Microstructures in titanomagnetites as guides to cooling rates of a Swedish intrusion
- 1 July 1979
- journal article
- research article
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 116 (4), 313-318
- https://doi.org/10.1017/s001675680004379x
Abstract
Summary: Iron-titanium oxides from Taberg in Sweden exhibit under the electron microscope several microstructural features not visible when studied by optical microscopy, including homogeneous nucleation of magnetitess from ulvöspinelss, and the spinodal decomposition of magnetitesss. Such microstructures have promise as indicators of cooling rates.This publication has 11 references indexed in Scilit:
- Nucleation of augite at antiphase boundaries in pigeonitePhysics and Chemistry of Minerals, 1978
- Kinetic processes and thermal history of slowly cooling solidsNature, 1976
- Microstructures of Minerals as Petrogenetic IndicatorsAnnual Review of Earth and Planetary Sciences, 1975
- The nature of dark-etching rims in meteoritic taeniteGeochimica et Cosmochimica Acta, 1973
- Closure temperature in cooling geochronological and petrological systemsContributions to Mineralogy and Petrology, 1973
- Tracer Diffusion Data for Metals, Alloys, and Simple OxidesPublished by Springer Nature ,1970
- Kinetics and mechanisms of exsolutionChemical Geology, 1970
- Iron-Titanium Oxide Minerals and Synthetic EquivalentsJournal of Petrology, 1964
- Heating experiments on some natural titaniferous magnetitesMineralogical Magazine and Journal of the Mineralogical Society, 1957
- A ferro-ortho-titanate ore from Södra UlvönGeologiska Föreningen i Stockholm Förhandlingar, 1946