TY - JOUR
T1 - Zirconolite and xenotime U-Pb age constraints on the emplacement of the Golden Mile Dolerite sill and gold mineralization at the Mt Charlotte mine, Eastern Goldfields Province, Yilgarn Craton, Western Australia
AU - Rasmussen, Birger
AU - Mueller, Andreas
AU - Fletcher, Ian
PY - 2009
Y1 - 2009
N2 - In situ SHRIMP U-Pb dating of magmatic zirconolite (CaZrTi2O7) in the Golden Mile Dolerite from the Mt Charlotte gold deposit (Yilgarn Craton, Australia), yielded the first robust emplacement age (2680 ± 9 Ma) for the principle host-rock of gold mineralization in the Kalgoorlie district. In contrast, co-magmatic zircon gave ages from ca. 2680 Ma to ca. 2170 Ma, reflecting isotopic resetting of high-U and -Th crystals. In situ SHRIMP analysis of hydrothermal xenotime (YPO4), which co-exists with gold in alteration pyrite, provided a Pb/Pb isochron age of 2655 ± 13 Ma. This date indicates that the youngest deposit in the Kalgoorlie district (Mt Charlotte) predates circa2.65 Ga, and provides a new minimum age for the structurally older Golden Mile deposit. Our results indicate that gold mineralization at Mt Charlotte is ~50 million years older than indicated by recent 40Ar/39Ar ages and places new constraints on the timing of late-stage regional faulting (D4) in the province.
AB - In situ SHRIMP U-Pb dating of magmatic zirconolite (CaZrTi2O7) in the Golden Mile Dolerite from the Mt Charlotte gold deposit (Yilgarn Craton, Australia), yielded the first robust emplacement age (2680 ± 9 Ma) for the principle host-rock of gold mineralization in the Kalgoorlie district. In contrast, co-magmatic zircon gave ages from ca. 2680 Ma to ca. 2170 Ma, reflecting isotopic resetting of high-U and -Th crystals. In situ SHRIMP analysis of hydrothermal xenotime (YPO4), which co-exists with gold in alteration pyrite, provided a Pb/Pb isochron age of 2655 ± 13 Ma. This date indicates that the youngest deposit in the Kalgoorlie district (Mt Charlotte) predates circa2.65 Ga, and provides a new minimum age for the structurally older Golden Mile deposit. Our results indicate that gold mineralization at Mt Charlotte is ~50 million years older than indicated by recent 40Ar/39Ar ages and places new constraints on the timing of late-stage regional faulting (D4) in the province.
KW - Zirconolite, Xenotime, U–Pb dating, SHRIMP, Gold mineralization, Yilgarn Craton
U2 - 10.1007/s00410-008-0352-7
DO - 10.1007/s00410-008-0352-7
M3 - Article
SN - 0010-7999
VL - 157
SP - 559
EP - 572
JO - Contributions to Mineralogy and Petrology
JF - Contributions to Mineralogy and Petrology
ER -