These rocks contain less than 45% silica. The most characteristic minerals are olivines, pyroxenes, hornblende. These rocks are dark, sometimes green (olivine) because of the mafic minerals in their composition.
Dunite consist almost entirely of olivine, often accompanied by accessory chrome spinel.
Describing:Texture: holocrystalline, phaneritic |
Minerals: olivine |
Peridotite is an olivine-rich, coarse-grained rock. This rocks are subjected to serpentinisation. Peridotite do not have volcanic equivalent.
Describing:Texture: holocrystalline, phaneritic |
Minerals: olivine, pyroxene |
Pyroxenite and hornblendite mostly consist of pyroxenes and hornblende, respectively there are some possible accessory minerals like olivine, feldspar, nepheline.
autor: Wlodi
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