Standard ICP element analysis @ AAC

These dolerites, which are characterized by a within-plate tholeiite geochemical signature, are organized in several dense swarms across the belt. Their geochemical compositions are homogeneous although they intrude a large geographical area subdivided into several domains each characterized by different tectonic-metamorphic settings. Although the closure temperature of apatite is lower than the emplacement temperature of the magma, physical models show that the time needed to solidify and cool these mafic dikes and sills below the apatite closure temperature is basically of the order of years or less. Consequently, the U-Pb dates obtained on apatite can be interpreted as the emplacement ages for these mafic intrusions. Our results demonstrate that, in all cases, the apatite grains do carry enough radiogenic Pb to be dated by in situ U-Pb analyses and yield a Pb-corrected mean age of These results reveal the existence of a major and short-lived magmatic event in the Variscan belt of Brittany during the Devonian-Carboniferous transition, a feature further highlighted by field evidence. Geophysical Journal International, , — Aldrich, L. Derry, Ed.

INVITATION

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Skip to search form Skip to main content You are currently offline. Some features of the site may not work correctly. DOI: Conventional dating of molybdenite ReOs provides one of few options for direct dating of sulfide mineralization. Unfortunately, in situ dating of molybdenite is considered unreliable due to intra-granular decoupling of ReOs.

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All publications more feeds DOI: BibTeX file. This included the construction of a low-volume sample cell and the establishment of a data reduction routine.

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Thank you for visiting nature. You are using a browser version with limited support for CSS. To obtain the best experience, we recommend you use a more up to date browser or turn off compatibility mode in Internet Explorer. In the meantime, to ensure continued support, we are displaying the site without styles and JavaScript. A Nature Research Journal. Establishing temporal constraints of faulting is of importance for tectonic and seismicity reconstructions and predictions.

Conventional fault dating techniques commonly use bulk samples of syn-kinematic illite and other K-bearing minerals in fault gouges, which results in mixed ages of repeatedly reactivated faults as well as grain-size dependent age variations. Here we present a new approach to resolve fault reactivation histories by applying high-spatial resolution Rb-Sr dating to fine-grained mineral slickenfibres in faults occurring in Paleoproterozoic crystalline rocks.

U-Pb dating of zircon by laser ablation ICP-MS: recent improvements and new insights

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It was revealed that the simultaneous U—Pb and U—Th zircon dating technique using LA-ICP-MS is easy to apply and is useful for Quaternary tephras in that it can give age information on the tephra itself and xenocrystic zircons in a quick and cost-effective manner. The double dating technique employed here has the merit that zircons yielding Quaternary U—Pb ages can be immediately cross-checked by the U—Th method.

It was revealed that the simultaneous U-Pb and U-Th zircon dating technique using LA-ICP-MS is easy to apply and is useful for Quaternary tephras in that it can give age information on the tephra itself and xenocrystic zircons in a quick and cost-effective manner. The double dating technique employed here has the merit that zircons yielding Quaternary U-Pb ages can be immediately cross-checked by the U-Th method.

Published by Elsevier B. Few attempts have been performed on dating zircons using U-Pb and U-Th methods simultaneously, although there are essentially no technical barriers. Bacon et al. This means that both methods can validate each other especially when dated simultaneously.

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In this work, a novel method for high spatial resolution U-Pb dating of zircon by laser ablation In quest of enhancing the analytical sensitivity of LA-ICP-MS, high laser ablation Published online May doi: //​.

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