Effects of Metasomatism on Mineral Systems and Their Host Rocks: Alkali Metasomatism, Skarns, Greisens, Tourmalinites, Rodingites, Black-Wall Alteration and Listvenites

Chapter
Part of the Lecture Notes in Earth System Sciences book series (LNESS)

Abstract

Heat-liberating events, such as igneous intrusions emplaced into cool crustal rocks, will result not only in loss of heat to the surrounding environment, but also in the transport of volatile components, which are responsible for metasomatic processes. Some of the most impressive results of these processes are, for example, fenites (K- and Na-metasomatism), skarns (Ca-metasomatism) and tourmalinisation (B-metasomatism).

Keywords

Fluid Inclusion Country Rock Ultramafic Rock Greenstone Belt Rare Earth Element 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

Notes

Acknowledgments

I thank Dan Harlov for inviting me to provide a chapter on metasomatic processes associated with mineral systems and for his useful suggestions. Rob Kerrich, Wolfgang Bach, Daniel Harlov and Håkon Austrheim are thanked for their constructive comments, which considerably improved this contribution. I publish this chapter with the permission of the Executive Director of the Geological Survey of Western Australia.

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© Springer Berlin Heidelberg 2013

Authors and Affiliations

  1. 1.Geological Survey of Western AustraliaEast PerthAustralia
  2. 2.Centre for Exploration TargetingUniversity of Western AustraliaCrawleyAustralia

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