Correction to: Ion microprobe dating of fissure monazite in the Western Alps: insights from the Argentera Massif and the
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Swiss Journal of Geosciences
Open Access
CORRECTION
Correction to: Ion microprobe dating of fissure monazite in the Western Alps: insights from the Argentera Massif and the Piemontais and Briançonnais Zones Emmanuelle Ricchi1* , Edwin Gnos2, Daniela Rubatto3,4, Martin John Whitehouse5 and Thomas Pettke3
Correction to: Swiss Journal of Geosciences (2020) 113:15 https://doi.org/10.1186/s00015-020-00365 -3
Following publication of the original article (Ricchi et al. 2020), multiple typesetting errors were identified in the article. The updated sections/sentences are given below and the changes have been highlighted in bold typeface. Keywords 208
Pb/232Th fissure monazite age, Western Alps, High pressure, Argentera Massif, Tectonic activity, Hydrothermal monazite chemistry. Introduction In monazite-bearing fissures, quartz and adularia typically form at an early stage of fissure formation ( 1) were removed from the dataset. Top‑NNW thrusting (> 35 Ma) The oldest fissure monazite age of the Western Alps is recorded at ~ 36 Ma by BALZI2 grain from the Briançonnais Zone (Figs. 1 and 6) and is interpreted to be related to Late Eocene—earliest Oligocene top-NNW thrusting (episode (1); Table 2) which started at or before 38 Ma (Cardello et al. 2019). Acknowledgements
Editorial handling: Paola Manzotti. The original article can be found online at https://doi.org/10.1186/s0001 5-020-00365-3. *Correspondence: [email protected] 1 Department of Earth Sciences, University of Geneva, Rue des Maraîchers 13, 1205 Geneva, Switzerland Full list of author information is available at the end of the article
We thank Gaspare Maletto, Roberto Bracco and Francis Guichon for providing the samples and valuable information on the sample localities. We also thank Daniel Marty and Paola Manzotti for the editing work as well as Neil Mancktelow and an anonymous reviewer for their helpful comments.
© The Author(s) 2020. This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativeco mmons.org/licenses/by/4.0/.
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The original article (Ricchi et al. 2020) has been corrected and the Publisher apologises to the authors and the readers for the inconvenience caused by this typesetting error. Author details 1 Department of Earth Sciences, University of Geneva, Rue des Maraî
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