Date of Award

2026

Degree Name

Physical and Applied Science

College

College of Science

Type of Degree

M.S.

Document Type

Thesis

First Advisor

Dr. Aley El-Shazly

Second Advisor

Dr. Michael Caudill

Third Advisor

Dr. David Brink-Roby

Abstract

Rare earth elements (REEs) and Yttrium are classified as “critical minerals” that are used in many industries and are typically extracted from carbonatites and related alkaline plutonic rocks. The limited availability of REE+Y requires finding alternate sources such as coal fly ash, tonstein, fireclays, and shales. This study investigates the potential enrichment of shales, fireclays, and siltstones interbedded with coal from southwestern WV in REEY, and the mechanisms of such enrichment. Using ICP-AES analysis of various rock types shows that shales, silty shales, and siderite nodules interbedded with Fire Clay and Chilton Coal beds in the Kanawha Formation record the highest ΣREEY values. Scanning Electron Microscope examination of these samples shows that the REEY are hosted exclusively by monazite (Ce, La, Nd, Th)PO4, and xenotime (Y, HREE)PO4. Textures of these two minerals suggest a detrital origin with minor diagenetic overgrowths. The occurrence of the minerals sanidine, zircon with oscillatory zoning, and resorbed quartz grains all suggests that most detrital minerals have a volcanic origin. High ΣREEY values in siderite nodules containing framboidal pyrite can be linked to a diagenetic origin of this enrichment.

Subject(s)

Geology.

Geochemistry.

Sedimentology.

Sedimentary rocks.

Coal mines and mining.

Shale.

Mineralogy.

Minerals.

Petrology.

Rare earth metals.

Scanning electron microscopy.

West Virginia.

Long1.pdf (322 kB)
Long 2.pdf (203 kB)

Share

COinS