The Internal Organization of Speleothems

Authors

  • Charles A. Self 4 Tyne Street, Bristol, BS2 9UA

DOI:

https://doi.org/10.3986/ac.v33i1.327

Abstract

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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Published

2016-05-19

How to Cite

Self, C. A. (2016). The Internal Organization of Speleothems. Acta Carsologica, 33(1). https://doi.org/10.3986/ac.v33i1.327

Issue

Vol. 33 No. 1 (2004)

Section

Original papers

License

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