{"id":64997,"date":"2025-05-15T13:59:35","date_gmt":"2025-05-15T10:59:35","guid":{"rendered":"https:\/\/bilimvegelecek.com.tr\/?p=64997"},"modified":"2025-05-15T13:59:35","modified_gmt":"2025-05-15T10:59:35","slug":"19-nisan-2025-simav-nasa-fay-kusagi-deprem-firtinasinin-sismolojik-ozellikleri","status":"publish","type":"post","link":"https:\/\/bilimvegelecek.com.tr\/index.php\/2025\/05\/15\/19-nisan-2025-simav-nasa-fay-kusagi-deprem-firtinasinin-sismolojik-ozellikleri","title":{"rendered":"19 Nisan 2025 Simav Na\u015fa Fay Ku\u015fa\u011f\u0131 deprem f\u0131rt\u0131nas\u0131n\u0131n sismolojik \u00f6zellikleri"},"content":{"rendered":"

Prof. Dr. Haluk Eyido\u011fan<\/strong><\/p>\n

22 Nisan 2025 tarihinde bas\u0131na yans\u0131yan deprem haberlerinden birinin ba\u015fl\u0131\u011f\u0131 \u015f\u00f6yleydi; \u201cK\u00fctahya\u2019da yeni fay hatt\u0131 ortaya \u00e7\u0131kt\u0131\u201d (Cumhuriyet Gazetesi, 22 May\u0131s 2025). K\u00fctahya Dumlup\u0131nar \u00dcniversitesi\u2019den Jeoloji Y\u00fcksek M\u00fchendisi Prof. Dr. Cafer \u00d6zkul, “K\u00fc\u00e7\u00fck \u00f6l\u00e7ekteki bu depremler, daha \u00f6nce tespit edilmemi\u015f ve haritalanmam\u0131\u015f bir yerde ger\u00e7ekle\u015fti<\/em>” yorumunu yapm\u0131\u015ft\u0131<\/p>\n

Habere konu olan deprem etkinli\u011fi K\u00fctahya Simav il\u00e7esinin kuzeyinde Yemi\u015fli K\u00f6y\u00fc \u00e7evresinde olrtaya \u00e7\u0131kan deprem f\u0131rt\u0131nas\u0131yd\u0131. Bu deprem etkinli\u011finin yeri incelendi\u011finde, depremin Simav il\u00e7esinin i\u00e7erisinden ge\u00e7en do\u011frultu at\u0131ml\u0131 fay (DA) olarak tescil edilen Simav Fay\u0131 (Emre vd, 2012, 2018) ile do\u011frudan ili\u015fkili olmad\u0131\u011f\u0131, ancak Ege b\u00f6lgesinde geli\u015fen geni\u015flemeli jeotektonik rejim ve Simav Fay\u0131\u2019n\u0131n k\u0131smen etkisi alt\u0131nda kuzeyde geli\u015fen Na\u015fa Fay Ku\u015fa\u011f\u0131 \u00e7evresinde, Yemi\u015fli K\u00f6y\u00fc do\u011fusunda olu\u015ftu\u011fu anla\u015f\u0131lm\u0131\u015ft\u0131r. Sismolojik g\u00f6zlemlerden hareketle yapt\u0131\u011f\u0131m inceleme ve de\u011ferlendirmem ile ilgili a\u00e7\u0131klamalar\u0131m a\u015fa\u011f\u0131daki yaz\u0131mda yer almaktad\u0131r.<\/p>\n

