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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Publication Details
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)