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Geochronology","{\"openalex\":\"W2489082161\",\"doi\":\"10.1016/b978-0-08-095975-7.00310-7\"}","2026-05-21T07:14:03.201256747","2026-05-21T07:14:14.211970677","doi","10.1016/b978-0-08-095975-7.00310-7","arxivId","openalexId","W2489082161","abstractText","publishedDate","2013-11-07","publishedYear",2013,"venue","Treatise on Geochemistry",296,"authors","keywords",[181,182,183],"pdfUrl","topVenue","Geological and Geochemical Analysis","Geochemistry and Geologic Mapping","Radioactive element chemistry and processing","paper_W2072107094","Evaluating uncertainties in the calibration of isotopic reference materials and multi-element isotopic tracers (EARTHTIME Tracer Calibration Part II)","{\"openalex\":\"W2072107094\",\"doi\":\"10.1016/j.gca.2015.02.040\"}","2026-05-20T12:39:28.237886388","2026-05-20T12:39:28.237754514","10.1016/j.gca.2015.02.040","W2072107094","2015-03-18",2015,"Geochimica et Cosmochimica Acta",332,[182,196,197],"Groundwater and Isotope Geochemistry","Radioactivity and Radon Measurements","paper_W2103651454","U–Pb systematics of the McClure Mountain syenite: thermochronological constraints on the age of the 40Ar/39Ar standard MMhb","{\"openalex\":\"W2103651454\",\"doi\":\"10.1007/s00410-006-0077-4\"}","2026-05-19T22:36:16.250613692","2026-05-19T22:36:16.250411987","10.1007/s00410-006-0077-4","W2103651454","2006-03-21",2006,"Contributions to Mineralogy and Petrology",374,[181,182,210],"earthquake and tectonic studies","paper_W2092678733","U-Pb dating of zircon in the Bishop Tuff at the millennial scale","{\"openalex\":\"W2092678733\",\"doi\":\"10.1130/g24017a.1\"}","2026-05-19T21:54:55.208618022","2026-05-19T21:54:55.20915132","10.1130/g24017a.1","W2092678733","Research Article| December 01, 2007 U-Pb dating of zircon in the Bishop Tuff at the millennial scale J.L. Crowley; J.L. Crowley 1Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA Search for other works by this author on: GSW Google Scholar B. Schoene; B. Schoene 1Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA Search for other works by this author on: GSW Google Scholar S.A. Bowring S.A. Bowring 1Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA Search for other works by this author on: GSW Google Scholar Author and Article Information J.L. Crowley 1Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA B. Schoene 1Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA S.A. Bowring 1Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA Publisher: Geological Society of America Received: 26 Apr 2007 Revision Received: 06 Aug 2007 Accepted: 09 Aug 2007 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 The Geological Society of America, Inc. Geology (2007) 35 (12): 1123–1126. https://doi.org/10.1130/G24017A.1 Article history Received: 26 Apr 2007 Revision Received: 06 Aug 2007 Accepted: 09 Aug 2007 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation J.L. Crowley, B. Schoene, S.A. Bowring; U-Pb dating of zircon in the Bishop Tuff at the millennial scale. Geology 2007;; 35 (12): 1123–1126. doi: https://doi.org/10.1130/G24017A.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Zircon from the Bishop Tuff (eastern California) was dated by the U-Pb isotope dilution thermal ionization mass spectrometry (ID-TIMS) method to evaluate time scales of magmatic evolution and applicability of the method to rocks younger than 1 Ma. The 206Pb/238U dates from 17 of 19 grains are equivalent with a weighted mean of 767.1 ± 0.9 ka that overlaps with the published 40Ar/39Ar sanidine age, requiring that most zircon crystallized immediately before eruption. Dates from two grains that are 6 and 12 k.y. older indicate minimum times that a small portion of the grains resided in the magma. These findings are consistent with chemical zoning patterns in zircon that suggest a relatively simple crystallization history, yet contrast with previous results of ion microprobe dating of zircon that show 50–80 k.y. of magma residence. The weighted mean 207Pb/235U date is ∼52 k.y. older than the 206Pb/238U date, a difference that is attributed to excess 207Pb from initial Pa/U disequilibrium. The results demonstrate that high-precision ID-TIMS geochronology can resolve magma chamber dynamics of <1 Ma silicic eruptions at the millennial scale. