Abstract
The motorway tunnel Golo rebro is situated on Styrian motorway. It intersects eastern part of Konjiška gora. From the north to the south it intersects the following rocks: paleozoic clastic rocks (inner part of the Labot/Lavanttal fault zone), slope debris with clay matrix (probabbly of tertiary or quartenary age), dolomite, dolomitized limestone and limestone, carbonate breccia and dolomite, dolomitized limestone and limestone, which are partly converted into tectonic breccia. Carbonate rocks are of middle triassic - anisian age. Rocks are strongly tectonised.
Highlights
The motorway tunnel Golo rebro is situated on Styrian motorway
From the north to the south it intersects the following rocks: paleozoic clastic rocks, slope debris with clay matrix, dolomite, dolomitized limestone and limestone, carbonate breccia and dolomite, dolomitized limestone and limestone, which are partly converted into tectonic breccia
Carbonate rocks are of middle triassic - anisian age
Summary
Ključne besede: Konjiška gora, predor, Labotska prelomna cona, paleozojske klastične kamnine, triasne karbonatne kamnine, tektonizirane kamnine, Slovenija. Key voords: Konjiška gora, tunnel, Labot/Lavanttal fault zone, paleozoic clastic rocks, triassic carbonate rocks, tectonised rocks, Slovenia. Izvleček Avtocestni predor Golo rebro se nahaja na štajerski avtocesti na vzhodnem delu Konjiške gore. V smeri od severa proti jugu preseka sledeče kamninske odseke: paleozojske klastične kamnine (ožje območje Labotske prelomne cone), močno zaglinjen grušč (verjetno terciarne ali kvartarne starosti), dolomit, dolomitiziran apnenec in apnenec, karbonatno brečo ter dolomit, dolomitiziran apnenec in apnenec, delno spremenjene v tektonsko brečo. Karbonatne kamnine so srednje triasne - anizijske starosti.
Sign-in/Register to view highlights & summary Sign-in/Register to access full text options 
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
