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This paper discusses the interpretation of high-resolution X-ray fluorescence (XRF) data from the Bone Spring and Upper Wolfcamp formations in the Delaware Basin, focusing on sedimentary processes and stratigraphic architecture. It highlights the advantages of XRF for analyzing fine-scale mineralogical and geochemical variations, which are crucial for understanding depositional cyclicity and rock properties in unconventional hydrocarbon production. The study emphasizes the challenges posed by the complex de

Author
mgachemichael
Language
EN

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