Mineralogy of Amphibolite Interlayers in the Gneiss Complex, Northwest Adirondack Mountains, New York
- 1 March 1964
- journal article
- Published by University of Chicago Press in The Journal of Geology
- Vol. 72 (2) , 131-156
- https://doi.org/10.1086/626973
Abstract
No abstract availableThis publication has 19 references indexed in Scilit:
- Compositional characteristics and equilibrium relations in mineral assemblages of a metamorphosed iron formation [Quebec]American Journal of Science, 1960
- Co-existing Pyroxenes: Some Causes of Variation and Anomalies in the optically Derived Compositional Tie-Lines, with Particular Reference to Charnockitic RocksGeological Magazine, 1960
- Potassium Content of Natural Plagioclases and the Origin of AntiperthitesThe Journal of Geology, 1959
- 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 Compositions of Coexisting Pyroxenes in Metamorphic AssemblagesGeological Magazine, 1958
- PROGRESSIVE METAMORPHISM AND GRANITIZATION OF THE MAJOR PARAGNEISS, NORTHWEST ADIRONDACK MOUNTAINS, NEW YORKGSA Bulletin, 1958
- Crystal Growth and the Distribution of ElementsThe Journal of Geology, 1955
- Thermometric and petrogenetic significance of titaniferous magnetiteAmerican Journal of Science, 1955
- XVIII.—The Geochemistry of the Charnockite Series of Madras, IndiaTransactions of the Royal Society of Edinburgh, 1955
- The Distribution of Fe++and Mg++in Coexisting Olivines and PyroxenesThe Journal of Geology, 1951