Role of fluids in transport and fractionation of uranium and thorium in magmatic processes
- 1 December 1990
- journal article
- Published by Springer Nature in Nature
- Vol. 348 (6301) , 531-533
- https://doi.org/10.1038/348531a0
Abstract
No abstract availableThis publication has 19 references indexed in Scilit:
- Ra-Th disequilibria systematics: Timescale of carbonatite magma formation at Oldoinyo Lengai volcano, TanzaniaPublished by Elsevier ,2003
- Pb-isotopic evidence for U-Th-Pb behaviour in a prograde amphibolite to granulite fades transition from the Lewisian complex of north-west Scotland: Implications for Pb-Pb datingGeochimica et Cosmochimica Acta, 1989
- UThRa radioactive disequilibria and magmatic processesEarth and Planetary Science Letters, 1988
- Residence time of thorium, uranium and lead in the mantle with implications for mantle convectionNature, 1985
- The behavior of 232Th and the 238U decay chain nuclides during magma formation and volcanismGeochimica et Cosmochimica Acta, 1984
- Comparison of 230Th-238U disequilibrium systematics in lavas from three hot spot regions: Hawaii, Prince Edward and SamoaGeochimica et Cosmochimica Acta, 1984
- Sodic granitoids and felsic gneisses associated with uranium-thorium mineralisation, Crockers Well, South AustraliaMineralium Deposita, 1984
- K, U and Th in mid-ocean ridge basalt glasses and heat production, K/U and K/Rb in the mantleNature, 1983
- Uranium mineralization and granite magmatism in the British IslesPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1979
- Uranium in South Africa and South West Africa (Namibia)Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1979