Karsten Secher
Abstract
Open-access reader
Carbonatite was emplaced in two stages at c. 600 Ma in the border between the Archaean craton and the Nagssugtoqidian mobile belt. During and after emplacement hydrothermal activity gave rise to fenitisation and alteration with increased contents of Nb and REE adjacent to the igneous core.
OpenAlex reports 9 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
Carbonatite was emplaced in two stages at c. 600 Ma in the border between the Archaean craton and the Nagssugtoqidian mobile belt. During and after emplacement hydrothermal activity gave rise to fenitisation and alteration with increased contents of Nb and REE adjacent to the igneous core.
Key concepts: Geology, Carbonatite, Oceanography, Geochemistry, Mantle (geology)