Chemical and isotope compositions of rocks dredged from the Shatsky Rise

Magmatic rocks of the Shatsky Rise form two groups replacing one another in time. The earlier ferrotholeiites enriched in potassium compose large massifs. Trachybasalts form seamounts and neotectonic ridges. Composition of volcanites indicates that two sources of magmatism took part in their formation: a depleted source characteristic of basalts of mid-ocean ridges and a ''plume'' source participating in formation of oceanic plateaus.

Data and Resources

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Cite this as

Kashintsev, Georgy L (2002). Dataset: Chemical and isotope compositions of rocks dredged from the Shatsky Rise. https://doi.org/10.1594/PANGAEA.761699

DOI retrieved: 2002

Additional Info

Field Value
Imported on November 30, 2024
Last update November 30, 2024
License CC-BY-3.0
Source https://doi.org/10.1594/PANGAEA.761699
Author Kashintsev, Georgy L
Given Name Georgy L
Family Name Kashintsev
Source Creation 2002
Publication Year 2002
Resource Type application/zip - filename: Kashintsev-2002
Subject Areas
Name: Oceans

Related Identifiers
Title: Magmatism of the Shatsky Rise
Type: DOI
Relation: IsSupplementTo
Year: 2002
Source: Translated from Okeanologiya, 2002, 42(4), 582-591
Authors: Kashintsev Georgy L .