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.","2007-01-01",2007,"Geology",376,[181,224,182],"Geology and Paleoclimatology Research","paper_W1965913526","Statistical geochemistry reveals disruption in secular lithospheric evolution about 2.5 Gyr ago","{\"openalex\":\"W1965913526\",\"doi\":\"10.1038/nature11024\"}","2026-05-19T15:40:38.242696762","2026-05-19T15:42:28.183273137","10.1038/nature11024","W1965913526","2012-05-01",2012,"Nature",399,[181,182,210],"paper_W1669138304","Derivation of isotope ratios, errors, and error correlations for U‐Pb geochronology using ²⁰⁵Pb‐²³⁵U‐(²³³U)‐spiked isotope dilution thermal ionization mass spectrometric data","{\"openalex\":\"W1669138304\",\"doi\":\"10.1029/2006gc001492\"}","2026-05-16T05:07:30.212979266","2026-05-19T02:22:45.185895903","10.1029/2006gc001492","W1669138304","A comprehensive treatment of the derivation of U‐Pb isotope ratios and their corresponding uncertainties from isotope dilution thermal ionization mass spectrometric measurements is presented. Standard parametric statistical methods of error propagation are utilized to convolve uncertainties associated with instrumental mass fractionation, tracer subtraction, blank Pb and U subtraction, and initial common Pb correction. Derivations include errors and error correlations for total sample U/Pb and Pb isotope ratios (including radiogenic and initial common Pb) for two‐ and three‐dimensional isochron calculations, radiogenic U/Pb and Pb isotope ratios for concordia and radiogenic model age calculations, and the propagation of model age errors from radiogenic isotope ratios.","2007-08-01","Geochemistry Geophysics Geosystems",495,[182,181,183],"https://onlinelibrary.wiley.com/doi/pdfdirect/10.1029/2006GC001492",true,"paper_W1898112109","Metrology and traceability of U–Pb isotope dilution geochronology (EARTHTIME Tracer Calibration Part I)","{\"openalex\":\"W1898112109\",\"doi\":\"10.1016/j.gca.2015.05.026\"}","2026-05-16T02:34:13.203036019","2026-05-21T19:26:58.182314884","10.1016/j.gca.2015.05.026","W1898112109","Mixed 235U–233U–205Pb(–202Pb) tracers for U–Pb isotope-dilution isotope ratio mass spectrometry have been prepared under the auspices of the EARTHTIME Initiative. The methods and results for the preparation and calibration of the U/Pb ratio and isotopic abundances are given, and the various sources of uncertainty are discussed and quantified. The accuracy of the EARTHTIME U–Pb tracer isotopic composition can be traced back to SI units via a series of assay and isotopic composition reference materials combined with the experiments described herein. The parameters used in calculating U/Pb ratios (and inferentially U–Pb dates) have correlated uncertainties that result in a total uncertainty contribution to 206Pb/238U dates of ± < 0.03% (95% confidence). For suitable terrestrial materials such as zircon, when other sources of uncertainty have been minimised (e.g., open-system behaviour, 238U/235U variation, intermediate daughter product disequilibrium, common Pb, etc.) the U–Pb tracer calibration uncertainty is a limiting factor in the accuracy of U–Pb geochronology – but less so than the uncertainty in the 238U and 235U decay constants (±0.11 and 0.14% 2σ). The calibration approach of the mixed EARTHTIME 235U–233U–205Pb(–202Pb) tracers, in addition to updated values for reference materials (e.g., mixed gravimetric reference solutions), and parameters (e.g., Pb reference material assay), can be applied to other laboratory-specific U–Pb tracers and will facilitate the generation of accurate and directly inter-comparable U–Pb data.","2015-05-19",513,[181,183,182],"paper_W2047314228","Reassessing the uranium decay constants for geochronology using ID-TIMS U–Pb data","{\"openalex\":\"W2047314228\",\"doi\":\"10.1016/j.gca.2005.09.007\"}","2026-05-15T21:11:05.382972705","2026-05-21T16:03:00.293060548","10.1016/j.gca.2005.09.007","W2047314228","2005-11-04",2005,539,[181,182,210],"paper_W2342124398","Community‐Derived Standards for LA‐ICP‐MS U‐(Th‐)Pb Geochronology – Uncertainty Propagation, Age Interpretation and Data Reporting","{\"openalex\":\"W2342124398\",\"doi\":\"10.1111/j.1751-908x.2016.00379.x\"}","2026-05-14T14:56:37.409227052","2026-05-21T18:24:41.213959411","10.1111/j.1751-908x.2016.00379.x","W2342124398","The LA ‐ ICP ‐ MS U‐(Th‐)Pb geochronology international community has defined new standards for the determination of U‐(Th‐)Pb ages. A new workflow defines the appropriate propagation of uncertainties for these data, identifying random and systematic components. Only data with uncertainties relating to random error should be used in weighted mean calculations of population ages; uncertainty components for systematic errors are propagated after this stage, preventing their erroneous reduction. Following this improved uncertainty propagation protocol, data can be compared at different uncertainty levels to better resolve age differences. New reference values for commonly used zircon, monazite and titanite reference materials are defined (based on ID ‐ TIMS ) after removing corrections for common lead and the effects of excess 230 Th. These values more accurately reflect the material sampled during the determination of calibration factors by LA ‐ ICP ‐ MS analysis. Recommendations are made to graphically represent data only with uncertainty ellipses at 2 s and to submit or cite validation data with sample data when submitting data for publication. New data‐reporting standards are defined to help improve the peer‐review process. 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Blair Schoene 人物

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