Chemical structure in granitic magmas - a signal from the source?

J. D. Clemens, P. A. Helps, G. Stevens

Research output: Chapter in Book/Report/Conference proceedingConference contributionpeer-review

Original languageEnglish
Title of host publicationPublished in Earth and Environmental Science: Transactions of the Royal Society of Edinburgh (2009) 100: pp 159-172 doi:10.1017/S1755691009016053 Organising Body: University of Stellenbosch and the Geological Society of South Africa Organising Body: University of Stellenbosch and the Geological Society of South Africa
Publication statusPublished - 2007
Externally publishedYes

Bibliographical note

Note: Published in Earth and Environmental Science: Transactions of the Royal Society of Edinburgh (2009) 100: pp 159-172 doi:10.1017/S1755691009016053

Organising Body: University of Stellenbosch and the Geological Society of South Africa

Organising Body: University of Stellenbosch and the Geological Society of South Africa

Keywords

  • chemical variation
  • differentiation
  • granitic magma
  • inherited heterogeneity
  • barberton greenstone-belt
  • s-type granites
  • source material restite
  • nevada volcanic field
  • south-africa
  • silicic magmas
  • northeastern brazil
  • sierra-nevada
  • central chile
  • zoned pluton
  • Earth systems and environmental sciences

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