{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,11,28]],"date-time":"2025-11-28T04:58:40Z","timestamp":1764305920951,"version":"build-2065373602"},"reference-count":0,"publisher":"Association of Lithuanian Serials (Publications)","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":[],"published-print":{"date-parts":[[2021]]},"abstract":"<jats:p>This study presents a detailed spatiotemporal analysis for the Frakull-Durr\u00ebs (F-D) fault zone at the beginning of 2020. For this purpose, the most frequently used statistical seismicity parameters such as magnitude completeness, Mc-value, Gutenberg-Richter b-value, recurrence times, annual probabilities and standard normal deviate, Z-value, were mapped. The F-D fault zone was divided into two seismogenic subregions, and Mc-value was taken as 2.5 for both the south and north parts. The b-value was estimated as 0.83 \u00b1 0.06 for the south part and 0.85 \u00b1 0.06 for the north part. b-values for both zones are smaller than 1.0 and these values may be considered to be a larger stress accumulation to build up over time and to be released by the next possible earthquakes. Clear decreasing trends were observed in time variations of b-values before the occurrences of several strong main shocks. Analyses of annual probabilities and recurrence times suggest that the study region has an intermediate\/long-term earthquake hazard in comparison to occurrences of strong\/destructive earthquakes in the short term. Some anomaly regions of a small b-value and a large Z-value were found along the F-D fault zone at the beginning of 2020: i) among Lushnje-Tirana-Durr\u00ebs including the middle part of the F-D fault zone, ii) in and around Lezha including the north end of the F-D fault zone. Thus, the combination of regions with the lowest b-value and largest Z-value may supply preliminary results for earthquake hazard, and these regions may be considered to be the most likely regions for future strong\/large earthquakes in the F-D fault zone.<\/jats:p>","DOI":"10.5200\/baltica.2021.1.5","type":"journal-article","created":{"date-parts":[[2022,2,21]],"date-time":"2022-02-21T05:30:26Z","timestamp":1645421426000},"page":"58-70","source":"Crossref","is-referenced-by-count":2,"title":["A comprehensive spatiotemporal evaluation of the current earthquake activity in different parts of the Frakull-Durr\u00ebs fault zone, Albania"],"prefix":"10.5200","author":[{"given":"Serkan","family":"\u00d6zt\u00fcrk","sequence":"first","affiliation":[{"name":"G\u00fcm\u00fc\u015fhane University, Turkey"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Rrapo","family":"Ormeni","sequence":"additional","affiliation":[{"name":"Polytechnic University of Tirana, Albania"}],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"28932","published-online":{"date-parts":[[2021]]},"container-title":["Baltica"],"original-title":[],"language":"en","link":[{"URL":"https:\/\/baltica.gamtc.lt\/administravimas\/uploads\/202134-105_ozturk_et_ormeni_60ade716a3961.pdf","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2025,11,7]],"date-time":"2025-11-07T14:02:16Z","timestamp":1762524136000},"score":1,"resource":{"primary":{"URL":"https:\/\/baltica.gamtc.lt\/lt\/publication\/309\/a-comprehensive-spatiotemporal-evaluation-of-the-current-earthquake-activity-in-different-parts-of-the-frakull-durres-fault-zone-albania"}},"subtitle":[],"short-title":[],"issued":{"date-parts":[[2021]]},"references-count":0,"URL":"https:\/\/doi.org\/10.5200\/baltica.2021.1.5","relation":{},"ISSN":["0067-3064"],"issn-type":[{"type":"print","value":"0067-3064"}],"subject":[],"published":{"date-parts":[[2021]]}}}