Summary: An account is given of the mineralogy and chemistry of the ‘pseudo-diorites’ of Dielette, the hornfelses from which they are derived, and the contami-nated granite veins associated with them.
Mineralogical Magazine; 1965 v. 34; no. 268; p. 389-395; DOI: 10.1180/minmag.1965.034.268.33
© 1965, The Mineralogical Society
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