Gemological Characteristics of Lvwen Stone and Its Color Genesis
Abstract
:1. Introduction
2. Materials and Methods
2.1. Materials
2.2. Specimen Preparation and Testing Methods
2.2.1. Specimen Preparation
2.2.2. X-ray Diffraction Analysis
2.2.3. Scanning Electron Microscope
2.2.4. Fourier-Transform Infrared Spectroscopy
2.2.5. Laser Ablation Inductively Coupled Plasma Mass Spectrometry
2.2.6. Ultraviolet–Visible Spectroscopy
3. Results
3.1. X-ray Diffraction Analysis
3.2. Spectroscopic Characterization
3.2.1. Fourier-Transform Infrared Spectroscopy Analysis
3.2.2. Ultraviolet–Visible Spectroscopy Analysis
3.3. Chemical Compositions
3.4. Microstructural Characteristics
4. Discussion
5. Conclusions
- (1)
- The mineral composition of Lvwen stone is calcite, with crystal cell parameters of a = 4.97 and c = 17.00 Å and calcite crystals with an average grain size of 1737 Å. The cabochons used in this study have obvious white bands even after being cut into blocks, indicating that the banding is not due to chatoyancy (“cat’s-eye effect”). The white bands are composed of parallel-arranged, ~100 μm–sized calcite crystals. In contrast, the green matrix is dominated by smaller (~10 μm) cryptocrystalline calcite particles. These differences in crystallinity contribute to the contrasting transparencies of the white bands and green matrix.
- (2)
- The chemical formula of Lvwen stone is Ca0.97Mn0.02Mg0.01 [CO3], and the content of ΣREE in the green matrix is higher than that in the white bands. There is a significantly larger content of Fe and Cu in the green matrix as compared with the white bands, showing that the green color of the matrix is formed by the absorption of light by Fe3+ and Cu2+ in the calcite lattice, resulting from the 6A1→4E(4D)d-d intra-ion electron transition of Fe3+ and 2E→2T2(2D)d-d intra-ion electron transition of Cu2+, respectively. In addition, different crystal particle sizes may also affect the color of the green matrix and the white bands.
- (3)
- The occurrence of the ~1125 cm−1 absorption band and the broadening of the ~1490 cm−1 band on the FTIR spectrum suggest that the reduced symmetry of the [CO3]2− distribution of calcite crystals in Lvwen stone, compared with that of ideal calcite, may be related to isomorphic substitution of Mg2+ and Mn2+ for Ca2+. The double absorptions at 2923 and 2854 cm−1 reveal the presence of aliphatic hydrocarbon inclusions in the study specimens.
- (4)
- Discriminant diagrams show that the green matrix and white bands of Lvwen stone had the same origin, and that both are the products of hydrothermal fluids. The presence of positive Ce anomalies in both the green matrix and white bands is an indication that the mineralizing fluid reductively remobilized earlier-formed Ce-oxides that had precipitated under oxidizing conditions. The orientation of crystals in the white bands perpendicular to the band plane shows that the study specimens formed in a tectonically controlled stress regime that permitted the formation of stretching veins.
