(Table XXXV, pages 238-241) Chemical composition of nodules from the Atlantic Ocean


The H2O is determined by air-drying the nodule samples at 200°C for two hours. The loss on ignition (LOI) is then measured after a one hour heating at 1100°C. In reducing the analyses to a detrital mineral free basis, SiO2, Al2O3, H2O, and CaCO3 in amounts greater than 5%, were considered as detrital minerals.

DOI https://doi.org/10.1594/PANGAEA.864080
Related Identifier https://doi.org/10.1594/PANGAEA.864089
Related Identifier http://www.sciencedirect.com/science/bookseries/04229894/1/supp/C
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.864080
Creator Mero, John L
Publisher PANGAEA - Data Publisher for Earth & Environmental Science
Publication Year 1965
Rights Creative Commons Attribution 3.0 Unported
OpenAccess true
Language English
Resource Type Dataset
Format text/tab-separated-values
Size 427 data points
Discipline Chemistry
Spatial Coverage (-78.783W, -53.000S, 124.483E, 39.950N); Bermuda Rise; Atlantic Ocean; North Atlantic Ocean; Indian Ocean
Temporal Coverage Begin 1939-01-01T00:00:00Z
Temporal Coverage End 1962-03-19T00:00:00Z