| Class: | 5D 04 |
| Name: | Cheung Cheuk Nam |
| Year: | 2017 – 2018 |
| 化學組成, 鍵及結構：
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Chemical composition, bonding and structure: (Mineral)
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| 形成：
它通過重建細粒狀的母體沉積岩而形成，如泥岩或頁岩。 原生物：(化石) |
Formation:
It formed by the reconstitution of fine-grained, parent sedimentary rocks,such as mudstones or shales. Living Specimens: (Fossil) |
| 特性：
千枚岩具有比石板更大的晶體。令它有更大程度的光線反射或光澤。板岩通常無光澤且不反光。光澤用於區分板岩與千枚岩。 |
Properties:
Phyllite has larger crystals than slate. This gives it a greater degree of light reflection or sheen. Slate is usually dull and non reflective.The sheen is used to distinguish phyllite from slate. |
| 用途：
千枚岩在住宅建築行業已有許多用途。因為它的質量，他們可以以不同的方式，以滿足大多數現代建築發展的需求和趨勢。它的質感和外觀使其很適合現代設計。例如酒店大堂，學校，博物館內部的地板磚
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Application:
Phyllite has found many uses in the residential construction industry. Because of its qualities, they can be worked in different ways to meet the demands and trends of most modern construction developments. The texture and appearance makes it suitable for modern design for example floor tile in the interior of hotel lobbies, schools, museums etc.
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| 分佈：
千枚岩通常沿著區域性的變質帶的邊界形成，也是海洋沉積岩被困在大陸板塊的摩擦之間。 千枚岩也可以在海底沉積盆地中發現。
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Distribution:
Phyllites often form along the boundaries of regional metamorphic belts where marine sedimentary rocks have been trapped in between the frictional movement of continental plates. Phyllite can also be found in sedimentary basins along the ocean floor.
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