Metasomatism and the Chemical Transformation of Rock

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Fluid-aided mass transfer and subsequent mineral re-equilibration are the two defining features of metasomatism and must be present in order for metamorphism to occur. Coupled with igneous and tectonic processes, metasomatism has played a major role in the formation of the Earth’s continental and oceanic crust and lithospheric mantle as well as in their evolution and subsequent stabilization. Meta...
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Fluid-aided mass transfer and subsequent mineral re-equilibration are the two defining features of metasomatism and must be present in order for metamorphism to occur. Coupled with igneous and tectonic processes, metasomatism has played a major role in the formation of the Earth’s continental and oceanic crust and lithospheric mantle as well as in their evolution and subsequent stabilization. Meta...
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  • Formats: pdf
  • ISBN: 9783642283949
  • Publication Date: 15 Aug 2012
  • Publisher: Springer Berlin Heidelberg
  • Product language: English
  • Drm Setting: DRM