Solid Earth
Solid Earth
SE
Articles | Volume 8, issue 4
Articles | Volume 8, issue 4
https://doi.org/10.5194/se-8-789-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/se-8-789-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Articles | Volume 8, issue 4
Research article
 | 
25 Jul 2017
Research article |  | 25 Jul 2017

Interpretation of zircon coronae textures from metapelitic granulites of the Ivrea–Verbano Zone, northern Italy: two-stage decomposition of Fe–Ti oxides

Elizaveta Kovaleva, Håkon O. Austrheim, and Urs S. Klötzli

Viewed

Total article views: 2,529 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,360 1,001 168 2,529 498 153 154
  • HTML: 1,360
  • PDF: 1,001
  • XML: 168
  • Total: 2,529
  • Supplement: 498
  • BibTeX: 153
  • EndNote: 154
Views and downloads (calculated since 16 May 2017)
Cumulative views and downloads (calculated since 16 May 2017)

Viewed (geographical distribution)

Total article views: 2,529 (including HTML, PDF, and XML) Thereof 2,274 with geography defined and 255 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (preprint)

Latest update: 14 Dec 2024
Download
Short summary
This is a study of unusual coronae textures formed by zircon in granulitic metapelites, Ivrea–Verbano Zone (northern Italy). Zircon coronas occur in two generations: (1) thick (5–20 µm) crescent-shaped aggregates and (2) thin (≤ 1 µm) thread-shaped and tangled coronae. Both are found in the same petrological context, so that the difference between two generations is very conspicuous. Formation of zircon coronae is attributed to the two-stage decomposition of Fe–Ti oxides, a rich source of Zr.
Read more