(Table 1) Chemical and isotope compositions of interstitial water in sediments from Mediterranean basin at DSDP Site 42-372
| Cobertura |
LATITUDE: 40.080000 * LONGITUDE: 4.796500 * DATE/TIME START: 1975-04-19T00:00:00 * DATE/TIME END: 1975-04-19T00:00:00 * MINIMUM DEPTH, sediment/rock: 120 m * MAXIMUM DEPTH, sediment/rock: 579 m |
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| Data(s) |
28/09/2000
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| Formato |
text/tab-separated-values, 49 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.704767 doi:10.1594/PANGAEA.704767 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.704810 Vengosh, Avner; Gieskes, Joris M; Mahn, Chris L (2000): New evidence for the origin of hypersaline pore fluids in the Mediterranean basin. Chemical Geology, 163(1), 287-298, doi:10.1016/S0009-2541(99)00131-X |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #42-372; Boron; Bromide; Chloride; Deep Sea Drilling Project; delta 11B; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; ICP-MS, Inductively coupled plasma - mass spectrometry; Iodometric chemical method; Leg42; Lithium; Mediterranean Sea/BASIN; Negative-thermal ionization mass spectrometry (N-TIMS); ODP sample designation; Sample code/label |
| Tipo |
Dataset |
