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

DOI

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.

Identifier
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

Provenance
Creator	Mero, John L
Publisher	PANGAEA - Data Publisher for Earth & Environmental Science
Publication Year	1965
Rights	Creative Commons Attribution 3.0 Unported
OpenAccess	true

Representation
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