Magmatic foliation
Appearance
![](http://upload.wikimedia.org/wikipedia/commons/thumb/1/1e/Saint-Martin-de-Fressengeas_Harzburgit2.jpg/250px-Saint-Martin-de-Fressengeas_Harzburgit2.jpg)
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[edit]
References[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