Simav Fay Ku\u015fa\u011f\u0131 do\u011frultu at\u0131ml\u0131 bir fayd\u0131r
\n<\/strong>K\u00fctahya\u2019n\u0131n Simav il\u00e7esi \u00fczerinden ge\u00e7en 205 km uzunlu\u011fundaki sa\u011f yanal do\u011frultu at\u0131ml\u0131 Simav Fay Ku\u015fa\u011f\u0131 KB-GD do\u011frultusunda uzanmakta olup, 7 fay par\u00e7as\u0131ndan (segment) olu\u015fmaktad\u0131r ( Emre vd, 2012, 2018).\u00a0 Sahada yap\u0131lan jeolojik-jeomorfolojik g\u00f6zlemler, GPS \u00f6l\u00e7\u00fcmleri, paleo-sismolojik bulgular ve deprem odak mekanizma \u00e7\u00f6z\u00fcmleri, Simav Fay Ku\u015fa\u011f\u0131\u2019n\u0131n do\u011frultu at\u0131ml\u0131 nitelikli bir kayma hareketi yapt\u0131\u011f\u0131n\u0131 g\u00f6stermektedir (Konak, 1982; Aktu\u011f vd, 2009; Duman vd, 2013; Emre vd, 2018). Simav Fay\u0131\u2019n\u0131n, Simav il\u00e7esine yak\u0131n \u00fc\u00e7 ana par\u00e7as\u0131 (segment), s\u0131ras\u0131yla bat\u0131dan do\u011fuya do\u011fru uzanan S\u0131nd\u0131rg\u0131 Fay\u0131, \u00c7aysimav Fay\u0131 ve \u015eaphane Fay\u0131\u2019d\u0131r (\u015eekil-1a,b,c\u00a0 ve \u00c7izelge-1). Simav Fay Ku\u015fa\u011f\u0131 do\u011fuda Afyon-Ak\u015fehir Graben Sistemi’ne ba\u011flanmaktad\u0131r. Simav Fay\u0131\u2019n\u0131n ba\u015fat do\u011frultu at\u0131m bile\u015feni yan\u0131 s\u0131ra \u00f6nemli bir e\u011fim at\u0131ml\u0131 bile\u015fenli deprem olup olmad\u0131\u011f\u0131 konusunda daha ayr\u0131nt\u0131l\u0131 ara\u015ft\u0131rmalar yap\u0131lmal\u0131d\u0131r.<\/p>\n

\"\"<\/p>\n

\"\"<\/p>\n

AFAD deprem ar\u015fivine g\u00f6re Simav Fay Ku\u015fa\u011f\u0131 ile Na\u015fa Fay Ku\u015fa\u011f\u0131\u2019n\u0131 kapsad\u0131\u011f\u0131 alanda 1900 ile 1 Mart 2025 tarihleri aras\u0131nda b\u00fcy\u00fckl\u00fc\u011f\u00fc 4.0 ve daha fazla olan depremlerin d\u0131\u015fmerkez da\u011f\u0131l\u0131ma bakt\u0131\u011f\u0131m\u0131zda (\u015eekil-1a), depremlerin b\u00fcy\u00fck \u00e7o\u011funlu\u011funun normal fay (NN) \u00f6zellikli Na\u015fa Fay Ku\u015fa\u011f\u0131 b\u00f6lgesinde kald\u0131\u011f\u0131 g\u00f6zlenmektedir. Na\u015fa Fay Ku\u015fa\u011f\u0131\u2019n\u0131n iki belirgin kolu vard\u0131r. Kuzeybat\u0131-g\u00fcneydo\u011fu uzan\u0131ml\u0131 bu kollar s\u0131ras\u0131yla Na\u015fa-2 ve Na\u015fa-3 olarak adland\u0131r\u0131lmaktad\u0131r (Emre vd, 2012, 2018).<\/p>\n

Google Earth \u00fczerinde Simav l\u00e7esinden Yemi\u015fli k\u00f6y\u00fcne do\u011fru bir profil \u00fczerinde topo\u011frafyaya bakt\u0131\u011f\u0131m\u0131zda, iki fay ku\u015fa\u011f\u0131 aras\u0131nda geli\u015fen \u00e7\u00f6k\u00fcnt\u00fc havzas\u0131 (graben) a\u00e7\u0131k bir bi\u00e7imde g\u00f6r\u00fclmektedir (\u015eekil-1b, c).\"\"<\/p>\n

