No.
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Pure olivine is not magnetic because it does not contain iron. However, some varieties of olivine, such as fayalite, can be weakly magnetic due to their iron content.
Yes, fayalite is a magnetic mineral because it contains iron atoms in its structure, which can exhibit magnetic properties. Fayalite is a member of the olivine mineral group and has a strong magnetic response due to the iron content.
The density of olivine ranges from 3.2 to 4.4 g/cm3, depending on its composition and structure.
Yes, olivine rock can weather and break down over time to form olivine-rich soils. The weathering process involves the physical and chemical breakdown of the olivine mineral, eventually leading to the release of nutrients that can support plant growth.
Olivine is the mineral present in much greater quantities in peridotite than gabbro. Peridotite is rich in olivine, while gabbro contains less olivine and more plagioclase feldspar.
Following Goldich Dissolution Series (Or going backwards by Bowen's Reaction Series), olivine weathers before Quartz. Quartz has a framework silicate structure and olivine has a isolated silicate structure.