Snježana Musa

Nusret Drešković

 

MOKRO POLJE U ZAPADNOJ HERCEGOVINI – PULL-APART STRUKTURA

 

DOI: 10.35666/28310438.2001.1.197  

UDC: 911.2:551.435.8(497.5-14Mokro polje)

 

Abstract: There are several small karst field (polje) in the karst relief of West Herzegovina. These fields are representing accumulation-tectonical morphostructure. In the structural-geomorphological sense those fields are trenches. On of those is Mokro polje. Mokro polje is accumulation-tectonical morphostructure. Geotectonical frame of appearing of this structure is default anticlinala Rasno-Kosmaj. In this area there are several negative morophostructures: Trn, Mokro polje, Lipno. Disconformities of relief and orographic structure in this anticlinala can be related with appearing of transversal fault. Along this faults it has been developed tectonical trenches and halftrenches at on side, and mountains: Kosmaj, Drežanj, Oštri Humac and Buhovo on the other side. On of them – Mokro polje have a characteristics of pull-apart structure.

Key words: West Herzegovina, accumulation-tectonical morphostructure, tectonical trenches, Mokro field, pull apart structure.

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