19 Nisan 2025\u2019de say\u0131s\u0131 artarak ba\u015flayan ve Na\u015fa Fay Ku\u015fa\u011f\u0131\u2019n\u0131n kuzeyinde olu\u015fan deprem f\u0131rt\u0131nas\u0131 (\u015eekil-2), bu iki normal fay yap\u0131lar\u0131 aras\u0131nda kalmaktad\u0131r. Bas\u0131na \u201cdaha \u00f6nce ke\u015ffedilmemi\u015f\u201d<\/em> olarak yans\u0131yan tan\u0131mlama, herhalde kuzeybat\u0131ya do\u011fru uzanan Na\u015fa Fay Ku\u015fa\u011f\u0131 normal fay yap\u0131lar\u0131n\u0131n, normal faylanma mekanizmal\u0131 bu deprem f\u0131rt\u0131nas\u0131 (\u015eekil-3) ile ili\u015fkili\u00a0olmad\u0131\u011f\u0131 d\u00fc\u015f\u00fcncesinden hareketle yap\u0131lm\u0131\u015ft\u0131r. Jeolog ve jeofizik\u00e7ilerin, Na\u015fa Fay\u0131\u2019n\u0131n kuzeybat\u0131ya do\u011fru uzant\u0131s\u0131 konusunda daha fazla ara\u015ft\u0131rma yapmas\u0131 \u00e7ok yararl\u0131 olacakt\u0131r.<\/p>\n

19 May\u0131s 2011 tarihinde Simav il\u00e7e merkezinin kuzeydo\u011fusunda 5.7 b\u00fcy\u00fckl\u00fc\u011f\u00fcnde bir depremle ba\u015flayan ve Simav ve \u00e7evresinde geni\u015f alanda hasar yapan depremin ve art\u00e7\u0131 depremlerinin konumlar\u0131 ve sismolojik y\u00f6ntemlerle hesaplanan odak mekanizmas\u0131 \u00e7\u00f6z\u00fcmleri (AFAD) normal fay hareketi kaynakl\u0131 olup, Simav Fay\u0131\u2019n\u0131n do\u011frultu at\u0131ml\u0131 karakterini yans\u0131tmamaktad\u0131r (\u015eekil-3, \u00c7izelge-1). AFAD\u2019\u0131n yay\u0131nlad\u0131\u011f\u0131 ve do\u011fru oldu\u011funu kabul etti\u011fimiz bu bulgular\u0131 yorumlad\u0131\u011f\u0131m\u0131zda, 19 May\u0131s 2011 depreminin Simav Fay\u0131 ile de\u011fil Na\u015fa Fay Ku\u015fa\u011f\u0131\u2019n\u0131n g\u00fcneydo\u011fu kollar\u0131 ile ili\u015fkili\u00a0oldu\u011fu anla\u015f\u0131lmaktad\u0131r.\"\"<\/p>\n

