Published June 1977
| Published
Journal Article
Open
Titanium and Aluminum in Biotite From High-Grade Archaean Gneisses, Langø, West Greenland
- Creators
- Dymek, R. F.
- Albee, A. L.
Chicago
Abstract
Biotite grains from a variety of gneiss types were analyzed by electron microprobe techniques for Na, Mg, Al, Si, K, Ca, Ti, Mn, Fe, Zn, F & Cl. TiO_2- and Al_2O_3-contents range continuously from < 0.1 to 6.0 and 13.9 to 20.6 wt % respectively. Most occur with ilmenite, but a few coexist with rutile. Biotite in pyribolite contains the least Al, and that in Kfeld-sill gneiss contains the most, suggesting that Al-content of biotite is related to the bulk composition of the host rock. For a given rock type, Ti in biotite tends to decrease as Mg/Fe and Al increase.
Additional Information
© 1977 American Geophysical Union.Attached Files
Published - Albee_1977p525.pdf
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- 39794
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- CaltechAUTHORS:20130806-152922789
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2013-08-09Created from EPrint's datestamp field
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- Division of Geological and Planetary Sciences (GPS)