| Reference Type | Journal (article/letter/editorial) |
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| Title | IV.—Narrative of a Geological Journey through Russia |
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| Journal | Geological Magazine |
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| Year | 1898 (March) | Series:Volume | 4:5 |
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| Page(s) | 110-116 | Issue | 3 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800141536 |
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| Mindat Ref. ID | 267786 | Long-form Identifier | mindat:1:5:267786:0 |
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| GUID | f9bc3fe0-46ad-4598-bacc-891e8512b8d4 |
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| Full Reference | (1898) IV.—Narrative of a Geological Journey through Russia. Geological Magazine, S. 4 Vol. 5 (3) 110-116 doi:10.1017/s0016756800141536 |
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| Plain Text | (1898) IV.—Narrative of a Geological Journey through Russia. Geological Magazine, S. 4 Vol. 5 (3) 110-116 doi:10.1017/s0016756800141536 |
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| In | (1898, March) Geological Magazine S. 4 Vol. 5 (3) Cambridge University Press (CUP) |
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| Abstract/Notes | Proceeding in a westerly direction from Tammerfors, we stopped near the station of Siuro to examine some railway cuttings where good sections of gneissose rock and mica-schist, both of Pre-Bothnian age, occur. Macroscopically, the gneissose rock is distinctly and regularly foliated, having small, lenticular, streaks of quartz abundantly disseminated. Locally, however, the section in the field exhibits much contortion; and thin, irregular, veins of quartz, manifestly of secondary origin, are not uncommon. |
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