Na\u015fa Fay Ku\u015fa\u011f\u0131 deprem f\u0131rt\u0131nas\u0131
\n<\/strong>Normal fay yap\u0131lar\u0131n\u0131n ve hareketlerinin yo\u011fun oldu\u011fu Ege b\u00f6lgesinde zaman zaman deprem f\u0131rt\u0131nalar\u0131 olmaktad\u0131r (Eyido\u011fan, 2020; USGS, 2025). Deprem f\u0131rt\u0131nas\u0131, genellikle b\u00fcy\u00fck ve \u00e7ok kuvvetli deprem i\u00e7ermeyen, k\u00fc\u00e7\u00fck ve orta kuvvette depremlerin yo\u011fun oldu\u011fu ve k\u00fcmelendi\u011fi bir deprem etkinli\u011fidir. Normal faylar\u0131n etkin oldu\u011fu tektonik alanlarda, bu t\u00fcr deprem etkinliklerine s\u0131k\u00e7a kar\u015f\u0131la\u015f\u0131l\u0131r. Bir s\u00fcre sonra, depremlerin b\u00fcy\u00fckl\u00fckleri ve say\u0131lar\u0131 azal\u0131r. B\u00fcy\u00fck deprem i\u00e7ermeyen ancak uzun s\u00fcren deprem etkinlikleri, sars\u0131nt\u0131lar\u0131n s\u00fcreklili\u011fi nedeniyle yak\u0131n yerle\u015fimlerde, ta\u015f\u0131ma g\u00fcc\u00fc d\u00fc\u015f\u00fck gev\u015fek zeminlerde ve dayan\u0131kl\u0131l\u0131k sorunu olan yap\u0131larda \u00f6nemli hasarlar yapabilirler.<\/p>\n

19 Nisan 2025 tarihinde belirginle\u015fen Na\u015fa Fay Ku\u015fa\u011f\u0131 deprem etkinli\u011fi (buradan itibaren \u201cdeprem f\u0131rt\u0131nas\u0131\u201d olarak adland\u0131r\u0131lacakt\u0131r<\/em>) asl\u0131nda 2 Mart 2025 tarihinde b\u00fcy\u00fckl\u00fc\u011f\u00fc 1.0 olan depremler ile ba\u015flam\u0131\u015f, en b\u00fcy\u00fc\u011f\u00fc 2.4 olan depremle s\u00fcrm\u00fc\u015f ve 7 adet deprem sonras\u0131 28 Mart 2025 tarihinde durmu\u015ftur. 19 Nisan 2025 tarihinde yeniden ba\u015flayan deprem etkinli\u011fi deprem f\u0131rt\u0131nas\u0131na d\u00f6n\u00fc\u015ferek, say\u0131s\u0131 ve b\u00fcy\u00fckl\u00fckleri giderek artan bir kimlik kazanmaya ba\u015flam\u0131\u015f ve ilgili kurumlar ve bas\u0131n arac\u0131l\u0131\u011f\u0131 ile duyurulmu\u015ftur.<\/p>\n

\"\"<\/p>\n

AFAD deprem verileri g\u00f6z \u00f6n\u00fcne al\u0131narak yapt\u0131\u011f\u0131m sismolojik incelemeye g\u00f6re 2 Mart 2025\u2018den 9 May\u0131s 2025 tarihleri aras\u0131nda Na\u015fa Fay Ku\u015fa\u011f\u0131 deprem f\u0131rt\u0131nas\u0131nda 966 adet deprem kaydedilmi\u015ftir. Bu depremlerin en k\u00fc\u00e7\u00fc\u011f\u00fc 1.0, en b\u00fcy\u00fc\u011f\u00fc ise 4.6 b\u00fcy\u00fckl\u00fc\u011f\u00fcnde olmu\u015ftur. Deprem f\u0131rt\u0131nas\u0131 i\u00e7erisindeki depremlerin b\u00fcy\u00fckl\u00fcklerini tarih s\u0131ras\u0131na g\u00f6re grafikledi\u011fimizde \u015eekil-4a\u2019da verilen g\u00f6r\u00fcn\u00fcm elde edilmi\u015ftir. Buna g\u00f6re Na\u015fa Fay Ku\u015fa\u011f\u0131\u2019n\u0131n kuzey b\u00f6lgesinde ba\u015flayan etkinlik d\u00f6rt farkl\u0131 \u201cdepremsellik devresi\u201d sergilemektedir. B\u00fcy\u00fckl\u00fckleri 3.0 ve daha fazla olan deprem say\u0131s\u0131n\u0131n d\u00f6rt farkl\u0131 devrede say\u0131lar\u0131 \u015f\u00f6yledir: Birinci devrede 2 deprem, ikinci devrede 2 deprem, \u00fc\u00e7\u00fcnc\u00fc devrede 5 deprem ve d\u00f6rd\u00fcnc\u00fc devrede 13 deprem say\u0131lm\u0131\u015ft\u0131r. Deprem f\u0131rt\u0131nas\u0131 s\u00fcrecinde en b\u00fcy\u00fck deprem olan 4.6 b\u00fcy\u00fckl\u00fc\u011f\u00fcndeki deprem \u00fc\u00e7\u00fcnc\u00fc devrede olmu\u015f, d\u00f6rt devrenin toplam\u0131nda b\u00fcy\u00fckl\u00fc\u011f\u00fc 4.0 ve daha fazla olan deprem say\u0131s\u0131 6 adet olmu\u015ftur (\u015eekil-4a).<\/p>\n

