- journal_title：The Canadian Mineralogist
- Contributor：Georgy A. Belyanin ; H.M. Rajesh ; Krishnan Sajeev ; Dirk D. Van Reenen
- Publisher：Mineralogical Association of Canada
- Date：2012-10-01
- Format：text/html
- Language：en
- Identifier：10.3749/canmin.50.5.1153
- journal_abbrev：Can Mineral
- issn：0008-4476
- volume：50
- issue：5
- firstpage：1153
- section：Articles
Sapphirine + quartz and orthopyroxene + sillimanite occur in garnet from an Mg-Al granulite from the Central Zone of the Limpopo Complex in South Africa. Textural evidence and a chemical gradient in garnet between the zones preserving the inclusions argue for the formation of sapphirine + quartz after orthopyroxene + sillimanite. Petrological observations, pressure-temperature phase diagrams, and compositional and model proportion results on isopleths indicate the sapphirine + quartz + garnet + orthopyroxene (high-Al) assemblage as the peak metamorphic assemblage (~1050 °C at ~8.5 kbars), whereas orthopyroxene (low-Al) + sillimanite represents the prograde stage (at ca. 900 °C at ~8.5 kbars). Our report of these two diagnostic ultrahigh-temperature mineral assemblages in garnet from an Mg-Al granulite is unique, given the rare occurrence of sapphirine + quartz postdating orthopyroxene + sillimanite assemblage in granulites.