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The SMOG method is used when:
Continental Crust
The layer of igneous, sedimentary, and metamorphic rocks that forms the continents and the areas of shallow seabed close to their shores.
Felsic Composition
Rocks rich in silica and aluminum, characterized by lighter minerals like quartz and feldspar.
Decompression
The reduction in pressure exerted on a material, often leading to changes in its physical state or phase.
Melting Mantle
The process in which the Earth's mantle, the layer between the crust and the core, experiences partial melting to form magma.
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