The intrusive granites which contain ores are the product of solidified magmas, most probably ones that have undergone significant magmatic differentiation.
Yes, magmas can be classified as intrusive or extrusive. Intrusive magmas form underground as the magma cools slowly, resulting in large crystals. Extrusive magmas, on the other hand, cool quickly on the Earth's surface, leading to fine-grained or glassy textures like obsidian or basalt.
Yes, magmas can be classified as intrusive or extrusive. Intrusive magmas cool and solidify beneath the Earth's surface, forming intrusive igneous rocks like granite. Extrusive magmas erupt onto the Earth's surface and solidify quickly, forming extrusive igneous rocks like basalt.
ALL minerals crystallise from molten materials. Magma consists of minerals. It is easy to believe that all magma is the same, but magmas are as different as rocks.
Think about this: When molten rock cools slowly, bigger crystals are created.Then think about this: Intrusive rocks cool quite slowly because they are created in the earth's crust.So... Intrusive igneous rocks have bigger crystals. Molten magma in the earth's crust cools slowly making rocks like granite with big crystals.Get it? got it?GOOD!!
No, magma is molten rock, and it is a semi liquid that exists below the surface (when it's above the surface, it's called lava). When magma cools underground it becomes an intrusive igneous rock which is composed of combinations of various minerals.
Island arc and continental arc magmas are similar in that both are formed through the process of subduction, where one tectonic plate is forced beneath another, leading to the melting of mantle rocks and the generation of magma. Both types of magmas typically exhibit similar compositions, often being andesitic to rhyolitic, due to the incorporation of water and sediments from the subducting plate, which affects their melting processes. Additionally, both can produce explosive volcanic activity as the generated magma rises and interacts with the surrounding crust.
Magmas are named according to their percentage of silicate mineral content .
Minerals that form from melted materials include minerals such as quartz, feldspar, and mica. These minerals typically crystallize from molten rock as it cools and solidifies. The specific minerals that form depend on factors like the composition of the melt and the rate of cooling.
Mafic and ultramafic magmas are high in dark, heavy minerals like pyroxene, amphibole, and olivine, which contribute to an igneous rock being dark in color with a higher specific gravity than felsic and intermediate magmas and rocks.
Mafic and ultramafic magmas are high in dark, heavy minerals like pyroxene, amphibole, and olivine, which contribute to an igneous rock being dark in color with a higher specific gravity than felsic and intermediate magmas and rocks.
Granitic magmas are thicker than basaltic magmas because they have higher silica content, which increases viscosity. The higher silica content leads to stronger bonding between the silica tetrahedra, making it more difficult for the magma to flow. Basaltic magmas, on the other hand, have lower silica content and are less viscous, allowing them to flow more easily.
Silicon is one of the most abundant elements in the crust and mantle. Since all magmas are derived from the crust or mantle, the silica content will be significant, and dependent on its source for its constituent percentage.