| Reference Type | Journal (article/letter/editorial) |
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| Title | Studies on the zeolites. Part II. Thomsonite (including faroelite) and gonnardite |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Hey, Max H. | Author |
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| Year | 1932 (June) | Volume | 23 |
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| Issue | 137 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_23/23-137-51.pdf+ |
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| DOI | doi:10.1180/minmag.1932.023.137.01 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 7136 | Long-form Identifier | mindat:1:5:7136:3 |
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| GUID | 0 |
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| Full Reference | Hey, Max H. (1932) Studies on the zeolites. Part II. Thomsonite (including faroelite) and gonnardite. Mineralogical Magazine and Journal of the Mineralogical Society, 23 (137) 51-125 doi:10.1180/minmag.1932.023.137.01 |
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| Plain Text | Hey, Max H. (1932) Studies on the zeolites. Part II. Thomsonite (including faroelite) and gonnardite. Mineralogical Magazine and Journal of the Mineralogical Society, 23 (137) 51-125 doi:10.1180/minmag.1932.023.137.01 |
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| In | (1932) Mineralogical Magazine Vol. 23 (137) Mineralogical Society |
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| Abstract/Notes | Thomsonite was first recognized by H. J. Brooke (1820) in a JL study of the mesotypes or 'needlestones'. The 'needlestone' of Lochwinnoch and Old Kilpatrick, Dumbartonshire, was found to be an independent species, in addition to the natrolite, mesolite, and scolecite into which k. F. Gehlen and J. N. Fachs, and J. N. Fuchs, had divided the mesotype of R. J. Haüy. The new species was named thomsonite, in honour of Dr. T. Thomson, who analysed the material a few months later. |
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These are possibly similar items as determined by title/reference text matching only.
