Next Article in Journal
Precursor Ratio-Driven Morphological Evolution of CVD-Grown MoS2 Microstructures
Previous Article in Journal
Effect of the Grain-Refining of A356 Aluminum Alloy Closed-Cell Foams on the Mechanical Compression Properties
 
 
Font Type:
Arial Georgia Verdana
Font Size:
Aa Aa Aa
Line Spacing:
Column Width:
Background:
Correction

Correction: Cui et al. Gemological Study of Black Nephrite from Dahua, Guangxi Province, China. Crystals 2026, 16, 220

1
School of Gemology, China University of Geosciences Beijing, 29 Xueyuan Road, Beijing 100083, China
2
Sciences Institute, China University of Geosciences, 29 Xueyuan Road, Beijing 100083, China
3
Ningbo Customs District Technology Center, Ningbo 315192, China
*
Author to whom correspondence should be addressed.
Crystals 2026, 16(8), 479; https://doi.org/10.3390/cryst16080479
Submission received: 21 July 2026 / Accepted: 21 July 2026 / Published: 23 July 2026
Error in Table
In the original publication [1], there was a mistake in Table 3 as published. In the original Table 3, Row 17, Column 1, the phrase “the ion number of Fe” was inadvertently included and is redundant. The correct description should be “the sum of the ion numbers of Si, Al, and Ti”. This phrase has now been removed from the table. Accordingly, we request that Table 3 be replaced with the corrected version. The corrected Table 3 appears below. The authors state that the scientific conclusions are unaffected. This correction was approved by the Academic Editor. The original publication has also been updated.

Reference

  1. Cui, M.; He, M.; Yang, M.; Peng, B.; Wu, S. Gemological Study of Black Nephrite from Dahua, Guangxi Province, China. Crystals 2026, 16, 220. [Google Scholar] [CrossRef] [Scilit]
Table 3. Chemical composition of tremolite in samples (wt%).
Table 3. Chemical composition of tremolite in samples (wt%).
MY1-1MY1-2MY1-3MY1-4MY2-1MY2-2MY3-1MY3-2MY3-3MY4-1MY4-2MY4-3MY4-4MY4-5MY4-6
SiO256.7857.9757.5257.3957.3856.6157.3556.7455.4557.456.9660.5259.7559.7459.82
Al2O30.290.150.210.120.170.190.190.170.280.360.270.150.230.170.21
TiO20.030.070.040.020.060.090.010.030.050.02b.d.l.b.d.l.b.d.l.0.040.03
FeOt1.181.171.261.240.620.921.411.211.260.840.960.810.81.271.01
MnO0.30.410.370.290.530.470.520.510.350.580.610.440.570.590.6
MgO25.4624.6424.8325.1425.2125.1224.7825.5525.6825.3124.9624.1623.6823.8223.77
CaO13.1713.11313.6312.6312.7613.513.4813.4311.912.6411.0411.0811.4611.05
Na2O0.030.080.080.060.040.060.030.030.030.040.040.020.040.040.03
K2O0.020.020.040.010.020.020.01b.d.l.0.030.030.010.020.030.010.01
Cr2O3b.d.l.b.d.l.0.050.01b.d.l.b.d.l.b.d.l.0.02b.d.l.b.d.l.0.010.01n.dn.dn.d
NiO0.04b.d.l.b.d.l.0.01b.d.l.0.020.02b.d.l.0.010.01b.d.l.b.d.l.0.04b.d.l.0.07
Total…97.3197.6197.3997.996.6696.2597.8197.7396.5696.4896.4597.1796.2197.1496.6
Si7.773 7.815 7.854 7.813 7.877 7.823 7.819 7.752 7.679 7.880 7.849 8.143 8.133 8.068 8.111
Al0.047 0.024 0.033 0.018 0.028 0.031 0.030 0.027 0.046 0.058 0.044 0.024 0.037 0.027 0.033
Ti0.004 0.007 0.004 0.002 0.007 0.009 0.001 0.003 0.005 0.002 b.d.l.b.d.l.b.d.l.0.004 0.003
Mn0.035 0.047 0.042 0.033 0.062 0.055 0.059 0.058 0.041 0.067 0.071 0.050 0.065 0.067 0.069
Mg5.197 4.951 5.053 5.101 5.159 5.174 5.037 5.204 5.302 5.180 5.126 4.847 4.805 4.795 4.805
Ca1.932 1.891 1.902 1.987 1.857 1.889 1.971 1.974 1.993 1.749 1.866 1.591 1.616 1.658 1.605
Na0.008 0.022 0.021 0.015 0.009 0.015 0.007 0.007 0.009 0.010 0.009 0.005 0.010 0.010 0.008
K0.004 0.003 0.006 0.001 0.004 0.003 0.002 0.000 0.005 0.005 0.001 0.004 0.006 0.002 0.002
Crb.d.l.b.d.l.0.006 0.001 b.d.l.b.d.l.b.d.l.0.002 b.d.l.b.d.l.0.002 0.001 n.dn.dn.d
Ni0.004 b.d.l.b.d.l.0.001 b.d.l.0.002 0.002 b.d.l.0.001 0.001 b.d.l.b.d.l.0.004 b.d.l.0.008
Fe3+0.135 0.220 0.144 0.141 0.071 0.106 0.161 0.138 0.146 0.097 0.111 b.d.l.b.d.l.b.d.l.b.d.l.
Fe2+b.d.l.0.045 b.d.l.b.d.l. b.d.l.b.d.l.b.d.l.b.d.l.b.d.l.b.d.l.b.d.l.0.091 0.091 0.144 0.115
Mg/(Mg + Fe2+)10.991111111110.980.980.970.98
MineralsTrTrTrTrTrTrTrTrTrTrTrTrTrTrTr
Notes: The tremolite formulae were calculated on the basis of 23 oxygens. Tr = tremolite. FeOt: FeO + Fe2O3. Fe3+ contents were estimated based on the charge balance. b.d.l., below the detected line.
Disclaimer/Publisher’s Note: The statements, opinions and data contained in all publications are solely those of the individual author(s) and contributor(s) and not of MDPI and/or the editor(s). MDPI and/or the editor(s) disclaim responsibility for any injury to people or property resulting from any ideas, methods, instructions or products referred to in the content.

Share and Cite

MDPI and ACS Style

Cui, M.; He, M.; Yang, M.; Peng, B.; Wu, S. Correction: Cui et al. Gemological Study of Black Nephrite from Dahua, Guangxi Province, China. Crystals 2026, 16, 220. Crystals 2026, 16, 479. https://doi.org/10.3390/cryst16080479

AMA Style

Cui M, He M, Yang M, Peng B, Wu S. Correction: Cui et al. Gemological Study of Black Nephrite from Dahua, Guangxi Province, China. Crystals 2026, 16, 220. Crystals. 2026; 16(8):479. https://doi.org/10.3390/cryst16080479

Chicago/Turabian Style

Cui, Mingying, Mingyue He, Mei Yang, Bijie Peng, and Shaokun Wu. 2026. "Correction: Cui et al. Gemological Study of Black Nephrite from Dahua, Guangxi Province, China. Crystals 2026, 16, 220" Crystals 16, no. 8: 479. https://doi.org/10.3390/cryst16080479

APA Style

Cui, M., He, M., Yang, M., Peng, B., & Wu, S. (2026). Correction: Cui et al. Gemological Study of Black Nephrite from Dahua, Guangxi Province, China. Crystals 2026, 16, 220. Crystals, 16(8), 479. https://doi.org/10.3390/cryst16080479

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