Results 191 to 200 of about 4,931 (238)
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Geochimica et Cosmochimica Acta, 2018
Understanding the physical basics of tectonic events, related fluid flow and ore deposition represents one of the great challenges in modern geosciences.
B. Walter +6 more
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Understanding the physical basics of tectonic events, related fluid flow and ore deposition represents one of the great challenges in modern geosciences.
B. Walter +6 more
semanticscholar +1 more source
U–Pb geochronology of the Coldwell Complex, northwestern Ontario, Canada
Canadian Journal of Earth Sciences, 1985The Coldwell Complex gives a U–Pb zircon age of 1188 ± 56 Ma, a U–Pb tritomite age of 1126 ± 6 Ma, and a Pb–Pb potash feldspar age of 1139 ± 55 Ma. These ages are all significantly older than the previously published Rb–Sr and K–Ar ages. We interpret these ages as follows: (1) emplacement of the complex at 1188 Ma as part of the initial stages of the ...
A. Turek +2 more
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Alpha-recoil in U?Pb geochronology: effective sample size matters
Contributions to Mineralogy and Petrology, 2003Displacement of the daughter isotope by α-recoil results in an open system on the nanoscale. For a heterogeneous distribution of U and Th, this redistribution of intermediate and stable daughter isotopes results in subvolumes with a deficit of Pb and others with an excess of Pb.
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An improved micro-capsule for zircon dissolution in UPb geochronology
Chemical Geology: Isotope Geoscience section, 1987A new design of Teflon® micro-capsule for mineral dissolution is described which offers advantages over the conventional Krogh vessel for use in zircon UPb geochronology. The TFE Teflon® capsules have friction-fit caps and are intended to reside inside a larger Teflon® pressure vessel.
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In-situ U Pb geochronology of vesuvianite in skarn deposits
Chemical Geology, 2022Yu Zhang +11 more
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TEMORA 1: a new zircon standard for Phanerozoic U–Pb geochronology
, 2003L. P. Black +6 more
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High-Precision U-Pb Zircon Geochronology and the Stratigraphic Record
Reviews in Mineralogy and Geochemistry, 2003The rock stratigraphic record exists as a rich, albeit complex and incomplete repository of Earth history, tracing the processes of biological evolution, climate change, oceanic and atmospheric chemistry, sea-level fluctuations, mountain-building and erosion, and basin subsidence. Without a detailed and precise temporal framework, however, the richness
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Hf isotopic compositions of the standard zircons and baddeleyites used in U–Pb geochronology
, 2006Fu-Yuan Wu +4 more
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Towards a more accurate U–Pb geochronology
Chemical Geology, 2001Desmond E Moser, David J Scott
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