THREE NATURAL ZIRCON STANDARDS FOR U‐TH‐PB, LU‐HF, TRACE ELEMENT AND REE ANALYSES

Wiley - Tập 19 Số 1 - Trang 1-23 - 1995
Michael Wiedenbeck1, Paul Allé1, Fernando Corfú2, William L. Griffin3, M. Meier4, Felix Oberli4, Albrecht von Quadt4, J C Roddick5, Wolfgang Spiegel6
1CNRS, Centre de Recherches Pétrographiques et Géochimiques B.P. 20, 54501 Vandoeuvre-lès-Nancy Cedex, France
2Department of Geology, Royal Ontario Museum, 100 Queen's Park, Toronto, Ontario M5S 2C6, Canada
3CSIRO, Division of Mineral Physics, PO box 136, North Ryde, NSW, 2113, Australia
4Institut für Isotopengeologie und Mineralische Rohstoffe, ETH-Zentrum, CH - 8092 Zürich, Switzerland
5Geological Survey of Canada, 601 Booth St., Ottawa, Ontario, K1A 0E8, Canada
6Institut für Angewandte Mineralogie und Geochemie, Technische Universität München, Lichtenbergstraße 4, D ‐ 8046 Garching bei München, Germany

Tóm tắt

We report here the results of a study to develop natural zircon geochemical standards for calibrating the U‐(Th)‐Pb geochronometer and Hf isotopic analyses. Additional data were also collected for the major, minor and trace element contents of the three selected sample sets. A total of five large zircon grains (masses between 0.5 and 238 g) were selected for this study, representing three different suites of zircons with ages of 1065 Ma, 2.5 Ma and 0.9 Ma. Geochemical laboratories can obtain these materials by contacting Geostandards Newsletter.

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