Magmatic foliation is a term in geology, for foliation in granitoids that form by magmatic flow, "submagmatic flow," by high-temperature solid-state deformation and moderate- to low-temperature solid-state deformation.[1]
Remember, granitoids are igneous rocks.[2][3]
See also
editReferences
edit- ^ ScienceDirect: Foliations in granitoids can form by magmatic flow, ‘submagmatic flow’, high-temperature solid-state deformation and moderate- to low-temperature solid-state deformation. A, accessdate: March 23, 2017
- ^ Springer: Metamorphism of Granitoids - Springer, accessdate: March 23, 2017
- ^ Granite: metamo, accessdate: March 23, 2017
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