Author Contributions
Funding
Data Availability Statement
Acknowledgments
Conflicts of Interest
References
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NaO | MgO | SiO2 | CaO | MnO | CuO | SrO | |
---|---|---|---|---|---|---|---|
S1-green-1 | 0.38 | 0.49 | 0.21 | 52.56 | 1.62 | 0.32 | 0.36 |
S1-green-2 | 0.40 | 0.47 | 0.21 | 52.45 | 1.65 | 0.34 | 0.36 |
S1-green-3 | 0.38 | 0.47 | 0.26 | 52.43 | 1.68 | 0.35 | 0.36 |
Average | 0.39 | 0.48 | 0.24 | 52.48 | 1.65 | 0.33 | 0.36 |
S2-green-1 | 0.36 | 0.51 | 0.30 | 52.44 | 1.63 | 0.30 | 0.36 |
S2-green-2 | 0.35 | 0.47 | 0.31 | 52.29 | 1.77 | 0.36 | 0.35 |
S2-green-3 | 0.35 | 0.47 | 0.30 | 52.38 | 1.72 | 0.34 | 0.36 |
Average | 0.35 | 0.48 | 0.30 | 52.37 | 1.71 | 0.33 | 0.36 |
S3-green-1 | 0.35 | 0.49 | 0.31 | 52.57 | 1.54 | 0.29 | 0.36 |
S3-green-2 | 0.36 | 0.50 | 0.31 | 52.44 | 1.62 | 0.28 | 0.37 |
S3-green-3 | 0.35 | 0.48 | 0.31 | 52.33 | 1.73 | 0.35 | 0.35 |
Average | 0.35 | 0.49 | 0.31 | 52.45 | 1.63 | 0.31 | 0.36 |
S1-white-1 | 0.38 | 0.56 | 0.21 | 53.00 | 1.16 | 0.19 | 0.40 |
S1-white-2 | 0.40 | 0.57 | 0.21 | 52.84 | 1.27 | 0.21 | 0.39 |
S1-white-3 | 0.42 | 0.58 | 0.26 | 52.85 | 1.19 | 0.18 | 0.39 |
Average | 0.40 | 0.57 | 0.24 | 52.90 | 1.20 | 0.19 | 0.39 |
S2-white-1 | 0.36 | 0.56 | 0.30 | 53.02 | 1.14 | 0.17 | 0.38 |
S2-white-2 | 0.37 | 0.59 | 0.30 | 52.98 | 1.17 | 0.17 | 0.37 |
S2-white-3 | 0.37 | 0.59 | 0.32 | 52.92 | 1.17 | 0.17 | 0.38 |
Average | 0.37 | 0.58 | 0.31 | 52.98 | 1.16 | 0.17 | 0.38 |
S3-white-1 | 0.37 | 0.57 | 0.32 | 52.96 | 1.18 | 0.17 | 0.37 |
S3-white-2 | 0.36 | 0.57 | 0.31 | 53.04 | 1.14 | 0.16 | 0.37 |
S3-white-3 | 0.36 | 0.57 | 0.33 | 53.11 | 1.08 | 0.15 | 0.36 |
Average | 0.36 | 0.57 | 0.32 | 53.04 | 1.14 | 0.15 | 0.37 |
V | Cr | Fe | Co | Ni | Zn | |
---|---|---|---|---|---|---|
S1-green-1 | 0.34 | 0.51 | 185.88 | 38.88 | 3.20 | 399.46 |
S1-green-2 | 0.26 | 0.76 | 204.03 | 38.36 | 3.96 | 416.37 |
S1-green-3 | 0.28 | 0.78 | 237.38 | 39.29 | 3.22 | 453.73 |
Average | 0.29 | 0.68 | 209.10 | 38.84 | 3.46 | 423.19 |
S2-green-1 | 0.18 | 0.46 | 218.61 | 36.80 | 2.98 | 407.60 |
S2-green-2 | 0.24 | 0.12 | 268.16 | 36.89 | 3.70 | 471.20 |
S2-green-3 | 0.29 | 0.00 | 233.86 | 36.55 | 1.71 | 400.73 |
Average | 0.24 | 0.20 | 240.21 | 36.75 | 2.80 | 426.51 |
S3-green-1 | 0.31 | 0.00 | 223.69 | 34.95 | 2.30 | 382.36 |
S3-green-2 | 0.29 | 0.00 | 231.72 | 37.30 | 3.44 | 375.34 |
S3-green-3 | 0.28 | 0.00 | 276.33 | 36.38 | 1.80 | 443.82 |
