Chemical composition of rocks from the Marcus-Necker Rise

Rudnik, Grigory B;Matveenkov, Vladimir V

Description

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.

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Mentions (0)

Metrics

Dataset Index

0.3

FAIR Score

88%

Citations

0

Mentions

0

Metrics Over Time

Publication Details

DOI

Publisher

PANGAEA

License

Creative Commons Attribution 3.0 Unported

Assigned Domain

Subfield

Renewable Energy, Sustainability and the Environment

Field

Energy

Domain

Physical Sciences

Confidence Score

62%

Source

Scholar Data Model

Keywords

Event labelLatitude of eventLongitude of eventElevation of eventSample typeSample code/labelSilicon dioxideTitanium dioxideAluminium oxideIron oxide, Fe2O3Iron oxide, FeOManganese oxideMagnesium oxideCalcium oxideSodium oxidePotassium oxideWater in rockPhosphorus pentoxideLoss on ignitionSumTrawl netDredgeWet chemistryLoss of ignition analysisCalculatedVityaz-48VITYAZVityaz (ex-Mars)Archive of Ocean Data (ARCOD)

Normalization Factors

FT

94.23

CTw

1.00

MTw

1.00