『Abstract
A significant resource of vanadium and molybdenum exists near
Julia Creek, Australia, where the middle Cretaceous organic-rich
Toolebuc Formation lies between 0 and 25 m of the surface. We
present and discuss a comprehensive geochemical study of the Toolebuc
Formation and its enclosing stratigraphy near Julia Creek to understand
this ore deposit. V and Mo contents in fresh facies are strongly
associated with total organic carbon (TOC) contents, but not with
Al or CaCO3; this suggests that V and Mo
were originally concentrated in the organic fraction. However,
chemical extractions using H2O2
indicate that Mo was originally concentrated in pyrite. The data
also suggest that V was mobilized from organic matter during early
diagenesis and became associated with clays as little V was extracted
by H2O2 in the fresh
samples. TOC contents in the Toolebuc Formation were removed during
weathering, residually enriching trace metals including V and
Mo, and as a result, the TOC relationship with V and Mo disintegrates.
With weathering, both V and Mo predominantly became associated
with iron oxide/hydroxide phases (and possibly other unidentified
phases) as these elements in the weathered facies were highly
soluble in the sodium citrate-sodium dithionite digestion. Large
shale-hosted V and Mo deposits such as Julia Creek offer a potentially
viable alternative to the currently mined magnetite-hosted deposits.
A thorough understanding of the formation and host mineral phases
for V and Mo of these shale deposits, however, is critical to
ensure that these valuable metals can be feasibly extracted.
Keywords: Vanadium; Molybdenum; Toolebuc Formation; Eromanga Basin;
Oil shale; Coquina; Inorganic geochemistry』
Introduction
Geological setting
Local geology
Samples and methods
Primary samples and geochemical analyses
Supplemental samples, preparation and analyses
Bulk rock extractions
Results
Bulk rock mineralogy
Bulk rock geochemistry
Bulk rock geochemistry related to aluminosilicates (clay fraction)
Bulk rock geochemistry related to calcite (carbonate fraction)
Bulk rock geochemistry in relation to TOC (organic component)
Bulk rock geochemistry in relation to sulphides/sulphates
Trace element variation: vanadium
Trace element variation: molybdenum
Isocon plots
Bulk rock extractions
Discussion
Bulk rock extractions
Vanadium and molybdenum hosts
Conclusions
Acknowledgements
References