Hernández-Mendiola, E.Bernal, Juan PabloLounejeva, E.Mortimer, GrahamMcCulloch, Malcolm Thomas2015-12-101871-1014http://hdl.handle.net/1885/52745We describe an analytical methodology to quantify238U-234U and230Th using isotope-dilution systematics and inductively coupled plasma-quadrupole mass spectrometry (ICP-QMS) for geochronological purposes. This required characterization of the mass spectrometer detector performance over a large dynamic range, including a careful calibration between pulse and analogue ion-counting modes. Our methodology gives an analytical precision for234U/238U and230Th/238U of 4‰ and 7‰ (2 × standard error), respectively, and yields230Th-ages with 4-5% uncertainty from 500 ng of238U. We tested our methodology by analyzing carbonate samples (corals and speleothems) which were previously dated using MC-ICPMS; excellent agreement between both techniques was obtained. Our results indicate that ICP-QMS is suitable to obtain valuable meaningful geochronological data, but it is limited to dating samples older than 1 ka, and younger than 400 ka. Our methodology thus represents an attractive alternative to obtain geochonological data to select the most interesting samples prior to high-precision analysis. Moreover, such data would also valuable to build preliminary age-models, which can be further complemented with high-precision analyses.Keywords: carbonate rock; coral; geochronology; inductively coupled plasma method; speleothem; uranium series dating; Anthozoa Corals; ICP-QMS; Speleothems; U-series dating201110.1016/j.quageo.2011.09.0012016-02-24