Deprem f\u0131rt\u0131nas\u0131n\u0131n enlem de\u011fi\u015fkenine g\u00f6re konum ve b\u00fcy\u00fckl\u00fck grafi\u011fi ise \u015eekil-4b\u2019de verilmi\u015ftir. Grafikteki de\u011fi\u015fim incelendi\u011finde 4.6 b\u00fcy\u00fckl\u00fc\u011f\u00fcndeki depremin oldu\u011fu \u00fc\u00e7\u00fcnc\u00fc devrede deprem f\u0131rt\u0131nas\u0131 etkinli\u011fi g\u00fcneye do\u011fru g\u00f6\u00e7 etmi\u015f (\u015eekil-2), izleyen g\u00fcnlerde g\u00fcney do\u011fru g\u00f6\u00e7 d\u00f6rd\u00fcnc\u00fc devrede 24 Nisan 2025 tarihinde en belirgin duruma gelmi\u015ftir. 9 May\u0131s 2025 tarihi itibariyle oransal olarak say\u0131s\u0131 ve b\u00fcy\u00fckl\u00fckleri azalm\u0131\u015ft\u0131r.<\/p>\n

Sonu\u00e7
\n<\/strong>K\u00fctahya, Simav il\u00e7esi kuzeyinde Yemi\u015fli K\u00f6y\u00fc \u00e7evresinde 2 Mart 2025 tarihinde ba\u015flayan deprem f\u0131rt\u0131nas\u0131 s\u0131ras\u0131nda 9 May\u0131s 2025 tarihine kadar, b\u00fcy\u00fckl\u00fc\u011f\u00fc 1.0 ile 4.6 aras\u0131nda 966 adet deprem olmu\u015ftur. Depremler, Simav kuzeyinde kuzeybat\u0131-g\u00fcneydo\u011fu do\u011frultusunda uzanan Na\u015fa Fay Ku\u015fa\u011f\u0131\u2019n\u0131n kuzeybay\u0131 ucunda ger\u00e7ekle\u015fmi\u015ftir. Sismolojik y\u00f6ntemlerle hesap edilen odak mekanizmas\u0131 \u00e7\u00f6z\u00fcmleri, deprem f\u0131rt\u0131nas\u0131n\u0131n normal fay hareketlili\u011fi ile ilgili oldu\u011funu g\u00f6stermi\u015ftir. 19 Nisan 2025 tarihinde yo\u011funla\u015fan deprem etkinli\u011fi zaman i\u00e7erisinde d\u00f6rt devre \u015feklinde s\u00fcrm\u00fc\u015ft\u00fcr. Deprem f\u0131rt\u0131nas\u0131n\u0131n zaman ve mekandaki sismolojik \u00f6zellikleri, Na\u015fa Fay Ku\u015fa\u011f\u0131\u2019n\u0131n kuzeybat\u0131 b\u00f6lgesinin jeotektonik \u00f6zelliklerinin daha ayr\u0131nt\u0131l\u0131 ara\u015ft\u0131r\u0131lmas\u0131 gerekti\u011fini g\u00f6stermektedir.<\/p>\n

