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- W2463848016 abstract "Ventersdorp-age dolerite intrusions cutting the Witwatersrand Group quartzites have mantle δ 18 O values, of between 5,5 and 6,7‰. This is consistent with their not having exchanged oxygen since intrusion. These dolerites were intruded before the peak of metamorphism of the Witwatersrand Basin and are now almost completely recrystallized to lower-greenschist facies minerals. The δ 18 O values of the Witwatersrand quartzites analysed range from 8,6 to 10,3‰. Connate water released from the sediments during metamorphism at ca 350 o C could have exchanged with the intrusions with very high water/rock ratios without changing of δ 18 O values of the intrusions. Whole rock oxygen isotope data cannot, therefore, constrain the amont of fluid exchange which has affected the Witwatersrand Basin during metamorphism" @default.
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- W2463848016 date "1990-08-01" @default.
- W2463848016 modified "2023-09-23" @default.
- W2463848016 title "Fluid interaction in the Witwatersrand goldfields; oxygen isotope geochemistry of Ventersdorp-age dolerite intrusions" @default.
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