Partial melting of the Appin Quartzite driven by fracture-controlled H[sub]2O infiltration in the aureole of the Ballachulish Igneous Complex, Scottish Highlands

Marian B. Holness, John D. Clemens

Research output: Contribution to journalArticlepeer-review

Original languageEnglish
Pages (from-to)154-168
JournalContributions to Mineralogy and Petrology
Volume136
Issue number1-2
Publication statusPublished - Jul 1999
Externally publishedYes

Bibliographical note

Note: This work was supported by the Natural Environment Research Council [grant number GR9/1589].

Keywords

  • Scotland
  • evolution
  • rock
  • crystallization
  • granite
  • model
  • Earth systems and environmental sciences

Cite this