Next Article in Journal
Analysis of QualitySpec Trek Reflectance from Vertical Profiles of Taiga Snowpack
Next Article in Special Issue
Precious Metal Enrichment at the Myra Falls VMS Deposit, British Columbia, Canada
Previous Article in Journal
Holocene Soil Evolution in South Siberia Based on Phytolith Records and Genetic Soil Analysis (Russia)
Previous Article in Special Issue
A New Occurrence of Terrestrial Native Iron in the Earth’s Surface: The Ilia Thermogenic Travertine Case, Northwestern Euboea, Greece
 
 
Font Type:
Arial Georgia Verdana
Font Size:
Aa Aa Aa
Line Spacing:
Column Width:
Background:
Correction

Correction: Patrick Nadoll et al. REY and Trace Element Chemistry of Fluorite from Post-Variscan Hydrothermal Veins in Paleozoic Units of the North German Basin. Geosciences, 2018, 8, 283

1
GeoZentrum Nordbayern, Friedrich-Alexander-University Erlangen-Nuremberg, Schlossgarten 5, 91054 Erlangen, Germany
2
Geowissenschaftliches Zentrum der Universität Göttingen, Goldschmidtstrasse 1-3, 37077 Göttingen, Germany
3
Department of Physics and Earth Sciences, Jacobs University Bremen, Campus Ring 1, 28759 Bremen, Germany
4
GFZ, German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany
*
Author to whom correspondence should be addressed.
Geosciences 2018, 8(11), 403; https://doi.org/10.3390/geosciences8110403
Submission received: 1 November 2018 / Accepted: 1 November 2018 / Published: 5 November 2018
(This article belongs to the Special Issue Magmatic-Hydrothermal Ore Deposits)
The authors would like to correct the published article [1]:
On page 22 and page 23, Figures 9 and 10 should be changed from:
Figure 9. Tb/La versus Tb/Ca atomic ratio diagram after Möller et al. [33] for fluorite from the ABB, LSB, Biwender Vein (Harz), and Flechtingen High. For reference, fields compiled and established by Makin et al. [28], Duschl et al. [11], and Kraemer et al. [43]—North Pennine Ore Field (NPO), Alston Block (A) and Askrigg Block (B) are plotted. Labels, groupings and colours in the diagram (e.g., AI, Sohle 3) correspond to sample populations shown in Figures 4 and 5. See text for discussion.
Figure 9. Tb/La versus Tb/Ca atomic ratio diagram after Möller et al. [33] for fluorite from the ABB, LSB, Biwender Vein (Harz), and Flechtingen High. For reference, fields compiled and established by Makin et al. [28], Duschl et al. [11], and Kraemer et al. [43]—North Pennine Ore Field (NPO), Alston Block (A) and Askrigg Block (B) are plotted. Labels, groupings and colours in the diagram (e.g., AI, Sohle 3) correspond to sample populations shown in Figures 4 and 5. See text for discussion.
Geosciences 08 00403 g001aGeosciences 08 00403 g001b
Figure 10. La/Ho versus Y/Ho plot for a selection of fluorite samples from the ABB and the Flechtingen High. The grouping and colours correspond to those in Figure 5. See text for discussion.
Figure 10. La/Ho versus Y/Ho plot for a selection of fluorite samples from the ABB and the Flechtingen High. The grouping and colours correspond to those in Figure 5. See text for discussion.
Geosciences 08 00403 g002
To the following correct version:
Figure 9. Tb/La versus Tb/Ca atomic ratio diagram after Möller et al. [33] for fluorite from the ABB, LSB, Biwender Vein (Harz), and Flechtingen High. For reference, fields compiled and established by Makin et al. [28], Duschl et al. [11], and Kraemer et al. [43]—North Pennine Ore Field (NPO), Alston Block (A) and Askrigg Block (B) are plotted. Labels, groupings and colours in the diagram (e.g., AI, Sohle 3) correspond to sample populations shown in Figures 4 and 5. See text for discussion.
Figure 9. Tb/La versus Tb/Ca atomic ratio diagram after Möller et al. [33] for fluorite from the ABB, LSB, Biwender Vein (Harz), and Flechtingen High. For reference, fields compiled and established by Makin et al. [28], Duschl et al. [11], and Kraemer et al. [43]—North Pennine Ore Field (NPO), Alston Block (A) and Askrigg Block (B) are plotted. Labels, groupings and colours in the diagram (e.g., AI, Sohle 3) correspond to sample populations shown in Figures 4 and 5. See text for discussion.
Geosciences 08 00403 g003
Figure 10. La/Ho versus Y/Ho plot for a selection of fluorite samples from the ABB and the Flechtingen High. The grouping and colours correspond to those in Figure 5. See text for discussion.
Figure 10. La/Ho versus Y/Ho plot for a selection of fluorite samples from the ABB and the Flechtingen High. The grouping and colours correspond to those in Figure 5. See text for discussion.
Geosciences 08 00403 g004
On page 2 the 1.2 headline should be changed from:
  • 1.2. Fluorite (Ca2F) Geochemistry
  • To the following correct version:
  • 1.2. Fluorite (CaF2) Geochemistry
The authors apologize for any inconvenience this has caused to the readers. The changes do not affect the scientific results of this paper. The manuscript will be updated, and the original version will remain online on the article webpage, with a reference to this Correction.

References

  1. Nadoll, P.; Rehm, M.; Duschl, F.; Klemd, R.; Kraemer, D.; Sośnicka, M. REY and Trace Element Chemistry of Fluorite from Post-Variscan Hydrothermal Veins in Paleozoic Units of the North German Basin. Geosciences 2018, 8, 283. [Google Scholar] [CrossRef]

Share and Cite

MDPI and ACS Style

Nadoll, P.; Rehm, M.; Duschl, F.; Klemd, R.; Kraemer, D.; Sośnicka, M. Correction: Patrick Nadoll et al. REY and Trace Element Chemistry of Fluorite from Post-Variscan Hydrothermal Veins in Paleozoic Units of the North German Basin. Geosciences, 2018, 8, 283. Geosciences 2018, 8, 403. https://doi.org/10.3390/geosciences8110403

AMA Style

Nadoll P, Rehm M, Duschl F, Klemd R, Kraemer D, Sośnicka M. Correction: Patrick Nadoll et al. REY and Trace Element Chemistry of Fluorite from Post-Variscan Hydrothermal Veins in Paleozoic Units of the North German Basin. Geosciences, 2018, 8, 283. Geosciences. 2018; 8(11):403. https://doi.org/10.3390/geosciences8110403

Chicago/Turabian Style

Nadoll, Patrick, Meike Rehm, Florian Duschl, Reiner Klemd, Dennis Kraemer, and Marta Sośnicka. 2018. "Correction: Patrick Nadoll et al. REY and Trace Element Chemistry of Fluorite from Post-Variscan Hydrothermal Veins in Paleozoic Units of the North German Basin. Geosciences, 2018, 8, 283" Geosciences 8, no. 11: 403. https://doi.org/10.3390/geosciences8110403

Note that from the first issue of 2016, this journal uses article numbers instead of page numbers. See further details here.

Article Metrics

Back to TopTop