(Figure 6) Selected elemental ratios from X-ray fluorescence (XRF) core scanning of sediment core DP30PC
| Cobertura |
LATITUDE: 39.834500 * LONGITUDE: 17.800800 * MINIMUM DEPTH, sediment/rock: 0.020 m * MAXIMUM DEPTH, sediment/rock: 8.275 m |
|---|---|
| Data(s) |
06/01/2014
|
| Formato |
text/tab-separated-values, 6521 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.825342 doi:10.1594/PANGAEA.825342 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.825473 Goudeau, Marie-Louise Sophie; Grauel, Anna-Lena; Tessarolo, Chiara; Leider, Arne; Chen, Liang; Bernasconi, Stefano M; Versteegh, Gerard JM; Zonneveld, Karin A F; Boer, Wim; Alonso-Hernandez, C M; de Lange, Gert Jan (2014): The Glacial-Interglacial transition and Holocene environmental changes in sediments from the Gulf of Taranto, Central Mediterranean. Marine Geology, 348, 88-102, doi:10.1016/j.margeo.2013.12.003 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #64PE297; AGE; Barium/Titanium ratio; Bromine/Titanium ratio; Calcium/Titanium ratio; Calculated; Center for Marine Environmental Sciences; DEPTH, sediment/rock; DP30PC; Iron/Titanium ratio; MARUM; PC; Pelagia; Piston corer; Potassium/Titanium ratio; Silicon/Titanium ratio; Strontium/Calcium ratio; Zirconium/Titanium ratio |
| Tipo |
Dataset |
