Meso-Neoproterozoic Mafic Sills along the South-Eastern Margin of the Siberian Craton, SE Yakutia: Petrogenesis, Tectonic and Geochemical Features

We report major and trace element concentrations, along with Nd isotope compositions, for Late Mesoproterozoic to Early Neoproterozoic dolerite sills from the Sette-Daban ridge (southern Verkhoyansk, south-east Siberia). Based on their major element composition, all rocks correspond to low-Ti (

Saved in:
Bibliographic Details
Published in:Minerals (Basel) 2020-09, Vol.10 (9), p.805
Main Authors: Savelev, Aleksandr D., Malyshev, Sergey V., Savatenkov, Valery M., Ignatov, Daniil D., Kuzkina, Anastasia D.
Format: Article
Language:English
Subjects:
Age
Basalt
Continental crust
Cratons
Depletion
Earth mantle
Enrichment
Fluids
Geochemistry
Geological time
Geology
Igneous rocks
Isotopes
Melting
Mid-ocean ridges
Petrogenesis
Quartz
Rare earth elements
Rifting
Rivers
Sediments
Sills
Subduction
Subduction (geology)
Tectonics
Titanium dioxide
Trace elements
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:We report major and trace element concentrations, along with Nd isotope compositions, for Late Mesoproterozoic to Early Neoproterozoic dolerite sills from the Sette-Daban ridge (southern Verkhoyansk, south-east Siberia). Based on their major element composition, all rocks correspond to low-Ti (
ISSN:2075-163X
2075-163X
DOI:10.3390/min10090805