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What may be formed by fractional crystallization of olivine an pyroxene?
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What type of rock may be formed by fractional crystallization of olivine and pyroxene.?
Peridotite.
Relate the classification og igneous rocks to bowen's reaction series?
The left branch of the Y-shaped arrangement consists of the discontinuous series that begins with olivine at the highest temperature and progresses through pyroxene, amphibole, and biotite as the temperature decreases. This series is discontinuous because the reaction occurs at a fixed temperature at constant pressure wherein the early-formed mineral is converted to a more stable crystal. Each mineral in the series displays a different silicate structure that exhibits increased polymerization as the temperature drops; olivine belongs to the island silicate structure type; pyroxene, the chain; amphibole, the double chain; and biotite, the sheet. On the other hand, the right branch is the continuous reaction series in which plagioclase is continuously reacting with the liquid to form a more albitic phase as the temperature decreases. In both cases, the liquid is consumed in the reaction. When the two reaction series converge at a low temperature, minerals that will not react with the remaining liquid approach eutectic crystallization. Potash feldspar, muscovite, and quartz are crystallized. The phases that are crystallized first are the common minerals that compose basalt or gabbro, like bytownite or labradorite with pyroxene and minor amounts of olivine. Andesite or diorite minerals, such as andesine with either pyroxene or amphibole, crystallize next and are followed by orthoclase and quartz, which are the essential constituents of rhyolite or granite. A basaltic liquid at the top of the Y can descend to the bottom of the series to crystallize quartz only if the earlier reactions are prevented. As demonstrated above, complete reactions between early-formed minerals and the liquid depletes the supply of the liquid, thereby curtailing the progression down the series. One means by which basaltic magma can be transformed to rocks lower in the series is by fractional crystallization. In this process, the early-formed minerals are removed from the liquid by gravity (such minerals as olivine and pyroxene are denser than the liquid from which they crystallized), and so unreacted liquid remains later in the series.
Is igneous rock formed by crystallization of molten rock?
Yes! That's precisely how igneous rock is formed
What is the material that igneous rock is made of called?
Igneous rock is formed from the crystallization of molten magma or lava. Intrusive igneous rock is formed beneath Earth's crust from magma. Extrusive igneous rock is formed above Earth's crust from the crystallization of lava.
What five features are formed by magma?
igneous rocks, lava, crystallization, granite, deformation.
What type of rock may be formed by fractional crystallization of olivine and pyroxene.?
Peridotite.
What igneous rock may be formed by fractional crystallization of olivine and pyroxene?
ultramafic
Minerals that are formed by magma are formed by what?
Crystallization
Relate the classification og igneous rocks to bowen's reaction series?
The left branch of the Y-shaped arrangement consists of the discontinuous series that begins with olivine at the highest temperature and progresses through pyroxene, amphibole, and biotite as the temperature decreases. This series is discontinuous because the reaction occurs at a fixed temperature at constant pressure wherein the early-formed mineral is converted to a more stable crystal. Each mineral in the series displays a different silicate structure that exhibits increased polymerization as the temperature drops; olivine belongs to the island silicate structure type; pyroxene, the chain; amphibole, the double chain; and biotite, the sheet. On the other hand, the right branch is the continuous reaction series in which plagioclase is continuously reacting with the liquid to form a more albitic phase as the temperature decreases. In both cases, the liquid is consumed in the reaction. When the two reaction series converge at a low temperature, minerals that will not react with the remaining liquid approach eutectic crystallization. Potash feldspar, muscovite, and quartz are crystallized. The phases that are crystallized first are the common minerals that compose basalt or gabbro, like bytownite or labradorite with pyroxene and minor amounts of olivine. Andesite or diorite minerals, such as andesine with either pyroxene or amphibole, crystallize next and are followed by orthoclase and quartz, which are the essential constituents of rhyolite or granite. A basaltic liquid at the top of the Y can descend to the bottom of the series to crystallize quartz only if the earlier reactions are prevented. As demonstrated above, complete reactions between early-formed minerals and the liquid depletes the supply of the liquid, thereby curtailing the progression down the series. One means by which basaltic magma can be transformed to rocks lower in the series is by fractional crystallization. In this process, the early-formed minerals are removed from the liquid by gravity (such minerals as olivine and pyroxene are denser than the liquid from which they crystallized), and so unreacted liquid remains later in the series.
Is olivine formed by evaporation of shallow sea water?
Olivine is not an evaporite.
Does olivine rock form to become soil?
Sand is formed from the breakdown of rocks. If a rock contains large amounts of olivine, then when this rock weathers, olivine sand will be formed. There are beaches in New Zealand that are almost exclusively made of green olivine crystals.
What is formed from the crystallization of magma?
igneous rock
What are minerals that form from magma are formed by?
Crystallization
What type of rock is formed when magma undergoes crystallization above ground?
Extrusive igneous rock is formed from the crystallization of magma (lava) above ground.
How is zircon formed?
Zircon forms from the crystallization of magma.
What term refers to the removal and isolation of early-formed mineral grains that can cause the composition of the remaining magma to change?
The process of fractional crystallization is part of igneous differentiation, where minerals crystallize at different temperatures and under complex circumstances.
How Metal-rich veins are formed at the end or what?
magma crystallization