KAYNAKLAR<\/strong><\/p>\n

-Aktu\u011f, B., Nocquet, J. M., Cing\u00f6z, A., Parsons, A., Erkan, Y., England, P., Lenk, O., G\u00fcrdal, M.A., K\u0131l\u0131\u00e7o\u011flu, A., Akdeniz, H., Tekg\u00fcl, A., 2009. Deformation of western Turkey from a combination of permanent and campaign GPS data: limits to block-like behaviour. J Geophys Res. doi:1029\/2008jb006000<\/p>\n

-Cumhuriyet Gazetesi (22 May\u0131s 2025) https:\/\/www.cumhuriyet.com.tr\/turkiye\/yaklasik-50-sarsinti-olmustu-kutahyada-yeni-fay-hatti-ortaya-cikti-2321408<\/p>\n

-Duman, T.Y., Elmac\u0131 H, \u00d6zalp S, Olgun, \u015e., Emre, \u00d6., 2013. Simav Fay Zonunda ilk paleosismolojik bulgular. 66. T\u00fcrkiye Jeoloji Kurultay\u0131, 1\u20135 Nisan 2013, Ankara ODT\u00dc K\u00fclt\u00fcr ve Kongre Merkezi, Bildiri \u00d6zleri Kitab\u0131, 28-29.<\/p>\n

-Emre, \u00d6., Duman, T. Y., \u00d6zalp, S., Do\u011fan, A ., 2012. Simav Fay\u0131 ve 19 May\u0131s 2011 Simav Depremi (Mw: 5.8). 65. T\u00fcrkiye Jeoloji Kurultay\u0131, 2-6 Nisan 2012, MTA Genel M\u00fcd\u00fcrl\u00fcg \u02d8\u00fc K\u00fclt\u00fcr Sitesi, Bildiri Ozleri Kitab\u0131, pp 10\u201311, Ankara<\/p>\n

-Emre, \u00d6., Duman, T.Y., \u00d6zalp, S., \u015earo\u011flu, F., Olgun, \u015e., Elmac\u0131, H. & \u00c7an, T., 2018. Active fault database of Turkey. Bull Earthq Bull Earthquake Eng. DOI 10.1007\/s10518-016-0041-2<\/p>\n

-Eyido\u011fan, H. & Jackson, J., 1985.\u00a0 A seismological study of normal faulting in the Demirci, Ala\u015fehir and Gediz earthquakes of 1969\u201370 in western Turkey: Implications for the nature and geometry of deformation in the continental crust, Geophysical Journal International, v81, Issue 3, 569-607.<\/p>\n

-Eyido\u011fan, H., 2020. Manisa Akhisar Civar\u0131ndaki Deprem Aktivitesi ile Gutenberg-Richter Parametrelerinin Zamansal ve Mek\u00e2nsal \u00d6zelliklerinin \u0130ncelenmesi, T\u00fcrk Deprem Ara\u015ft\u0131rma Dergisi, Cilt 2, Say\u0131: 2, 139-159. https:\/\/dergipark.org.tr\/en\/pub\/tdad\/article\/776186<\/p>\n

-Kartal, R. F. ve Kadi\u0307ri\u0307og\u0306lu, F. T., 2015. 2011-2012 Simav Depremleri (Ml=5.7, Ml=5.0, Ml=5.4) ve Bo\u0308lgenin Tektonik Yap\u0131s\u0131 ile I\u0307lis\u0327kisi, Yerbilimleri, 35 (3), 185-198.<\/p>\n

-Konak, N., 2012. Simav Dolay\u0131n\u0131n Jeolojisi ve Metaforf Kaya\u00e7lar\u0131n\u0131n Evrimi. \u0130stanbul Yerbilimleri Dergisi. 2012;3(1-2).<\/p>\n

