S2 - Iron intensities of the measured split core sediment surface area from XRF core scanning of Site 208-1262
| Cobertura |
LATITUDE: -27.185833 * LONGITUDE: 1.577000 * DATE/TIME START: 2003-03-24T00:00:00 * DATE/TIME END: 2003-03-29T00:00:00 * MINIMUM DEPTH, sediment/rock: 95.04 m * MAXIMUM DEPTH, sediment/rock: 150.54 m |
|---|---|
| Data(s) |
25/01/2007
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| Formato |
text/tab-separated-values, 8607 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.592293 doi:10.1594/PANGAEA.592293 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.603177 Westerhold, Thomas; Röhl, Ursula; Laskar, Jacques; Raffi, Isabella; Bowles, Julie; Lourens, Lucas Joost; Zachos, James C (2007): On the duration of magnetochrons C24r and C25n and the timing of early Eocene global warming events: Implications from the Ocean Drilling Program Leg 208 Walvis Ridge depth transect. Paleoceanography, 22, PA2201, doi:10.1029/2006PA001322 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #208-1262; Center for Marine Environmental Sciences; COMPCORE; Composite Core; Depth, composite; DEPTH, sediment/rock; Intercore correlation; Iron, area, total counts; Joides Resolution; Leg208; MARUM; Ocean Drilling Program; ODP; ODP sample designation; Sample code/label; Walvis Ridge, Southeast Atlantic Ocean; X-ray fluorescence core scanner (XRF) II, Bremen |
| Tipo |
Dataset |
