Detecting Micro- and Nanoscale Variations in Element Mobility in High-Grade Metamorphic Rocks-Reference-Cited by-同舟云学术

Detecting Micro- and Nanoscale Variations in Element Mobility in High-Grade Metamorphic Rocks

Published:2017-12-01 Issue: Volume: Page:277-291
ISSN:2328-8779
Container-title:Microstructural Geochronology
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Author:

Kusiak Monika A.¹²,Wilde Simon A.³,Wirth Richard²,Whitehouse Martin J.⁴,Dunkley Daniel J.¹³,Lyon Ian⁵,Reddy Steven M.⁶⁷,Berry Andrew⁸,de Jonge Martin⁹

Affiliation:

1. Institute of Geological Sciences; Polish Academy of Sciences; Warsaw Poland

2. GeoForschungsZentrum, Section 4.3 Chemistry and Physics of Earth Materials; Potsdam Germany

3. Department of Applied Geology; Curtin University; Perth Australia

4. Swedish Museum of Natural History; Stockholm Sweden

5. School of Earth, Atmospheric and Environmental Sciences; University of Manchester; Manchester UK

6. School of Earth and Planetary Sciences; Curtin University; Perth Western Australia Australia

7. Geoscience Atom Probe; Advanced Resource Characterisation Facility Curtin University; Perth Australia

8. Research School of Earth Sciences; Australian National University; Canberra Australia

9. Australian Synchrotron; Australian Nuclear Science and Technology Organisation; Australia

Publisher

John Wiley & Sons, Inc.

Reference71 articles.

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3. Trace element signature and U-Pb geochronology of eclogite-facies zircon, Bergen Arcs, Caledonides of W Norway;Bingen;Contrib. Mineral. Petrol.,2004

4. 4 Zircon ages from one rock - The history of a 3930 Ma-old granulite from Mount Sones, Enderby Land, Antarctica;Black;Contrib. Mineral. Petrol.,1986

5. The difficulties of dating mafic dykes - An Antarctic example;Black;Contrib. Mineral. Petrol.,1991

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