The Internal Organization of Speleothems
Siga se izloča kot sekudarni jamski mineral, njeno notranjo zgradbo lahko preučujemo z mineraloškimi metodami. Ontogenija mineralov je metoda, razvita v Rusiji, pri kateri so posamezni kristali in njihovi agregati preučevani kot fi zična telesa in ne kot mineralna vrsta. Članek podaja kratek vodnik...
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| Format: | Article |
| Language: | English |
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Slovenian Academy of Sciences and Arts
2016-05-01
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| Series: | Acta Carsologica |
| Online Access: | https://ojs.zrc-sazu.si/carsologica/article/view/327 |
| Summary: | Siga se izloča kot sekudarni jamski mineral, njeno notranjo zgradbo lahko preučujemo z mineraloškimi metodami. Ontogenija mineralov je metoda, razvita v Rusiji, pri kateri so posamezni kristali in njihovi agregati preučevani kot fi zična telesa in ne kot mineralna vrsta. Članek podaja kratek vodnik po terminologiji ontogenije s poudarkom na jamskih mineralih.
Speleothems are secondary cave mineral deposits whose internal organization can be studied by mineralogical techniques. The ontogeny of minerals is a technique developed in Russia whereby individual crystals and their aggregates are studied as physical bodies rather than as mineral species. This paper gives a concise guide to the terminology of ontogeny, as applied to cave mineral deposits. |
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| ISSN: | 0583-6050 1580-2612 |