(Table 3) Sedimentology of core W8803B-51GC
| Cobertura |
LATITUDE: 1.300000 * LONGITUDE: -133.600000 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 4.65 m |
|---|---|
| Data(s) |
04/12/1993
|
| Formato |
text/tab-separated-values, 924 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.76313 doi:10.1594/PANGAEA.76313 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.729776 Murray, Richard W; Leinen, Margaret W; Isern, Alexandra R (1993): Biogenic flux of Al to sediment in the central Pacific Ocean: evidence for increased productivity during glacial periods. Paleoceanography, 8(5), 651-670, doi:10.1029/93PA02195 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #Accumulation rate, calcium carbonate; Accumulation rate, sediment, mean; AGE; Aluminium; Aluminium/Titanium ratio; Aluminium flux; Calcium carbonate; Calculated; Density, dry bulk; Department of Geology, Oregon State University; DEPTH, sediment/rock; Element analysis coulometric; GC; Gravity corer; ICP-MS, Inductively coupled plasma - mass spectrometry; OSU; Titanium; Titanium flux; W8803B; W8803B-51GC; Wecoma; X-ray fluorescence (XRF) |
| Tipo |
Dataset |
