Compositional and volume changes accompanying progressive serpentinization of dunites from the Webster-Addie ultramafic body, North Carolina

K.C. Condie*, J.A. Madison

*Corresponding author for this work

Research output: Contribution to journalArticle

12 Citations (Scopus)

Abstract

Chemical and modal analyses of 22 partially serpentinized dunites from the Webster-Addie ultramafic body in North Carolina suggests losses of Mg and Fe, additions of Si and Na, and an increase in volume during progressive serpentinization of the dunites.

Original languageEnglish
Pages (from-to)1173-1179
Number of pages7
JournalAmerican Mineralogist
Volume54
Issue number7-8
Publication statusPublished - Jul 1969
Externally publishedYes

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