This is a Preprint and has not been peer reviewed. This is version 1 of this Preprint.

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Abstract
This Chapter provides an overview of the nature and origin of kimberlites, carbonatites and alkaline silicate rocks, with emphasis on the strategic mineral deposits linked to these types of mantle-derived volcanism (e.g., diamonds and rare-earth elements). It is demonstrated that many of the critical raw materials hosted by carbonatites and alkaline silicate rocks are essential for the transition to a renewable energy based global economy. Both geoscientific and metallurgical research will be of paramount importance to better understand these volatile-rich magmatic systems and their economic mineralization.
DOI
https://doi.org/10.31223/X51Q7M
Subjects
Education
Keywords
Critical metals, sustainable development goals, deep carbon cycle, mineral exploration, diamond, peralkaline rocks
Dates
Published: 2025-02-27 08:00
Last Updated: 2025-02-27 14:00
License
CC BY Attribution 4.0 International
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Conflict of interest statement:
None
Data Availability (Reason not available):
All data used and compiled are made available
There are no comments or no comments have been made public for this article.