{"id":171478,"date":"2026-01-28T12:42:12","date_gmt":"2026-01-28T12:42:12","guid":{"rendered":"https:\/\/kamucalisani.net\/?p=171478"},"modified":"2026-01-28T12:42:12","modified_gmt":"2026-01-28T12:42:12","slug":"3-8lik-deprem-sonrasi-uzmandan-carpici-aciklama-risk-sanildigindan-buyuk","status":"publish","type":"post","link":"https:\/\/kamucalisani.net\/index.php\/2026\/01\/28\/3-8lik-deprem-sonrasi-uzmandan-carpici-aciklama-risk-sanildigindan-buyuk\/","title":{"rendered":"3.8\u2019lik deprem sonras\u0131 uzmandan \u00e7arp\u0131c\u0131 a\u00e7\u0131klama: Risk san\u0131ld\u0131\u011f\u0131ndan b\u00fcy\u00fck"},"content":{"rendered":"

Afet ve Acil Durum Y\u00f6netimi Ba\u015fkanl\u0131\u011f\u0131 (AFAD) verilerine g\u00f6re, d\u00fcn saat 23.15\u2019te Trabzon\u2019un Karadeniz a\u00e7\u0131klar\u0131nda 3.8 b\u00fcy\u00fckl\u00fc\u011f\u00fcnde deprem oldu. Yerin 28 kilometre derinli\u011finde meydana gelen deprem, k\u0131sa s\u00fcreli tedirginli\u011fe neden oldu. \u00c7evre illerden de hissedilen depremde ilk belirlemelere g\u00f6re herhangi bir olumsuzluk ya\u015fanmad\u0131\u011f\u0131 bildirildi. KT\u00dc Jeofizik M\u00fchendisli\u011fi B\u00f6l\u00fcm Ba\u015fkan\u0131 Prof. Dr. Nilg\u00fcn Say\u0131l, 3.8 b\u00fcy\u00fckl\u00fc\u011f\u00fcndeki depreme ili\u015fkin, de\u011ferlendirme ve uyar\u0131larda bulundu.<\/p>\n

Karadeniz ve \u00e7evresinin, d\u00fc\u015f\u00fck depremselli\u011fe sahip bir b\u00f6lge olarak tan\u0131mlanmakta oldu\u011funu belirten Say\u0131l, \u201cB\u00f6lge depremleri, s\u0131\u011f odakl\u0131 olup kabuksald\u0131r. S\u0131k\u0131\u015fma tektoni\u011finin belirgin oldu\u011fu kuzeydo\u011fu k\u0131y\u0131lar\u0131nda, bindirme mekanizmas\u0131na sahip depremler olu\u015fmaktad\u0131r. Karadeniz B\u00f6lgesi, \u00e7ok kompleks tektonik birimleri i\u00e7inde bar\u0131nd\u0131rmaktad\u0131r. \u00d6zellikle Kafkaslar, \u00f6nemli s\u0131k\u0131\u015fma b\u00f6lgesidir ve b\u00f6lgede b\u00fcy\u00fck \u00f6l\u00e7ekte transform faylar, s\u0131k\u0131\u015fma tektoni\u011fi ve buna ba\u011fl\u0131 bindirme t\u00fcr\u00fc faylar etkili olmaktad\u0131r. Karadeniz\u2019in k\u0131y\u0131 kesimlerini ve dolay\u0131s\u0131yla \u015fehrimizi etkileyen do\u011fudan bat\u0131ya do\u011fru uzanan Kuzey Anadolu Fay Zonu (KAFZ) ve kuzeyden de sahile paralel uzanan Karadeniz Fay\u0131 s\u0131ralanmaktad\u0131r. G\u00fcneyde bulunan KAFZ \u00e7ok aktif, Karadeniz Fay\u0131 ise yava\u015f hareket eden bir fayd\u0131r. Magnit\u00fcd\u00fc 7.0\u2019nin \u00fczerinde deprem \u00fcretme potansiyeli olan KAFZ\u2019\u0131n, ilimize en yak\u0131n mesafesi 100-150 kilometredir. Bu fay \u00fczerinde, bu b\u00fcy\u00fckl\u00fckteki depremler meydana geldi\u011finde Trabzon ve \u00e7evresi, \u00f6zellikle sahil kesimi gibi zay\u0131f (gev\u015fek) zemin \u00f6zelli\u011findeki yerler de bu depremleri, olduk\u00e7a \u015fiddetli bir \u015fekilde hissedecektir\u201d dedi.<\/p>\n

\n
<\/img><\/div>\n<\/div>\n

M\u0130KROB\u00d6LGELEME \u00c7ALI\u015eMA YAPILMASI \u00d6NER\u0130S\u0130<\/strong><\/p>\n

