Formation of the Mount Weld rare earth deposit, Western Australia: Geochronology constraints

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Abstract

Constraining the age of protracted chemical weathering in stable cratonic areas that may form thick regoliths and the potential enrichment of various elements is challenging. Economic deposits of aluminium, iron, copper, nickel, cobalt, niobium, and rare earth elements (REEs) form in this manner. Determining the age of formation can provide key information for exploration of similar deposits as well as to better constrain  paleoclimatic conditions. This study describes our effort to constrain the age of formation of the Mount Weld deposit, a world-class carbonatite-derived REE laterite deposit. We utilize multiple geochronological techniques on different minerals. The oldest dates, ranging from ca. 100 to 50 Ma, were from laser ablation ICPMS, Lu-Hf dating of churchite, a heavy REE phosphate mineral formed by mineral saturation in groundwater. Growth bands on individual minerals show a younging outwards. 40Ar/39Ar geochronology of cryptomelane, a potassium-bearing manganese oxide mineral, yielded ages ranging from ca. 40 to 26 Ma. Similarly, (U–Th)/He geochronology of goethite yielded ages from ca. 45 to 19 Ma.

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Publication type Conference Paper
Publication Subtype Conference Paper
Title Formation of the Mount Weld rare earth deposit, Western Australia: Geochronology constraints
Volume 2
Year Published 2025
Language English
Publisher Society for Geology Applied to Mineral Deposits
Contributing office(s) Geology, Geophysics, and Geochemistry Science Center
Description 5 p.
First page 695
Last page 699
Conference Title 18th SGA Biennial Meeting
Conference Location Golden, CO
Conference Date August 3-7, 2025
Country Australia
Other Geospatial Mount Weld deposit
Additional publication details