The Composition and Origin of Vanadium-Rich Clay Minerals in Colorado Plateau Jurassic Sandstones

J. D. Meunier*
GS CNRS-CREGU, CREGU, BP23, 54501 Vandoeuvre les Nancy, France
* Present address: Laboratoire de Geoscience de l'Environment, URA CNRS 132 Case 431, Université d'Aix-Marseille III, 13397 Marseille Cedex 20, France.

Abstract: The composition and origin of vanadium-bearing clay minerals in the Jurassic (Morrison and Entrada Formations) sandstones of the Colorado Plateau are reassessed using microanalyses (microprobe and scanning electron microscope). The main V-clays are authigenic illite and chlorite of various petrologic habits: clay casts and matrix, pore lining, replacement of detrital grains. The chemical composition of the V-clays is similar in three different localities in the Morrison Formation separated by about 50 km, suggesting that the V-clays are the result of a large regional event. In both illite and chlorite, Al and V are inversely correlated, showing that V replaces Al in the octahedral position. The chlorite contains a complex mixture of divalent and trivalent cations that cannot fit within a sudoite structure. A classification of V-micas is proposed that employs V3+/sum of the octahedral cations vs. the sum of the interlayer charges. V-illite and roscoelite from the Colorado Plateau are characteristic of diagenetic/hydrothermal environments. For a given locality the composition of the V-clays does not vary with habit, showing that these minerals formed at thermodynamic equilibrium.

Key Words: Chlorite • Diagenegis • Illite • Microprobe • Roseoelite • Sandstone • SEM • Vanadium

Clays and Clay Minerals; August 1994 v. 42; no. 4; p. 391-401; DOI: 10.1346/CCMN.1994.0420403
© 1994, The Clay Minerals Society
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