(Table 1) Magnesium isotope composition of analyzed unlithified sediments of ODP Hole 112-685A and 201-1230A from the Peru Margin
Cobertura |
MEDIAN LATITUDE: -9.112775 * MEDIAN LONGITUDE: -80.583500 * SOUTH-BOUND LATITUDE: -9.113000 * WEST-BOUND LONGITUDE: -80.583500 * NORTH-BOUND LATITUDE: -9.112550 * EAST-BOUND LONGITUDE: -80.583500 * DATE/TIME START: 1986-11-22T13:50:00 * DATE/TIME END: 2002-03-16T22:35:00 * MINIMUM DEPTH, sediment/rock: 6.5 m * MAXIMUM DEPTH, sediment/rock: 459.1 m |
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Data(s) |
25/01/2016
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Formato |
text/tab-separated-values, 112 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.857296 doi:10.1594/PANGAEA.857296 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
doi:10.1594/PANGAEA.857303 Mavromatis, Vasileios; Meister, Patrick; Oelkers, Eric H (2014): Using stable Mg isotopes to distinguish dolomite formation mechanisms: A case study from the Peru Margin. Chemical Geology, 385, 84-91, doi:10.1016/j.chemgeo.2014.07.019 |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #112-685A; 201-1230A; Comment; delta 25Mg; delta 25Mg, standard deviation; delta 26Mg; delta 26Mg, standard deviation; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; Event label; Joides Resolution; Latitude of event; Leg112; Leg201; Longitude of event; Main Lithology; MC-ICP-MS Thermo-Finnigan Neptune; Ocean Drilling Program; ODP; ODP sample designation; Replicates; Sample code/label; South Pacific Ocean; Traces |
Tipo |
Dataset |