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The Tribunal finds the Claimant’s reasons to wait to apply and the fact it took it upon himself to determine when that would be may have been good reasons not to apply, however they are not in accordance with the jurisprudence and are not considered good cause.
He stated he contacted Service Canada to confirm that the monies would be allocated based on his normal weekly earnings and to file when the severance ended which he calculated this period to be around the end of June.
(3) Rb/Sr on Precambrian shales: In Figure 2 we show the age calculated from the Rb–Sr isotopic ratios of two black shales.
The analyses consist of 90 x 75 μm laser spots along a single lamination with the calculated ages being in agreement with other dating methods.
 In the case of Albrecht the claimant’s ignorance of the law constituted good cause, however the Tribunal does not see how the reason of ignorance of the law can be justified and applied in this case.
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87Rb and 87Sr) followed by reaction with N2O to produce 87Sr16O at a mass of 103 amu allowing it to be distiguished from 87Rb. Rb–Sr isochron for the Barney Creek Formation (Left) and the Artic Bay Formation (Right).
In both cases 90 analyses were performed to define the isochron.
New developments in in-situ dating of shales: Rb–Sr via LA–QQQ–ICP–MS ARC Mc Arthur Basin Linkage Team (1) Introduction: 87 87 The Rb–Sr dating technique, based on the radiactive decay of Rb to Sr, is a well established technique.
87 87 (2) LA–QQQ–ICP–MS: Laser ablation–triple quad–inductively coupled plasma– 87 87 mass spectometry allows us to separate Rb from Sr within the mass spectometer (Fig. This allows us to produce abundant in-situ data at low cost.
(3) Application to the Precambrian: A persistent problem in Precambrian sedimentary successions is that due to a lack of a fossil record, biostratigraphic correlations and age determinations are imprecise and uncertain.
The significantly smaller error for the Artic Bay Formaion (Right) is due to a fully constrained initial 87Sr/86Sr ratio (y-intercept).
Acknowlegements: This work is supported by the Australian Research Council, University of Adelaide, Northern Territory Geological Survey, University of Wollongong, University of South Australia, Czech Academy of Sciences, Santos and Origin Energy.