Features of the Riphean-Early Paleozoic magmatism of the southeast of the Siberian platform

Features of the Riphean-Early Paleozoic magmatism of the southeast of the Siberian platform

Geochemical study of mafic dikes and sills of the Riphean (Ulakhanbam) and Ordovician (Suordakh) ages in the area of the Sette-Daban ridge allowed to establish differences between these complexes. For the Ulakhanbam magmatic rocks, the mantle source was basically similar in characteristics to E-MORB...

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Veröffentlicht in:IOP conference series. Earth and environmental science 2019-08, Vol.319 (1), p.12017
Hauptverfasser: Savelev, A D, Yu Lebedeva, O
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Sprache:eng
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Contamination
Isotopes
Lava
Ordovician
Paleozoic
Rock intrusions
Sediment pollution
Soil contamination
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description Geochemical study of mafic dikes and sills of the Riphean (Ulakhanbam) and Ordovician (Suordakh) ages in the area of the Sette-Daban ridge allowed to establish differences between these complexes. For the Ulakhanbam magmatic rocks, the mantle source was basically similar in characteristics to E-MORB. Despite the possible sediment contamination, wide range of εNd(T) values is most likely due to the specific composition of the mantle source, which likely had an admixture of OIB material. The Ordovician reservoir had OIB characteristics, whereas the MORB material had a subordinate significance.
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subjects Contamination
Isotopes
Lava
Ordovician
Paleozoic
Rock intrusions
Sediment pollution
Soil contamination
title Features of the Riphean-Early Paleozoic magmatism of the southeast of the Siberian platform
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