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Kevin L. Shelton

Researcher at University of Missouri

Publications -  80
Citations -  1977

Kevin L. Shelton is an academic researcher from University of Missouri. The author has contributed to research in topics: Dolomite & Dolomitization. The author has an hindex of 24, co-authored 79 publications receiving 1818 citations. Previous affiliations of Kevin L. Shelton include Korea University & Yale University.

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Dolomitization and Dolomite Neomorphism in the Back Reef Facies of the Bonneterre and Davis Formations (Cambrian), Southeastern Missouri

TL;DR: The back reef facies of the Bonneterre and Davis Formations consists of dolomitized cryptalgalaminates and partially dolomeditized peloid mudstones as mentioned in this paper.
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Gold-rich mesothermal vein deposits of the Republic of Korea; geochemical studies of the Jungwon gold area

TL;DR: Measured and calculated compositions of ore fluids in the Jungwon area (delta 18 O = 5.0 to 7.7ppm; delta D = -78 to -113ppm) indicate that gold was deposited from a highly evolved meteoric water that underwent extreme 18 O enrichment and moderate D enrichment.
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Composition and origin of ore-forming fluids in a carbonate-hosted porphyry copper and skarn deposit; a fluid inclusion and stable isotope study of Mines Gaspe, Quebec

TL;DR: In this article, three distinct thermal fluids are associated with late-stage porphyry copper ore deposition and the largest ore concentrations were the result of rapid cooling of the ore-bearing fluids by convecting meteoric waters.
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Fluid-Inclusion Studies of Regionally Extensive Epigenetic Dolomites, Bonneterre Dolomite (Cambrian), Southeast Missouri: Evidence of Multiple Fluids during Dolomitization and Lead-Zinc Mineralization

TL;DR: In this article, micro-thermometric data for fluid inclusions in the regionally extensive epigenetic dolomite at the base of the ore-hosting Bonneterre Dolomite and in gangue Dolnite of the Viburnum Trend Pb-Zn district are presented.
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Cyclic variations of sulfur isotopes in Cambrian stratabound Ni-Mo- ( PGE-Au) ores of southern China

TL;DR: In this paper, the authors attributed cyclic variations of δ 34 S values over a range of at least 48‰ in pyrite nodules from stratabound Ni-Mo-PGE(Au) ores of southern China are attributed to biogenic reduction of seawater sulfate in an anoxic, phosphogenic, and metallogenic basin.