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The accumulation of non-formula elements in zircons during weathering : Ancient zircons from the Jack Hills, Western Australia

Pidgeon, R. T. (författare)
Nemchin, A. A. (författare)
Roberts, M. P. (författare)
visa fler...
Whitehouse, Martin J., 1962- (författare)
Naturhistoriska riksmuseet,Enheten för geovetenskap,Nordsim
Bellucci, J. J. (författare)
Naturhistoriska riksmuseet,Enheten för geovetenskap
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 (creator_code:org_t)
2019
2019
Engelska.
Ingår i: Chemical Geology. - 0009-2541 .- 1872-6836. ; 530
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • In this contribution we describe the influx of non-formula elements (Fe, Ca, Al, Y, U and Th) into fractures and selected zone lamellae in zircons from Jack Hills during recent weathering and discuss the effects of this on overlapping SIMS U-Th-Pb and oxygen isotope analyses. Previous research has recognised the importance of fractures in the generation of anomalous U-Th-Pb and oxygen isotope systems. In this report we show that besides fractures specific zones in euhedrally zoned zircon can act as pathways for the influx of weathering solutions and contain a similar range of trace element materials as do the fractures. Whereas zero-age discordant U-Pb systems of Jack Hills zircons have been explained by many authors in terms of Pb loss, present results confirm conclusions of our previous study that the main discordance mechanism of Jack Hills zircons is U-Th gain, due to overlap of SIMS analyses with mineralized fractures and zone lamellae with excess weathering-fluid-deposited U and Th. We explain the anomalously light and heavy oxygen isotopes and significant OH in SIMS analyses that overlap fractures and mineralized zones as due to the presence in the fractures of Ca, Fe, Al oxides and hydroxides with complexly fractionated oxygen isotopic systems. There is a suggestion in some of the elemental maps that there has been minor dispersion of trace elements away from fractures. But SIMS U-Th-Pb and oxygen isotope analyses on parts of the zircon away from fractures and mineralized zones show no evidence of interaction with weathering-fluid, indicating that penetration of weathering fluids into the body of the zircon at the location of the SIMS spots has not occurred. Results of this study have implications for other SIMS U-Th-Pb and oxygen isotope studies of zircons from rocks that have been subjected to weathering and also for early TIMS U-Pb measurements of bulk zircon samples that show zero Ma U-Pb discordance.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geokemi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geochemistry (hsv//eng)

Nyckelord

Jack Hills
Weathering of zircons
Non-formula elements in zircon
Discordant U-Th-Pb ags
Oxygen isotopes and OH in zircon
Zircon fractures
The changing Earth
Den föränderliga jorden

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