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Journal of the Geological Society ; 5 : — Seven centimetre-thick volcanic ash-fall layers interbedded within the thick Carboniferous successions of the Cantabrian Zone in northern Spain were dated by U—Pb zircon laser ablation inductively coupled plasma mass spectrometry across an interval ranging from Visean to Kasimovian, thus covering most of the Carboniferous period. All these ash layers occur in fossiliferous successions, allowing us to insert the radiometric data within a well-constrained biostratigraphic framework.
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We compare these materials with existing rutiles used already R19 and R10; and and show that the measured Usingle bondPb compositions i. This makes possible a Usingle bondPb normalisation procedure not reliant upon a common Pb correction that results in a significant decrease in the uncertainty contribution from the common Pb correction and better reproducibility of reference materials and unknowns for provenance analysis and other applications. Since rutile ages reflect mainly the time of cooling, rutile is a sensitive recorder of metamorphic thermochronological information and therefore is an excellent complement to detrital zircon UPb data.
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Geosciences Journal. We present new zircon U-Pb ages, Hf isotopes, and whole-rock geochemistry of the Xiaoxigong granite pluton in the Dunhuang block, northeastern Tarim Craton. Geochemical characteristics show that the granite belongs to the shoshonite series and has weakly peraluminous-metaluminous features.
Quantitative analyses can be obtained for most elements in the mass range amu practically 7 Li to U. Sample introduction to the ICP-MS system is setup for both liquid samples by nebulizer and solid material by laser ablation. The laboratory have a number of analytical procedures that are done routinely, which are listed below. We are always interested in developing new methods together with users of the laboratory, so please contact us to discuss your project.