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Title:Anomalous shallow fault creeping event on the Idrija Fault in summer 2025
Authors:ID Novak, Uroš (Author)
ID Bilham, Roger (Author)
ID Vičič, Blaž (Author)
ID Aoudia, Abdelkrim (Author)
Files:URL URL - Source URL, visit https://fgg-web.fgg.uni-lj.si/SUGG/referati.htm
 
.pdf PDF - Presentation file, download (10,87 MB)
MD5: 0E94C922183A20E5ED39B8657E76FA7B
 
Language:English
Typology:1.08 - Published Scientific Conference Contribution
Organization:Logo ZRC SAZU - The Research Centre of the Slovenian Academy of Sciences and Arts
Abstract:The Idrija Fault, a dextral strike-slip structure crossing the karstified carbonate Dinarides, exhibits complex shallow deformation strongly influenced by hydrological processes. Two Hall-effect creepmeters installed 8 km apart at Oblakov vrh and Kanomlja recorded abrupt shallow slip events of 0.15–0.50 mm during summer 2025. These slip episodes lasted up to 40 hours, consistent with creeping behavior and occurred without any accompanying seismicity, with regional earthquake magnitudes and frequencies remaining low. The last significant events were the 1998 and 2004 Posočje earthquakes. The observed deformation patterns cannot be explained by uniform tectonic slip and instead indicate different local mechanisms, including rainfall-driven pore-pressure diffusion, barometric pressure changes, karstic fluid pathways, and possibly shallow mass movement, that act along the fault. The observations highlight the strong coupling between hydrology, karst processes, and shallow fault mechanics, demonstrating that to some degree environmental controls dominate near-surface fault deformation on the Idrija Fault.
Keywords:Idrija Fault, shallow creep, active faulting, hydrological deformation, karst, Dinarides
Publication status:Published
Publication version:Version of Record
Year of publishing:2026
Number of pages:str. 67-71
PID:20.500.12556/DiRROS-28039 New window
UDC:551.243.1:556
COBISS.SI-ID:269995523 New window
Note:Besedilo v angl.;
Publication date in DiRROS:07.03.2026
Views:36
Downloads:22
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Record is a part of a monograph

Title:Raziskave s področja geodezije in geofizike 2025 : zbornik del : 31. srečanje Slovenskega združenja za geodezijo in geofiziko, Ljubljana, 5. februar 2026
Editors:Miran Kuhar, Matjaž Ličer, Ina Cecić, Mojca Šraj, Gregor Skok, Klemen Medved, Mihaela Triglav Čekada, Rudi Čop, Nina Zupančič, Tamara Jesenko, Polona Vreča
Place of publishing:Ljubljana
Publisher:Slovensko združenje za geodezijo in geofiziko
Year of publishing:2026
COBISS.SI-ID:268968195 New window

Document is financed by a project

Funder:ARIS - Slovenian Research and Innovation Agency
Project number:P6-0119
Name:Raziskovanje krasa

Funder:EC - European Commission
Project number:101131592
Name:EPOS Optimization and EvolutioN
Acronym:EPOS ON

Funder:EC - European Commission
Project number:101188365
Name:TowaRds AdvaNced multidiSciplinary Fault ObseRvatory systeMs²
Acronym:TRANSFORM2

Funder:ARIS - Slovenian Research and Innovation Agency
Project number:I0-E017
Name:Sofinanciranje izvajanja mednarodnega infrastrukturnega projekta EPOS

Secondary language

Language:Slovenian
Title:Nenavadno plitvo lezenje Idrijskega preloma poleti 2025
Abstract:Idrijski prelom, desno zmični prelom, ki seka močno zakrasele karbonatne Dinaride, kaže zapletene plitve deformacije skorje, ki so močno pod vplivom hidroloških procesov. Dva Hall-ova creepmetra, postavljena 8 km narazen na Oblakovem vrhu in v Kanomlji, sta poleti 2025 zabeležila nenadne plitve zdrse v velikosti 0,15–0,50 mm. Ti zdrsi so trajali do 40 ur, kar je značilno za lezenje, in so potekali brez kakršnekoli spremljajoče seizmične aktivnosti; magnituda in frekvenca regionalnih potresov sta ostali nizki. Zadnja pomembnejša potresa v širšem območju sta bila Posoška potresa leta 1998 in 2004. Zaznane deformacije ni mogoče razložiti z enotnim tektonskim (seizmičnim) zdrsom in kažejo, da vzdolž preloma delujejo različni lokalni aseizmični mehanizmi, med drugim padavinsko povzročena difuzija pornega tlaka, spremembe zračnega tlaka, pretakanje vode v kraških kanalih ter verjetno tudi plitvo premikanje pobočja. Opažanja poudarjajo močno povezanost med hidrologijo, kraškimi procesi in plitvo prelomno-mehaniko, kar kaže, da okoljski dejavniki v določeni meri prevladujejo pri plitvih deformacijah vzdolž Idrijskega preloma.
Keywords:Idrijski prelom, plitvo lezenje, aktivno prelamljanje, hidrološke deformacije, kras, Dinaridi


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