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

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

Research output: Contribution to conference › Paper › peer-review

Original languageEnglish
Publication statusPublished - 2007
Externally publishedYes
EventSixth Hutton Symposium on the Origin of Granites and Related Rocks - Stellenbosch, South Africa
Duration: 2 Jul 2007 → 6 Jul 2007

Conference

ConferenceSixth Hutton Symposium on the Origin of Granites and Related Rocks
Period2/07/07 → 6/07/07

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

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
  • 1 Conference contribution

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

    Clemens, J. D., Helps, P. A. & Stevens, G., 2007, 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.

    Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › peer-review

Cite this