-\u00d6zalp, S., Emre, O., Duman, T.Y., \u015earo\u011flu, F., Ozaksoy, V., Elmac\u0131, , Ko\u00e7, G., 2009. \u00c7ivril Graben system: morphotectonic structure and active fault characteristics, SW Turkey. 62nd Geological Congress of Turkey, 13\u201317 April 2009, Abstracts Book-II, pp 794\u2013795, Ankara, Turkey.<\/p>\n

-\u015eeng\u00f6r, C., 1987. Cross faults and differential stretching of hanging wall in regions of low-angle normal faulting: examples from western Turkey. In: Coward MP, Dewey JF, Hancock P (eds) Continental extensional tectonics, Geol Soc London, Special Publication 28:575\u2013589.<\/p>\n

-USGS, 2025. https:\/\/www.usgs.gov\/news\/what-earthquake-swarm<\/p>\n

S\u00f6zl\u00fck
\n<\/strong>Graben:<\/strong> Jeolojide\u00a0graben<\/strong>, yer kabu\u011funun iki fay aras\u0131ndaki al\u00e7alm\u0131\u015f ve derinle\u015fmi\u015f b\u00f6l\u00fcm\u00fcd\u00fcr. Genellikle tektonik hareketler sonucu olu\u015fur ve yery\u00fcz\u00fcnde \u00e7\u00f6k\u00fcnt\u00fc sonucu olu\u015fan bozukluklar olarak tan\u0131mlan\u0131r. Bu yap\u0131, genellikle \u00e7atlak veya fay sistemleri boyunca olu\u015fur ve \u00e7evresine g\u00f6re al\u00e7ak alanlar olu\u015fturur. Faylar boyunca \u00e7\u00f6k\u00fcnt\u00fc alanlar\u0131 g\u00f6ller de olu\u015fturur (\u00f6rn. Burdur G\u00f6l\u00fc, \u0130znik G\u00f6l\u00fc, Sivrice G\u00f6l\u00fc vb). Grabenler, volkanik ve sedimanter s\u00fcre\u00e7lerle de ili\u015fkilidir ve b\u00f6lgesel jeolojik faaliyetlerin g\u00f6stergesidir.<\/p>\n

Jeotektonik:<\/strong> Jeotektonik, k\u0131talar\u0131n olu\u015fumu, birle\u015fimi, par\u00e7alanmas\u0131, yitim ve da\u011f olu\u015fumu gibi yerk\u00fcrenin dinamik s\u00fcre\u00e7lerini inceleyen bir bilim dal\u0131d\u0131r. Bat\u0131 Anadolu’nun Ege adalar\u0131 ve Yunanistan ile jeotektonik a\u00e7\u0131dan benzer bir evrim ge\u00e7irdi\u011fi belirtilmektedir. Jeolojik, petrografik ve jeofizik veriler bu evrimi desteklemektedir. Do\u011fu Pontid b\u00f6lgesindeki jeotektonik \u00e7al\u0131\u015fmalar da bu alana \u00f6rnektir.<\/p>\n

Sismoloji (Deprembilim):<\/strong> Sismoloji, Yunanca ‘seismos’ (deprem) ve ‘logos’ (bilim) kelimelerinden t\u00fcremi\u015f olup, yer hareketlerini ve depremleri inceleyen jeofizik dal\u0131d\u0131r. Depremlerin olu\u015fum nedenlerini, yay\u0131lma bi\u00e7imlerini, etkilerini ve bunlar\u0131n \u00f6l\u00e7\u00fclmesini ara\u015ft\u0131r\u0131r. Sismoloji ayn\u0131 zamanda deprem haritalar\u0131 olu\u015fturulmas\u0131, deprem risklerinin belirlenmesi ve deprem tahmin \u00e7al\u0131\u015fmalar\u0131 gibi alanlarda da faaliyet g\u00f6sterir.<\/p>\n

