A multi-technique evaluation of hydrothermal hematite U Pb isotope systematics: Implications for ore deposit geochronology
Abstract
Hematite (α-Fe2O3) 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 formation within iron-oxide copper gold and banded iron formation deposits. However, there has been no detailed evaluation of the potential challenges this novel mineral geochronometer may present for accurate temporal interpretation. We report a multi-technique UPb...
Paper Details
Title
A multi-technique evaluation of hydrothermal hematite U Pb isotope systematics: Implications for ore deposit geochronology
Published Date
May 1, 2019
Journal
Volume
513
Pages
54 - 72
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