Glaucochroite (olivine, CaMnSiO4) from Franklin, New Jersey: its composition, occurrence, and formation.

P. B. Leavens, P. J. Dunn, Donald Burt

Research output: Contribution to journalArticle

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Abstract

Habit, association, chemistry and manner of formation are analysed for glaucochroite, a member of the olivine group, known primarily from the Zn-Mn-Fe deposit at Franklin, New Jersey. Cuspidine, Ca4Si2O7(F,OH)2, is confirmed as occurring at Franklin. It occurs with glaucochroite and hardystonite, and in solution vugs in willemite.-J.A.Z.

Original languageEnglish (US)
Pages (from-to)423-428
Number of pages6
JournalAmerican Mineralogist
Volume72
Issue number3-4
StatePublished - 1987
Externally publishedYes

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olivine group
habits
olivine
Deposits
deposits
Association reactions
occurrences
chemistry
Chemical analysis
zinc silicate

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geophysics

Cite this

Glaucochroite (olivine, CaMnSiO4) from Franklin, New Jersey : its composition, occurrence, and formation. / Leavens, P. B.; Dunn, P. J.; Burt, Donald.

In: American Mineralogist, Vol. 72, No. 3-4, 1987, p. 423-428.

Research output: Contribution to journalArticle

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