Ti in biotite and muscovite as an indication of metamorphic grade in almandine amphibolite facies rocks from Sudbury, Ontario
- 1 November 1968
- journal article
- research article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 32 (11) , 1222-1229
- https://doi.org/10.1016/0016-7037(68)90124-5
Abstract
No abstract availableKeywords
This publication has 8 references indexed in Scilit:
- The effect of crystal field stabilization on the distribution of transition metals between metamorphic mineralsGeochimica et Cosmochimica Acta, 1967
- On the Facies Series in Various Types of MetamorphismThe Journal of Geology, 1967
- Stability of Al2SiO5 polymorphsChemical Geology, 1967
- Chemical Study of Minerals from the Moine Schists of the Ardnamurchan Area, Argyllshire, ScotlandJournal of Petrology, 1967
- PROGRESSIVE METAMORPHISM AND GRANITIZATION OF THE MAJOR PARAGNEISS, NORTHWEST ADIRONDACK MOUNTAINS, NEW YORKGSA Bulletin, 1960
- Chemical Study of Garnet, Biotite, and Hornblende from Gneisses of Southwestern Quebec, with Emphasis on Distribution of Elements in Coexisting MineralsThe Journal of Geology, 1959
- The Role of Adsorption in the Fractionation and Distribution of ElementsThe Journal of Geology, 1955
- Some mineralogical and chemical changes induced by progressive metamorphism in the Green Bed group of the Scottish DalradianMineralogical Magazine and Journal of the Mineralogical Society, 1930