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Title:Geologic structure and origin of the Zadlog karst polje
Authors:ID Čar, Jože (Author)
ID Šegina, Ela (Author)
Files:.pdf PDF - Presentation file, download (30,85 MB)
MD5: B62C8C673FD523952A82D7B1E48DF71D
 
Language:English
Typology:1.01 - Original Scientific Article
Organization:Logo GeoZS - Geological Survey of Slovenia
Abstract:In the wider Idrija area in western Slovenia, several large plains formed along the thrusts within the dolomite and at the contact of dolomite and limestone. The purpose of this paper is to present the detailed structural-geological background of one such plain, namely the Zadlog plain, and based on these findings, to provide new starting points for analyzing the genetic conditions of other karst poljes in Notranjska. The Zadloško polje was formed in a wider near-fault crushed zone at the contact of two structural units within the Upper Triassic Norian-Rhaetian dolomite, with the thrust crossing the polje in its central part. The initially lowered area at the thrust represented a morphological basis, and the crushed zones in the dolomite played a hydrological retention role inducing the stagnation of surface water and, as a result, the formation of the karst polje. Younger fault tectonics then established efficient drainage of surface water and the erosion of sediments to the karst underground. Besdies this, slope equilibration leads us to conclude that the karst polje capability of hydrologic retention is recently decreased. The example of Zadloško polje shows that the thrust structures and associated hydrological conditions are the key elements for the formation of karst poljes in the dissected karst surface. Further detailed structural-geological mapping will reveal whether similar structural-geological conditions are the basis for the formation of other karst poljes in the region.
Keywords:karst polje, thrust and fault tectonics, dolomite, hydrogeology, Zadlog, Zadloško polje
Publication status:Published
Publication version:Version of Record
Publication date:16.12.2024
Year of publishing:2024
Number of pages:str. 249-271
Numbering:vol. 67, no. 2
PID:20.500.12556/DiRROS-22460 New window
UDC:551.44
ISSN on article:0016-7789
DOI:10.5474/geologija.2024.012 New window
COBISS.SI-ID:220235779 New window
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Publication date in DiRROS:21.05.2025
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Downloads:164
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Record is a part of a journal

Title:Geologija
Shortened title:Geologija
Publisher:Geološki zavod Slovenije
ISSN:0016-7789
COBISS.SI-ID:5636866 New window

Document is financed by a project

Funder:ARIS - Slovenian Research and Innovation Agency
Project number:P1-0419-2022
Name:Dinamična Zemlja

Licences

License:CC BY 4.0, Creative Commons Attribution 4.0 International
Link:http://creativecommons.org/licenses/by/4.0/
Description:This is the standard Creative Commons license that gives others maximum freedom to do what they want with the work as long as they credit the author.

Secondary language

Language:Slovenian
Title:Geološka zgradba in nastanek kraškega polja Zadlog
Abstract:Vzdolž narivov znotraj dolomita in narivov na kontaktu dolomita in apnenca so na Idrijskem v zahodni Sloveniji mestoma nastale večje izravnave. Namen tega prispevka je predstaviti podrobno strukturno-geološko ozadje ene takih izravnav, in sicer Zadloške uravnave in na podlagi teh ugotovitev podati nova izhodišča za prevetritev genetskih razmer tudi drugih kraških polj na Notranjskem. Zadloško polje je tako nastalo v razširjeni obprelomni zdrobljeni coni ob stiku dveh strukturnih enot znotraj zgornjetriasnega norijsko-retijskega dolomita, pri čemer narivnica prečka polje v njegovem osrednjem delu. Začetna obnarivna izravnava je predstavljala morfološko zasnovo, zdrobljeni coni v dolomitu pa sta imeli ključno vodno-zadrževalno vlogo pri zastajanju površinske vode in posledično pri nastanku kraškega polja. Mlajša prelomna tektonika je nato vzpostavila efektivno odvajanje voda in odnašanje sedimentov v kraško podzemlje. Prav tako opazujemo uravnavanje pobočij izravnave, zaradi česar menimo, da je vodno-zadrževalna sposobnost kraškega polja recentno zmanjšana. Primer Zadloškega polja kaže, da so narivna zgradba in z njo povezane hidrološke razmere ključni element za oblikovanje kraškega polja v razčlenjenem kraškem površju. Ali so podobne strukturno-geološke razmere osnova nastanka tudi ostalih kraških polj v regiji, bo razkrilo nadaljnje podrobno strukturno-geološko kartiranje.
Keywords:kraško polje, narivna in prelomna tektonika, dolomit, hidrogeologija, Zadlog, Zadloško polje


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