Chemical composition of rocks from the Marcus-Necker Rise

DOI

The Marcus Necker Rise has two geologically distinct parts: the western one is composed of the Marcus Wake seamounts and the eastern one of the Wake-Necker seamounts. The first contain differentiated alkali basaltoids, while the second show a distinctive prolonged and complicated history. The latter contain Early Cretaceous olivine basalts and Late Cretaceous alkali and hornblende basaltoids.

Supplement to: Rudnik, Grigory B; Matveenkov, Vladimir V (1978): Composition and stages of development of volcanic rocks in the Marcus-Necker Ridge. Oceanology, 18(3), 319-322

Identifier
DOI https://doi.org/10.1594/PANGAEA.755169
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.755169
Provenance
Creator Rudnik, Grigory B; Matveenkov, Vladimir V
Publisher PANGAEA
Publication Year 1978
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Language English
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 259 data points
Discipline Chemistry; Natural Sciences
Spatial Coverage (-169.122W, 18.317S, 157.383E, 23.867N); Marcus-Necker Ridge