T228 Science and Technology Advancement in Responsible Mining of Critical Minerals from Primary and Secondary Resources I
Wednesday, 25 September 2024
8:00 AM - 12:00 PM
209B
PROSPECTING FOR CRITICAL MINERALS AND RARE EARTH ELEMENTS FROM MARCELLUS SHALE IN THE WESTERN PORTION OF THE APPALACHIAN BASIN WITH NON-DESTRUCTIVE CORE CHARACTERIZATION
Paper number: T228-7
Program: Technical Sessions
Time: 9:30 AM – 9:45 AM
Authors
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Scott WorkmanNETL Support Contractor, Morgantown, WV
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Scott WorkmanNational Energy Technology Laboratory, Morgantown, WV
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Jessica DorscheNETL Support Contractor, Morgantown, WV
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Jessica DorscheNational Energy Technology Laboratory, Morgantown, WV
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Terry McKisicNational Energy Technology Laboratory, Morgantown, WV
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Terry McKisicNETL Support Contractor, Morgantown, WV
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Dustin CrandallNational Energy Technology Laboratory, Morgantown, WV
Abstract
Using historical core characterization data from 12 Marcellus wells from the western portion of the Appalachian Basin, this study builds an improved understanding of the chemostratigraphy of the basin. X-ray fluorescence (XRF) and CT images were used to determine lithologic intervals and potential ore bodies for further analysis, including benchtop digestion and inductively coupled plasma mass spectrometry (ICP-MS) to better understand the CM/REE enrichments. All 12 wells include 6 cm resolution elemental data from an Olympus Delta handheld XRF spectrometer, core petrophysical measurements (density, magnetic susceptibility, p-wave), and continuous medical CT images for the cored sections. Utilization of these resources enables the prospecting of potential well-to-well and cross basin targets.
The initial results of this analysis show the REE/CM enrichments are primarily within the redox sensitive organic black shale facies in the wells, indicated through enrichments in Ni, Cu, V, Mo, and Zn. We also find REE/CM enrichments within redox state transition zones where carbonate concretions form with large amounts of Ba, Fe, and S concurrent with enrichments in Ni and V. This occurs throughout the wells in Northwestern West Virginia and Southwest Pennsylvania in 2- to 3-ft intervals between the Cherry Valley Limestone and the organic-rich lower Marcellus.
Geological Society of America Abstracts with Programs. Vol. 56, No. 5
doi: 10.1130/abs/2024AM-404815
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