Average | 0.29 | 0.00 | 243.91 | 37.30 | 2.51 | 400.51 |
S1-white-1 | 0.21 | 0.74 | 135.69 | 34.99 | 3.47 | 226.68 |
S1-white-2 | 0.30 | 1.40 | 151.05 | 35.70 | 2.63 | 251.09 |
S1-white-3 | 0.25 | 0.46 | 109.16 | 35.07 | 3.62 | 220.96 |
Average | 0.25 | 0.87 | 131.97 | 35.25 | 3.24 | 232.91 |
S2-white-1 | 0.26 | 0.99 | 165.77 | 36.05 | 3.23 | 211.17 |
S2-white-2 | 0.17 | 0.74 | 112.69 | 37.96 | 2.95 | 232.60 |
S2-white-3 | 0.18 | 0.00 | 137.22 | 38.77 | 3.07 | 242.52 |
Average | 0.20 | 0.58 | 138.56 | 37.59 | 3.08 | 228.76 |
S3-white-1 | 0.29 | 1.28 | 167.06 | 36.46 | 2.29 | 243.10 |
S3-white-2 | 0.27 | 0.00 | 124.00 | 36.97 | 2.78 | 241.07 |
S3-white-3 | 0.25 | 0.00 | 117.14 | 36.46 | 1.54 | 255.99 |
Average | 0.27 | 0.43 | 136.07 | 36.63 | 2.20 | 246.72 |
The Number of Cations Based on Of.u. = 3 | Stoichiometric Number | |||||||
---|---|---|---|---|---|---|---|---|
S1-green | S2-green | S3-green | S1-white | S2-white | S3-white | Total Average | ||
Mg2+ | 0.01 | 0.01 | 0.01 | 0.01 | 0.01 | 0.01 | 0.01 | 1.00 |
Ca2+ | 0.96 | 0.96 | 0.96 | 0.97 | 0.97 | 0.97 | 0.97 | |
Mn2+ | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | |
C4+ | 1.00 | 1.00 | 1.00 | 1.00 | 1.00 | 1.00 | 1.00 | 1.00 |
S1-green-1 | S1-green-2 | S1-green-3 | S2-green-1 | S2-green-2 | S2-green-3 | S3-green-1 | S3-green-2 | S3-green-3 | Average | ||
La | 3.36 | 3.64 | 4.14 | 3.33 | 3.74 | 3.16 | 3.27 | 3.48 | 3.68 | 3.53 | |
Ce | 8.20 | 9.23 | 10.40 | 7.84 | 8.92 | 7.87 | 8.64 | 8.32 | 9.04 | 8.72 | |
Pr | 0.81 | 0.94 | 0.94 | 0.77 | 0.83 | 0.80 | 0.90 | 0.81 | 0.78 | 0.84 | |
Nd | 4.05 | 4.66 | 5.06 | 4.15 | 4.42 | 3.80 | 4.29 | 3.83 | 4.34 | 4.29 | |
Sm | 1.00 | 1.25 | 1.31 | 0.97 | 1.31 | 1.24 | 1.18 | 1.02 | 1.51 | 1.20 | |
Eu | 0.38 | 0.51 | 0.50 | 0.51 | 0.48 | 0.38 | 0.43 | 0.40 | 0.48 | 0.45 | |
Gd | 1.95 | 2.14 | 2.67 | 1.90 | 2.02 | 2.29 | 1.99 | 2.29 | 2.06 | 2.14 | |
Tb | 0.39 | 0.40 | 0.44 | 0.37 | 0.40 | 0.37 | 0.42 | 0.37 | 0.41 | 0.40 | |
Dy | 2.96 | 3.30 | 3.41 | 2.68 | 3.11 | 2.90 | 2.42 | 2.50 | 3.04 | 2.92 | |
Ho | 0.79 | 0.82 | 0.94 | 0.68 | 0.76 | 0.74 | 0.77 | 0.69 | 0.78 | 0.77 | |
Er | 2.46 | 2.62 | 2.71 | 2.29 | 2.36 | 2.12 | 2.38 | 2.08 | 2.65 | 2.41 | |
Tm | 0.35 | 0.35 | 0.38 | 0.32 | 0.32 | 0.35 | 0.33 | 0.36 | 0.33 | 0.34 | |
Yb | 2.46 | 2.50 | 2.72 | 2.27 | 2.54 | 2.49 | 2.11 | 2.26 | 2.35 | 2.41 | |
Lu | 0.33 | 0.30 | 0.37 | 0.33 | 0.37 | 0.32 | 0.33 | 0.26 | 0.35 | 0.33 | |
ΣREE | 29.49 | 32.66 | 35.98 | 28.42 | 31.57 | 28.83 | 29.46 | 28.67 | 31.80 | 30.76 | |
