Clay mineral composition of sediment core JR141_VC415
| Cobertura |
LATITUDE: -73.895800 * LONGITUDE: -115.931100 * DATE/TIME START: 2006-01-28T05:08:00 * DATE/TIME END: 2006-01-28T05:08:00 * MINIMUM DEPTH, sediment/rock: 0.20 m * MAXIMUM DEPTH, sediment/rock: 4.20 m |
|---|---|
| Data(s) |
11/12/2011
|
| Formato |
text/tab-separated-values, 192 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.755023 doi:10.1594/PANGAEA.755023 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.755199 Ehrmann, Werner; Hillenbrand, Claus-Dieter; Smith, James A; Graham, Alastair GC; Kuhn, Gerhard; Larter, Robert D (2011): Provenance changes between recent and glacial-time sediments in the Amundsen Sea embayment, West Antarctica: clay mineral assemblage evidence. Antarctic Science, 23(5), 471-486, doi:10.1017/S0954102011000320 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #Amundsen Sea; Chlorite; DEPTH, sediment/rock; Illite; Illite, integral width; Illite 5Å/10Å Esquevin-index; James Clark Ross; JR141_VC415; JR141 JR150; JR20060109; Kaolinite; Smectite; VC; VC415; Vibro Corer; X-ray diffraction TEXTUR, clay fraction |
| Tipo |
Dataset |
