Petrogenesis of Large Igneous Province and Carbonatite-Related Rare Earth Element Deposits

A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Mineral Deposits".

Deadline for manuscript submissions: 31 July 2024 | Viewed by 203

Special Issue Editors


E-Mail Website
Guest Editor
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China
Interests: mantle plume; large igneous province and the related deposits

E-Mail Website
Guest Editor
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China
Interests: magma plumbing system; mineralogy; REE and rare metal deposits

Special Issue Information

Dear Colleagues,

Large igneous provinces (LIPs) are produced by voluminous magma eruption (area >105 km2, volume >105 km3) within a relatively short time (1–5 Ma). They are the most magnificent expression of magmatism in the Earth’s interior on the surface. The formation of LIPs could trigger extensive thermal and material exchange between different earth spheres, and hence are considered to be closely related to the topographic and environmental changes, as well as major metallogenic events.

With the reputation of being “modern industrial vitamins”, rare earth elements (REE) are among the most important strategic resources in the world. Notably, the worldwide REE ore deposits of economic importance are commonly associated with carbonatite–alkaline complexes, also containing niobium (Nb)-rich minerals and apatite (P). Therefore, carbonatite-related REE-Nb-P deposits are among the focus of REE-Nb-P prospecting. Specifically, some carbonatite–alkaline complexes are closely related to LIPs, such as Deccan, Paraná-Etendeka, Siberia, Kola-Dneiper, Bushveld, Keweenawan and Tarim LIPs.

This Special Issue aims to contribute to the petrogenesis of LIPs and carbonatite-related REE deposits. It is organized to focus on the following scientific questions:

(1) To reveal the petrogenesis of carbonatite–alkaline complexes in LIPs and their implications on the formation of LIPs;

(2) To find out the factors controlling fractionation and enrichment of light, heavy rare earth elements, Nb and P elements in the carbonatitic magmatic-hyrothermal processes;

(3) To investigate new scientific models for future exploration and prospecting of REE resources worldwide.

Dr. Zhiguo Cheng
Dr. Xiaowei Li
Guest Editors

Manuscript Submission Information

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Keywords

  • large igneous provinces
  • mantle plume
  • carbonatite
  • rare earth element deposits

Published Papers

This special issue is now open for submission.
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