEA.218252 |
| 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 | #178-1096; Age model; Calculated, see reference(s); Chlorite; COMPCORE; Composite Core; Depth, composite; DEPTH, sediment/rock; Illite; Intercore correlation; interpolated; Joides Resolution; Kaolinite; Leg178; Lithogenic material; Ocean Drilling Program; ODP; ODP sample designation; Opal, biogenic silica; Sample code/label; Sedimentation rate; Size fraction < 0.002 mm, > 9 phi, clay; Smectite; South Pacific Ocean |
| Tipo |
Dataset |
