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Fractional crystallization of olivine and pyroxene can lead to the formation of a variety of igneous rocks, particularly those in the mafic and ultramafic categories. As these minerals crystallize from a melt, they can deplete the remaining liquid in magnesium and iron, resulting in the formation of more silica-rich minerals like plagioclase and amphibole in later stages. This process can eventually yield rocks such as basalt or gabbro, depending on the extent of crystallization and the composition of the initial melt.

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What igneous rock may be formed by fractional crystallization of olivine and pyroxene?

ultramafic


What type of rock may be formed by fractional crystallization of olivine and pyroxene.?

A mafic rock, such as gabbro or basalt, may be formed through fractional crystallization of olivine and pyroxene. Mafic rocks are characterized by their high content of magnesium and iron, which are common components of olivine and pyroxene minerals.


Olivine and pyroxene are commonly found in igneous rocks that are?

Olivine and pyroxene are commonly found in igneous rocks that are mafic in composition. These minerals indicate that the rock formed from magma with a higher iron and magnesium content. Mafic igneous rocks tend to be dark in color and have higher densities compared to felsic rocks.


Igneous rocks were formed from what minerals?

Igneous rocks are formed from minerals such as quartz, feldspar, pyroxene, and olivine. These minerals solidify from magma or lava as it cools and hardens, resulting in the formation of igneous rocks.


What is an example of a mafic rock?

Basalt is a common example of a mafic rock. It is dark in color, fine-grained, and rich in minerals like pyroxene and olivine. Basalt is formed from the solidification of magma with low silica content, typically from volcanic activity.


Which is a coarse-grained igneous rock composed of mainly pyroxene plagioclase feldspar and olivine?

Gabbro.


What kinds minerals you can find on surtsey?

Minerals found on Surtsey include olivine, pyroxene, magnetite, ilmenite, and plagioclase. These minerals are typical of volcanic islands like Surtsey, which was formed through volcanic activity.


How is Olivine formed?

Olivine is formed primarily through the crystallization of magma during the cooling of molten rock, particularly in mafic and ultramafic igneous environments. It typically crystallizes at high temperatures and is often found in basalt and peridotite. Additionally, olivine can form through metamorphic processes, where it is produced from the alteration of other minerals under high-temperature conditions. Its formation is a key component of the Earth's mantle, contributing to its mineral composition.


What minerals combine to form igneous rock?

It doesn't necessarily matter what the minerals are, as long as they form from cooling magma or lava. Igneous rocks are formed by the solidification of cooled magma (molten rock). They may form with or without crystallization, either below the surface as intrusive (plutonic) rocks or on the surface as extrusive (volcanic) rocks.


Minerals that are formed by magma are formed by what?

Crystallization


Is olivine formed by evaporation of shallow sea water?

Olivine is not an evaporite.


What rock is formed when lava cools down?

When lava cools down quickly at the surface of the Earth, it forms an igneous rock called basalt. Basalt is dark in color, fine-grained, and contains minerals such as olivine and pyroxene.

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