Normal fay:<\/strong> Normal faylar, fay d\u00fczlemi boyunca tavan blo\u011funun a\u015fa\u011f\u0131ya do\u011fru hareket etti\u011fi fay t\u00fcrleridir. Bu hareket, genellikle fay\u0131n iki taraf\u0131ndaki bloklar\u0131n birbirinden uzakla\u015fmas\u0131yla sonu\u00e7lan\u0131r. Bu t\u00fcr faylanmalar genellikle geni\u015fleme rejimlerinde, \u00f6rne\u011fin rift vadileri ve okyanus ortas\u0131 yay\u0131lma merkezleri gibi yerlerde g\u00f6r\u00fcl\u00fcr.<\/p>\n

Do\u011frultu at\u0131ml\u0131 fay:<\/strong> Do\u011frultu at\u0131ml\u0131 faylar, fay d\u00fczlemi boyunca bloklar\u0131n yatay olarak kayd\u0131\u011f\u0131 fay t\u00fcrleridir. Bu faylar, kayma y\u00f6n\u00fcne g\u00f6re sa\u011f veya sol y\u00f6nl\u00fc olarak s\u0131n\u0131fland\u0131r\u0131l\u0131r. Sa\u011f y\u00f6nl\u00fc fayda kar\u015f\u0131dan bak\u0131ld\u0131\u011f\u0131nda uzak blok sa\u011fa, sol y\u00f6nl\u00fc fayda ise sola do\u011fru hareket eder.<\/p>\n","protected":false},"excerpt":{"rendered":"

Prof. Dr. Haluk Eyido\u011fan 22 Nisan 2025 tarihinde bas\u0131na yans\u0131yan deprem haberlerinden birinin ba\u015fl\u0131\u011f\u0131 \u015f\u00f6yleydi; \u201cK\u00fctahya\u2019da yeni fay hatt\u0131 ortaya \u00e7\u0131kt\u0131\u201d (Cumhuriyet Gazetesi, 22 May\u0131s 2025). K\u00fctahya Dumlup\u0131nar \u00dcniversitesi\u2019den Jeoloji Y\u00fcksek M\u00fchendisi Prof. Dr. Cafer \u00d6zkul, “K\u00fc\u00e7\u00fck \u00f6l\u00e7ekteki bu depremler, daha \u00f6nce tespit edilmemi\u015f ve haritalanmam\u0131\u015f bir yerde ger\u00e7ekle\u015fti” yorumunu yapm\u0131\u015ft\u0131 Habere konu olan deprem […]<\/p>\n","protected":false},"author":1575,"featured_media":65003,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[19],"tags":[10138,7285,10139,10140],"class_list":["post-64997","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-bilim-gundemi","tag-kutahya","tag-prof-dr-haluk-eyidogan","tag-simav-deprem","tag-turkiye-deprem-gercegi"],"acf":[],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/bilimvegelecek.com.tr\/index.php\/wp-json\/wp\/v2\/posts\/64997","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/bilimvegelecek.com.tr\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/bilimvegelecek.com.tr\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/bilimvegelecek.com.tr\/index.php\/wp-json\/wp\/v2\/users\/1575"}],"replies":[{"embeddable":true,"href":"https:\/\/bilimvegelecek.com.tr\/index.php\/wp-json\/wp\/v2\/comments?post=64997"}],"version-history":[{"count":0,"href":"https:\/\/bilimvegelecek.com.tr\/index.php\/wp-json\/wp\/v2\/posts\/64997\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/bilimvegelecek.com.tr\/index.php\/wp-json\/wp\/v2\/media\/65003"}],"wp:attachment":[{"href":"https:\/\/bilimvegelecek.com.tr\/index.php\/wp-json\/wp\/v2\/media?parent=64997"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/bilimvegelecek.com.tr\/index.php\/wp-json\/wp\/v2\/categories?post=64997"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/bilimvegelecek.com.tr\/index.php\/wp-json\/wp\/v2\/tags?post=64997"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}