
Jadeite Texture Types & Their Geological Significance – Prof. Michelle Au’s Structural Analysis
Introduction
A jadeite’s value hinges not just on its color, but equally on its texture – the arrangement and interaction of its mineral crystals. Professor Michelle Au of the Hong Kong Gemmological Institute classifies jadeite textures into three genetic types: crystalloblastic, replacement, and cataclastic, each revealing distinct stages of the stone’s metamorphic history. This article deciphers her seminal research for collectors and gemology enthusiasts.
1. Texture Classification: The Three Genetic Types
1.1 Crystalloblastic Textures (Primary Metamorphism)
Formed during high-pressure metamorphism, these dominate jadeite’s structure:
- Granoblastic: Short-columnar jadeite crystals (e.g., “bean seed” jade) with granular, interlocking grains.
- Columnar/Fibrous: Fibrous jadeite (e.g., “glass seed”) indicates directional pressure during formation.
- Porphyroblastic: Large “phenocrysts” (e.g., “ice-bean seed”) embedded in finer matrix.
Key Quality Indicator:
- Fine-grained (0.1–0.5 mm) = Superior transparency (“water head”).
- Coarse-grained (>2 mm) = Opaque, lower value.
1.2 Replacement Textures (Fluid Alteration)
Post-metamorphic fluid interactions create:
- Edge Replacement: Mineral rims chemically altered (e.g., omphacite replacing jadeite edges).
- Net Replacement: Kosmochlor forming web-like patterns in chromite (Fig. 5).
- Pseudomorphism: Complete mineral replacement (e.g., kosmochlor mimicking chromite shapes).
1.3 Cataclastic Textures (Tectonic Stress)
- Fractured: Cracked grains from mild stress.
- Mylonitic: “Flow-like” patterns from deep crustal shearing.
2. Why Texture Matters
2.1 Practical Implications
- Transparency: Fibrous textures (e.g., “老坑種”) scatter light less, enhancing brilliance.
- Durability: Interlocked grains resist chipping.
- Authenticity: Synthetic jade lacks natural replacement textures.
2.2 Geological Storytelling
- Burmese Jadeite: High-pressure fibrous textures dominate.
- Russian Jadeite: More fractured/cataclastic due to tectonic activity.
3. Key Takeaways for Collectors
- Premium Grades: Seek fine-grained (<0.5 mm) or fibrous textures.
- Avoid: Coarse “bean seed” or heavily fractured stones.
- Geographic Clues: Replacement textures suggest Burmese origin; mylonitic textures may indicate Russian.
Source: Ouyang, Q. (2000). “Texture Types of Jadeite Jade and Its Genetic Implication.” Journal of Gems and Gemmology, 2(2), 1–6.
翡翠結構類型與地質意義——歐陽秋眉教授的權威解析
引言
翡翠的價值不僅取決於顏色,更與其結構(礦物晶體的排列方式)息息相關。香港珠寶學院歐陽秋眉教授將翡翠結構分為變晶結構、交代結構與碎裂結構三大成因類型,揭示翡翠漫長的地質演變歷程。本文為藏家解讀這項關鍵研究。
1. 結構分類:三大成因類型
1.1 變晶結構(主變質期)
形成於高壓變質環境,是翡翠的主體結構:
- 粒狀變晶:短柱狀硬玉晶體(如「豆種」),顆粒明顯。
- 柱狀/纖維狀:定向排列(如「玻璃種」)反映形成時的定向壓力。
- 斑狀變晶:粗大「斑晶」嵌於細粒基質中(如「冰豆種」)。
品質關鍵:
- 細粒(0.1–0.5毫米)= 高透明度(「水頭足」)。
- 粗粒(>2毫米)= 不透明,價值較低。
1.2 交代結構(流體作用)
後期熱液活動造成:
- 邊緣交代:礦物邊緣化學變化(如綠輝石取代硬玉外緣)。
- 網狀交代:鈉鉻輝石在鉻鐵礦中形成網格(圖版1-5)。
- 假象交代:礦物完全被取代(如鈉鉻輝石複製鉻鐵礦外形)。
1.3 碎裂結構(構造應力)
- 碎裂結構:礦物裂紋(輕微應力)。
- 糜稜結構:流動狀變形(深層地殼剪切)。
2. 結構的實際意義
2.1 鑑賞要點
- 透明度:纖維狀結構(如「老坑種」)光線散射少,更透亮。
- 耐久性:顆粒緊密結合者不易破损。
- 辨偽:合成翡翠缺乏天然交代紋理。
2.2 產地特徵
- 緬甸翡翠:以高壓纖維狀結構為主。
- 俄羅斯翡翠:因構造活動多碎裂紋理。
3. 給藏家的建議
- 優選:細粒(<0.5毫米)或纖維狀結構。
- 避開:粗粒「豆種」或裂隙多的翡翠。
- 產地判斷:交代結構多見於緬甸料;糜稜結構可能來自俄羅斯。
資料來源:歐陽秋眉(2000)。〈翡翠結構類型及其成因意義〉。《寶石和寶石學雜誌》,2(2),1–6。
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