Are Strongly Peraluminous Magmas Derived from Pelitic Sedimentary Sources?
- 1 November 1985
- journal article
- Published by University of Chicago Press in The Journal of Geology
- Vol. 93 (6) , 673-689
- https://doi.org/10.1086/628995
Abstract
No abstract availableThis publication has 54 references indexed in Scilit:
- Water contents of silicic to intermediate magmasPublished by Elsevier ,2003
- Distribution of oceanic and continental leads in the Arabian-Nubian ShieldContributions to Mineralogy and Petrology, 1983
- Mantle and crustal granites: Genetic classification of orogenic granites and the nature of their enclavesJournal of Volcanology and Geothermal Research, 1982
- The oxygen isotope composition of granitoid and sedimentary rocks of the southern Snake Range, NevadaContributions to Mineralogy and Petrology, 1982
- Plumbotectonics—the modelTectonophysics, 1981
- Controls on source and depth of emplacement of granitic magmaGeology, 1981
- Preliminary results on the oxygen isotopic composition of the lower crust, Kilbourne Hole Maar, New MexicoGeophysical Research Letters, 1980
- An inner Cordilleran belt of muscovite-bearing plutonsGeology, 1980
- Crustal anatexis: An experimental reviewTectonophysics, 1977
- Ultrametamorphism and granitoid genesisTectonophysics, 1977