phyllosilicate minerals
層狀硅酸鹽礦物
phyllosilicate structure
層狀硅酸鹽結構
phyllosilicate clay
層狀硅酸鹽粘土
phyllosilicate group
層狀硅酸鹽組
phyllosilicate layers
層狀硅酸鹽層
phyllosilicate composition
層狀硅酸鹽成分
phyllosilicate properties
層狀硅酸鹽性質
phyllosilicate textures
層狀硅酸鹽紋理
phyllosilicate classification
層狀硅酸鹽分類
phyllosilicate formation
層狀硅酸鹽形成
phyllosilicate minerals are essential for soil formation.
層硅酸鹽礦物對土壤形成至關重要。
the structure of phyllosilicate is characterized by layered sheets.
層硅酸鹽的結構以層狀薄片爲特徵。
phyllosilicate clays are commonly used in ceramics.
層硅酸鹽粘土常用於陶瓷。
researchers study phyllosilicate to understand its properties.
研究人員研究層硅酸鹽以瞭解其特性。
phyllosilicate can absorb water, affecting its behavior.
層硅酸鹽可以吸水，影響其行爲。
many phyllosilicate minerals are used in industrial applications.
許多層硅酸鹽礦物用於工業應用。
phyllosilicate plays a significant role in the geology of the region.
層硅酸鹽在該地區的地質中發揮着重要作用。
the identification of phyllosilicate in rocks can indicate past water activity.
岩石中層硅酸鹽的識別可以表明過去的水活動。
phyllosilicate is often found in metamorphic rocks.
層硅酸鹽通常出現在變質岩中。
understanding phyllosilicate behavior is crucial for environmental studies.
理解層硅酸鹽的行爲對環境研究至關重要。
phyllosilicate minerals
層狀硅酸鹽礦物
phyllosilicate structure
層狀硅酸鹽結構
phyllosilicate clay
層狀硅酸鹽粘土
phyllosilicate group
層狀硅酸鹽組
phyllosilicate layers
層狀硅酸鹽層
phyllosilicate composition
層狀硅酸鹽成分
phyllosilicate properties
層狀硅酸鹽性質
phyllosilicate textures
層狀硅酸鹽紋理
phyllosilicate classification
層狀硅酸鹽分類
phyllosilicate formation
層狀硅酸鹽形成
phyllosilicate minerals are essential for soil formation.
層硅酸鹽礦物對土壤形成至關重要。
the structure of phyllosilicate is characterized by layered sheets.
層硅酸鹽的結構以層狀薄片爲特徵。
phyllosilicate clays are commonly used in ceramics.
層硅酸鹽粘土常用於陶瓷。
researchers study phyllosilicate to understand its properties.
研究人員研究層硅酸鹽以瞭解其特性。
phyllosilicate can absorb water, affecting its behavior.
層硅酸鹽可以吸水，影響其行爲。
many phyllosilicate minerals are used in industrial applications.
許多層硅酸鹽礦物用於工業應用。
phyllosilicate plays a significant role in the geology of the region.
層硅酸鹽在該地區的地質中發揮着重要作用。
the identification of phyllosilicate in rocks can indicate past water activity.
岩石中層硅酸鹽的識別可以表明過去的水活動。
phyllosilicate is often found in metamorphic rocks.
層硅酸鹽通常出現在變質岩中。
understanding phyllosilicate behavior is crucial for environmental studies.
理解層硅酸鹽的行爲對環境研究至關重要。
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