Deniz dolgu alanlar\u0131na dikkati \u00e7eken Prof. Dr. Say\u0131l, \u201cKaradeniz B\u00f6lgesi\u2019nde Meydana Gelen Aletsel D\u00f6nem Deprem Aktivitesi\u2019ne bak\u0131ld\u0131\u011f\u0131nda; 3 Eyl\u00fcl 1968 tarihli Bart\u0131n Depremi (6.5 b\u00fcy\u00fckl\u00fc\u011f\u00fcnde) ve 23 Aral\u0131k 2012 tarihinde Karadeniz (G\u00fcrcistan) a\u00e7\u0131klar\u0131nda meydana gelen 5.8 b\u00fcy\u00fckl\u00fc\u011f\u00fcndeki deprem; b\u00f6lgenin pasif olmad\u0131\u011f\u0131n\u0131, \u00e7ok s\u0131k olmasa da deprem \u00fcretti\u011fini ve son ya\u015fanan k\u00fc\u00e7\u00fck depremler de aktivitenin s\u00fcrece\u011fini g\u00f6stermektedir. T\u00fcrkiye’nin \u2018Yeni Deprem Tehlike Haritas\u0131\u2019n\u0131n olu\u015fturulmas\u0131nda kullan\u0131lan jeofizik parametrelerden olan yer \u00e7ekimi ivmesi hesaplamalar\u0131na g\u00f6re, Trabzon\u2019da beklenen en b\u00fcy\u00fck yer ivme de\u011ferleri ortalama 0.2g civar\u0131ndad\u0131r. Bu ivme de\u011ferleri ilimizin \u2018D\u00fc\u015f\u00fck Tehlike\u2019 kategorisinde oldu\u011funu g\u00f6stermektedir. Ancak yer ivmesi de\u011feri, gev\u015fek zeminlerde ve dolgu alanlarda \u00e7ok daha fazla b\u00fcy\u00fcyecek ve depremin daha \u015fiddetli hissedilmesine neden olabilecektir. \u0130limizde son y\u0131llarda, deniz dolgu alanlar\u0131nda ve al\u00fcvyonal arazilerde yap\u0131la\u015fman\u0131n \u00e7o\u011falmas\u0131, riskleri daha da art\u0131rmaktad\u0131r. Bu sebeple \u00f6zellikle Trabzon\u2019un sahil kesimde bulunan dolgu ve al\u00fcvyon alanlar\u0131n, deprem b\u00fcy\u00fctmesine neden olabilecekleri dikkate al\u0131narak yap\u0131 stoklar\u0131n\u0131n g\u00fcvenliklerinin sorgulanmas\u0131 gerekmektedir. Yerel y\u00f6netimler taraf\u0131ndan mikrob\u00f6lgeleme \u00e7al\u0131\u015fmalar\u0131 yap\u0131larak depremde riskli alanlar\u0131n ve riskli binalar\u0131n belirlenmesi, bu kapsamda kentsel d\u00f6n\u00fc\u015f\u00fcm ve g\u00fc\u00e7lendirme i\u015flemleri uygulanarak yap\u0131lar\u0131n, depreme kar\u015f\u0131 g\u00fcvenli hale getirilmesi sa\u011flanmal\u0131d\u0131r\u201d ifadelerini kulland\u0131.<\/p>\n\n

<\/p>\n

Kaynak :\u00a0http:\/\/www.milliyet.com.tr\/gundem\/3-8lik-deprem-sonrasi-uzmandan-carpici-aciklama-risk-sanildigindan-buyuk-7528749<\/span><\/p>\n","protected":false},"excerpt":{"rendered":"

Karadeniz Teknik \u00dcniversitesi (KT\u00dc) Jeofizik M\u00fchendisli\u011fi B\u00f6l\u00fcm Ba\u015fkan\u0131 Prof. Dr. Nilg\u00fcn Say\u0131l, Trabzon\u2019da Karadeniz a\u00e7\u0131klar\u0131nda d\u00fcn meydana gelen 3.8 b\u00fcy\u00fckl\u00fc\u011f\u00fcndeki depreme ili\u015fkin kritik a\u00e7\u0131klamalarda bulundu.<\/p>\n","protected":false},"author":1,"featured_media":171479,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[3],"tags":[1087,583,2413,1055,524],"class_list":["post-171478","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-guncel","tag-bolge","tag-deprem","tag-fay","tag-karadeniz","tag-yapi"],"_links":{"self":[{"href":"https:\/\/kamucalisani.net\/index.php\/wp-json\/wp\/v2\/posts\/171478","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/kamucalisani.net\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/kamucalisani.net\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/kamucalisani.net\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/kamucalisani.net\/index.php\/wp-json\/wp\/v2\/comments?post=171478"}],"version-history":[{"count":1,"href":"https:\/\/kamucalisani.net\/index.php\/wp-json\/wp\/v2\/posts\/171478\/revisions"}],"predecessor-version":[{"id":171481,"href":"https:\/\/kamucalisani.net\/index.php\/wp-json\/wp\/v2\/posts\/171478\/revisions\/171481"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/kamucalisani.net\/index.php\/wp-json\/wp\/v2\/media\/171479"}],"wp:attachment":[{"href":"https:\/\/kamucalisani.net\/index.php\/wp-json\/wp\/v2\/media?parent=171478"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/kamucalisani.net\/index.php\/wp-json\/wp\/v2\/categories?post=171478"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/kamucalisani.net\/index.php\/wp-json\/wp\/v2\/tags?post=171478"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}