XinJing
JD-387
Additional information
| Stones | Bodhi Old Beads Lucky Cat, Duobao Bodhi Old Shape Beads 10*11Mm, Duobao Bodhi Old Shape Beads 11*12Mm, Green Bodhi Old Style Bead Olive Core Spacer, White Jade Bodhi Green Aventurine Lotus, White Jade Bodhi Lotus Bead Green Aventurine Lotus, White Jade Bodhi Lotus Bead Lucky Cat, White Jade Bodhi Lotus Pendant Multi-Circle, White Jade Bodhi Old Shape Beads Cat Claw Lucky Cat, White Jade Bodhi Old Style Beads Amulet, White Jade Bodhi Old Type Bead Olive Core Spacer, White Jade Bodhi Old Type Beads Sandalwood Pumpkin Lotus, White Jade Bodhi Pumpkin Pearl Green Aventurine Lotus |
|---|---|
| Size | See the size diagram |
| MOQ | 12 |
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Description
Natural Stone Details
Natural Characteristics
Naturally formed gemstones may show subtle inclusions, such as crystalline lines or transparent ice textures — authentic marks of nature.
Size Variation
Slight size differences within ±0.5mm are normal due to natural material variation and precision cutting tolerance.
Color Difference
Lighting, screen display, and perception differences may affect visual color — the actual gem color will be the reference.
Beads String Sizes
| Beads Size | Length (cm) | Approx PCS | Hole Size | Weight |
|---|---|---|---|---|
| 6mm | 35–38 | 60–63 | 0.9–1.2mm | 22–34g |
| 8mm | 35–38 | 45–47 | 0.9–1.2mm | 38–60g |
| 10mm | 35–38 | 36–37 | 1.0–1.2mm | 58–94g |
| 12mm | 35–38 | 31–32 | 1.2–1.5mm | 80–133g |
Bracelet Sizes
| Beads Size | Bracelet Length | Number of Beads | Weight | Suitable Wrist |
|---|---|---|---|---|
| 6mm | 17–18cm | 28–29 | 10–17g | 14.5–15cm |
| 8mm | 18–19cm | 22–23 | 17–30g | 15–15.5cm |
| 10mm | 19–20cm | 18–19 | 28–47g | 16–16.5cm |
| 12mm | 20–21cm | 16–17 | 43–73g | 17–17.5cm |
| 14mm | 21–22cm | 14–15 | 59–100g | 17.5–19cm |
* Weight may vary depending on material.
Natural Gemstone Characteristics
Natural pit
Formed by surface weathering or pressure release after crystallization.
Fissure
Secondary cracks formed by tectonic movements after rock formation.
Internal fissure
Natural ice-crack patterns from pressure changes during crystallization.
Paragenetic mineral
Minerals that crystallized together with the host stone under the same conditions.
Color zoning
Caused by uneven distribution of trace elements during crystal growth.
Black spot
Tiny mineral inclusions or carbon residues trapped inside.
Internal inclusion
Trapped minerals or gas-liquid cavities formed during crystal growth.
Silky inclusion
Fine fibrous structures reflecting light to create a silky luster.