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Stručni rad

The Layer

Jasna Kos-Modor ; Faculty of Mining, Geology and Petroleum Engineering, University of Zagreb, Zagreb, Croatia
Ema Jurkin   ORCID icon orcid.org/0000-0002-8658-5446 ; Faculty of Mining, Geology and Petroleum Engineering, University of Zagreb, Zagreb, Croatia

Puni tekst: hrvatski, pdf (524 KB) str. 25-27 preuzimanja: 1.050* citiraj
APA 6th Edition
Kos-Modor, J. i Jurkin, E. (2003). Sloj. KoG, 7. (7.), 25-27. Preuzeto s https://hrcak.srce.hr/3922
MLA 8th Edition
Kos-Modor, Jasna i Ema Jurkin. "Sloj." KoG, vol. 7., br. 7., 2003, str. 25-27. https://hrcak.srce.hr/3922. Citirano 20.10.2021.
Chicago 17th Edition
Kos-Modor, Jasna i Ema Jurkin. "Sloj." KoG 7., br. 7. (2003): 25-27. https://hrcak.srce.hr/3922
Harvard
Kos-Modor, J., i Jurkin, E. (2003). 'Sloj', KoG, 7.(7.), str. 25-27. Preuzeto s: https://hrcak.srce.hr/3922 (Datum pristupa: 20.10.2021.)
Vancouver
Kos-Modor J, Jurkin E. Sloj. KoG [Internet]. 2003 [pristupljeno 20.10.2021.];7.(7.):25-27. Dostupno na: https://hrcak.srce.hr/3922
IEEE
J. Kos-Modor i E. Jurkin, "Sloj", KoG, vol.7., br. 7., str. 25-27, 2003. [Online]. Dostupno na: https://hrcak.srce.hr/3922. [Citirano: 20.10.2021.]

Sažetak
The layer is the basic unit of sediment rocks. In the projection with heights the presentation of the regular layer limited with two parallel planes is shown. Profile of the layer is constructed and the thickness and inclination of layer are determined. Two cases of setting and solving the layer are demonstrated.

Ključne riječi
projection with heights; layer; outcrop line; thickness of layer

Hrčak ID: 3922

URI
https://hrcak.srce.hr/3922

[hrvatski]

Posjeta: 1.462 *