Skoči na glavni sadržaj

KoG, Vol. 8. No. 8., 2004.

Stručni rad

Faults

Jasna Kos-Modor ; Rudarsko-geološko-naftni fakultet Sveučilišta u Zagrebu, Zagreb, Croatia
Ema Jurkin orcid id orcid.org/0000-0002-8658-5446 ; Rudarsko-geološko-naftni fakultet Sveučilišta u Zagrebu, Zagreb, Croatia

Puni tekst: hrvatski pdf 443 Kb

str. 17-20

preuzimanja: 3.171

citiraj

Sažetak

The faults are basic structural units of lithosphere. They begin to create by the cracking and moving of the rocks because of the gravitation, expansion or compression forces. Two blocks of the rocks are formed, fault walls - hanging wall and foot wall, which are moving along the fault plane. In view of the moving of the hanging wall with respect to the foot wall, we distinguish the normal fault and the reverse fault. In the projection with heights, the normal fault and the reverse fault with two profiles are shown.

Ključne riječi

projection with heights; fault; fault plane; fault walls

Hrčak ID:

3709

URI

https://hrcak.srce.hr/3709

Datum izdavanja:

17.2.2005.

Podaci na drugim jezicima: hrvatski

Posjeta: 4.783 *