Establishing timescales for iron oxide copper-gold (IOCG) deposit formation and the
temporal relationships between ores and the magmatic rocks from which hydrothermal …

Hematite (α-Fe2O3) and magnetite (Fe3O4) readily accommodate a wide range of minor
and trace elements from across the periodic table at up to wt.% concentrations. This prompts …

Abstract Hematite (α-Fe 2 O 3) is a common iron-oxide mineral known to incorporate U into
its crystal lattice at up to wt% concentrations and has been previously used to date ore …

Abstract In the Borborema Province, iron formations occur in Archean-Paleoproterozoic
nuclei including the highly metamorphosed and deformed Granjeiro Complex. In this work …

Spatial associations between banded iron formation and iron-oxide Cu-Au (IOCG) style
mineralization are well documented in the Gawler Craton (South Australia), but the possible …

This study demonstrates the great value of iron oxide chemistry in low-temperature systems.
Hematite records elemental signatures of structural control, partial inheritance of pre-existing …

The first U-Pb hematite dates are reported for the Mantoverde and Carmen de Cobre iron
oxide copper-gold (IOCG) deposits in the northern segment of the Coastal Cordillera, Chile …

The petrography and geochemistry of zircon offers an exciting opportunity to better
understand the genesis of, as well as identify pathfinders for, large magmatic–hydrothermal …

In both nature and synthetic experiments, the common iron oxide haematite (α‐Fe2O3) can
incorporate significant amounts of U into its crystal structure and retain radiogenic Pb over …

Hematite and goethite deposits hosted in banded iron formations (BIFs) in the Pilbara craton
(Western Australia) represent one of Earth's most significant Fe reserves; however, the …