Anorogenic magmatism

In geology anorogenic magmatism is the formation, intrusion or eruption of magmas in other settings than convergent plate margins such as continental collision and subduction where orogeny is common.[1]

References

  1. ↑ Anorogenic magmatism in Dronning Maud Land (Antarctica)
This article is issued from Wikipedia - version of the 9/6/2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.