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Robert W Charles has written: 'Amphiboles on the join pargasite-ferropargasite' -- subject(s): Amphiboles
Pyroxenes have a single chain structure, while amphiboles have a double chain structure. Pyroxenes typically have a simpler, more elongated crystal structure compared to the more complex, ribbony structure of amphiboles. Additionally, pyroxenes commonly have a monoclinic or orthorhombic crystal system, while amphiboles have a monoclinic system.
Feldspars Piroxenes Amphiboles
Hornblende and other amphiboles have a double chain silicate structure, where silicon-oxygen tetrahedra are connected in double chains linked by other cations like aluminum, magnesium, and iron ions. This structure gives amphiboles their distinct prismatic shape and cleavage properties.
Amphiboles have a more complex structure than pyroxenes because they contain additional layers of oxygen and hydroxyl groups. This leads to a greater variety of chemical compositions and structural arrangements within amphiboles compared to pyroxenes. Additionally, amphiboles often exhibit more pronounced cleavage planes and a wider range of physical properties due to their more intricate structure.
Amphiboles are minerals containing mostly silicon, oxygen, iron, and magnesium.
Robert L. Virta has written: 'The phase relationship of talc and amphiboles in a fibrous talc sample' -- subject(s): Amphiboles, Phase rule and equilibrium, Talc 'The talc industry--an overview' -- subject(s): Talc, Talc industry
The mineral family that tends to form long needlelike crystals is the amphibole group. Examples of minerals in this group include hornblende and tremolite. These minerals are silicate minerals with a double chain structure, which contributes to their characteristic needlelike crystal habit.
Minerals form as hot magma cools inside the crust, or as lava hardens on the surface. When these liquids cool to a solid state, they form crystals. When elements and compounds that are dissolved in water leave a solution, crystallization occurs.
Chrysotile asbestos (White) is a Serpentine, Amosite (Grunerite) (Brown asbestos, and Crocidolite (Blue) are Amphiboles
Quartz and the Feldspar are very common. Other common silicates would be the mica group, even pyroxenes and the amphiboles.
Yes, amphiboles typically exhibit two directions of cleavage at approximately 56 and 124 degrees. Cleavage refers to the tendency of a mineral to break along certain planes due to its internal structure.