Microstructurally controlled trace element (Zr, U–Pb) concentrations in metamorphic rutile: An example from the amphibolites of the Bergen Arcs-Reference-Cited by-同舟云学术

Microstructurally controlled trace element (Zr, U–Pb) concentrations in metamorphic rutile: An example from the amphibolites of the Bergen Arcs

Published:2019-11-25 Issue:1 Volume:38 Page:103-127
ISSN:0263-4929
Container-title:Journal of Metamorphic Geology
language:en
Short-container-title:J Metamorph Geol

Author:

Moore Jo¹^ORCID,Beinlich Andreas¹^ORCID,Porter Jennifer K.¹²,Talavera Cristina²³^ORCID,Berndt Jasper⁴,Piazolo Sandra⁵^ORCID,Austrheim Håkon⁶^ORCID,Putnis Andrew¹⁴^ORCID

Affiliation:

1. The Institute for Geoscience Research (TIGeR) School of Earth and Planetary Sciences Curtin University Perth WA Australia

2. John de Laeter Centre Curtin University Perth WA Australia

3. School of Geosciences University of Edinburgh Edinburgh UK

4. Institut für Mineralogie University of Münster Münster Germany

5. School of Earth and Environment University of Leeds Leeds UK

6. Department of Geosciences Physics of Geological Processes (PGP) The Njord Centre University of Oslo Oslo Norway

Funder

Australian Research Council

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/jmg.12514

Reference114 articles.

1. Rutile solubility in H2O, H2O–SiO2, and H2O–NaAlSi3O8 fluids at 0.7–2.0 GPa and 700–1000 °C: Implications for mobility of nominally insoluble elements

2. The plastic deformation of titanium dioxide single crystals

3. Eclogitization of lower crustal granulites by fluid migration through shear zones

4. Fluid controlled eclogitization of granulites in deep crustal shear zones, Bergen arcs, Western Norway

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