Summary: A number of minerals and residual glasses from absarokites, shoshonites, and latites have been analysed by electron probe.
Clinopyroxenes show very little iron-enrichment and these rocks are thus distinguished from tholeiites and alkali basalts.
Glasses from this group are also distinct from tholeiites and alkali basalts and occupy a separate field on a CaO-Na2O-K2O diagram.
Mineralogical Magazine; December 1972 v. 38; no. 300; p. 936-945; DOI: 10.1180/minmag.1972.038.300.04
© 1972, The Mineralogical Society
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