δCe | 1.20 | 1.21 | 1.27 | 1.18 | 1.23 | 1.19 | 1.22 | 1.20 | 1.29 | ||
δEu | 0.84 | 0.95 | 0.81 | 1.14 | 0.90 | 0.69 | 0.85 | 0.81 | 0.83 | ||
S1-white-1 | S1-white-2 | S1-white-3 | S2-white-1 | S2-white-2 | S2-white-3 | S3-white-1 | S3-white-2 | S3-white-3 | Average | Chondrite * | |
La | 2.03 | 2.24 | 1.72 | 2.46 | 2.26 | 2.64 | 2.36 | 1.97 | 2.00 | 2.19 | 0.24 |
Ce | 4.93 | 5.59 | 4.05 | 5.87 | 5.65 | 6.64 | 6.14 | 5.21 | 5.39 | 5.50 | 0.61 |
Pr | 0.45 | 0.58 | 0.38 | 0.57 | 0.57 | 0.63 | 0.61 | 0.74 | 0.66 | 0.58 | 0.09 |
Nd | 2.41 | 2.63 | 1.80 | 2.74 | 2.76 | 3.42 | 2.99 | 2.45 | 2.53 | 2.64 | 0.46 |
Sm | 0.60 | 0.81 | 0.65 | 1.00 | 0.80 | 1.01 | 0.90 | 0.88 | 0.97 | 0.85 | 0.15 |
Eu | 0.28 | 0.24 | 0.21 | 0.27 | 0.31 | 0.34 | 0.25 | 0.33 | 0.30 | 0.28 | 0.06 |
Gd | 1.19 | 1.27 | 0.86 | 1.46 | 1.28 | 1.65 | 1.51 | 1.48 | 1.44 | 1.35 | 0.20 |
Tb | 0.20 | 0.25 | 0.19 | 0.24 | 0.24 | 0.24 | 0.23 | 0.35 | 0.32 | 0.25 | 0.04 |
Dy | 1.73 | 1.70 | 1.55 | 2.06 | 1.91 | 2.49 | 2.18 | 2.14 | 2.06 | 1.98 | 0.25 |
Ho | 0.41 | 0.50 | 0.35 | 0.49 | 0.52 | 0.58 | 0.59 | 0.54 | 0.50 | 0.50 | 0.05 |
Er | 1.33 | 1.58 | 1.09 | 1.68 | 1.56 | 1.86 | 1.68 | 1.47 | 1.06 | 1.48 | 0.16 |
Tm | 0.20 | 0.22 | 0.17 | 0.27 | 0.24 | 0.27 | 0.30 | 0.25 | 0.28 | 0.24 | 0.02 |
Yb | 1.26 | 1.49 | 1.13 | 1.75 | 1.63 | 1.83 | 1.75 | 1.58 | 1.63 | 1.56 | 0.16 |
Lu | 0.23 | 0.21 | 0.17 | 0.26 | 0.29 | 0.25 | 0.25 | 0.26 | 0.28 | 0.25 | 0.02 |
ΣREE | 17.24 | 19.31 | 14.32 | 21.11 | 20.01 | 23.87 | 21.73 | 19.64 | 19.42 | 19.63 | |
δCe | 1.24 | 1.18 | 1.22 | 1.20 | 1.20 | 1.25 | 1.24 | 1.04 | 1.13 | ||
δEu | 1.02 | 0.72 | 0.86 | 0.68 | 0.94 | 0.81 | 0.65 | 0.89 | 0.77 |
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Liu, Z.; Wang, W.; Yin, K.; Hong, H.; Algeo, T.J.; Yin, Z.; Pan, Y.; Lu, Z.; Han, W.; Wang, Y.; et al. Gemological Characteristics of Lvwen Stone and Its Color Genesis. Minerals 2022, 12, 1584. https://doi.org/10.3390/min12121584
Liu Z, Wang W, Yin K, Hong H, Algeo TJ, Yin Z, Pan Y, Lu Z, Han W, Wang Y, et al. Gemological Characteristics of Lvwen Stone and Its Color Genesis. Minerals. 2022; 12(12):1584. https://doi.org/10.3390/min12121584
Chicago/Turabian StyleLiu, Zhendong, Wenjie Wang, Ke Yin, Hanlie Hong, Thomas J. Algeo, Zuowei Yin, Yong Pan, Zhuo Lu, Wen Han, Yiming Wang, and et al. 2022. "Gemological Characteristics of Lvwen Stone and Its Color Genesis" Minerals 12, no. 12: 1584. https://doi.org/10.3390/min12121584