| Reference Type | Journal (article/letter/editorial) |
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| Title | A Heteromorph of Venanzite |
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| Journal | Geological Magazine |
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| Authors | Holmes, Arthur | Author |
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| Year | 1942 (August) | Volume | 79 |
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| Issue | 4 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s001675680007391x |
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| Generate Citation Formats |
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| Mindat Ref. ID | 247276 | Long-form Identifier | mindat:1:5:247276:2 |
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| GUID | 0 |
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| Full Reference | Holmes, Arthur (1942) A Heteromorph of Venanzite. Geological Magazine, 79 (4) 225-232 doi:10.1017/s001675680007391x |
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| Plain Text | Holmes, Arthur (1942) A Heteromorph of Venanzite. Geological Magazine, 79 (4) 225-232 doi:10.1017/s001675680007391x |
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| In | (1942, August) Geological Magazine Vol. 79 (4) Cambridge University Press (CUP) |
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| Abstract/Notes | Venanzite. Venanzite is a volcanic rock consisting essentially of y melilite, leucite, olivine, and a little phlogopitic biotite, which occurs as small lava-flows of late- or post-Pliocene age near San Venanzo, Umbria, Italy. This isolated centre of activity lies north-west of Lake Bolsena and is regarded as an outlying part of the Vulsinian district of the Roman netroaranhic nrovince. |
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