TL;DR: In this paper, a cross-calibration of U-Pb and Lu-Hf isotopic systems on mineral fractions from the Proterozoic Karlshamn and Sorkka dolerites in Sweden and Finland is presented.
TL;DR: In this paper, a combined method of simultaneously measuring U-Pb and Lu-Hf isotopes as well as trace elements in Phalaborwa baddeleyite and 91500, GJ-1, TEMORA-1 and SK10-2 zircons was described.
Abstract: This paper describes a combined method of simultaneously measuring U-Pb and Lu-Hf isotopes as well as trace elements in Phalaborwa baddeleyite and 91500, GJ-1, TEMORA-1 and SK10-2 zircons by means of Neptune MC-ICPMS and Agilent Q-ICPMS connected to a 193 nm excimer laser ablation system. Material ablated by laser was carried in different proportions into Q-ICPMS for U-Pb isotopic and trace elemental and MC-ICPMS for Lu-Hf isotopic compositions. Experiments indicate that different proportions of ablated material for the Q-ICPMS and MC-ICPMS (6:4, 5:5 and 4:6 respectively) do not show any bias for the zircon/baddeleyite U-Pb age, Lu-Hf isotope and trace elemental compositions within analytical errors. Using 40―60 μm spot size, the obtained U-Pb ages of Phalaborwa baddeleyite, 91500, GJ-1, TEMORA and SK10-2 zircons are 2065±15 (2 σ , n =20), 1063±6 (2 σ , n =19), 613±6 (2 σ , n =20), 416±5 (2 σ , n =20) and 32.6±0.5 (2 σ , n =20) Ma, respectively. The 176 Hf/ 177 Hf ratios are 0.281231±24 (2SD, n =20), 0.282310±35 (2SD, n =19), 0.282028±34 (2SD, n =20), 0.282687±34 (2SD, n =20) and 0.282752±53 (2SD, n =20), respectively. The obtained trace elemental compositions are identical to the reference values. Therefore, this kind of technique makes it possible to simultaneously obtain the U-Pb age, Lu-Hf isotopes and trace elemental compositions of zircon and baddeleyite, which could be an important tool in solving problems in earth sciences.
TL;DR: In this article, the ages of the lowermost unit (251.7 9 0.4 Ma) and near-uppermost unit(251.1 9 0 3 Ma) of the Siberian flood-volcanic event were obtained for the Maymecha-Kotuy area, Russia.
TL;DR: Baddeleyite is an ideal mineral for U-Pb dating because it has abundant U (up to 3000 ppm), negligible initial common Pb, rarely occurs as xenocrysts, and, in unmetamorphosed samples, experiences negligible Pb loss as discussed by the authors.