Son d\u00f6nemde art\u0131\u015f g\u00f6steren deprem sars\u0131nt\u0131lar\u0131 devam ederken, 2023 y\u0131l\u0131nda K\u0131br\u0131s i\u00e7in deprem ara\u015ft\u0131rmas\u0131 yapan T\u00fcrkiye\u2019deki Maden Tetkik ve Arama Genel M\u00fcd\u00fcrl\u00fc\u011f\u00fc (MTA) \u00e7al\u0131\u015fmalar\u0131n\u0131 s\u00fcrd\u00fcr\u00fcyor. MTA Genel M\u00fcd\u00fcrl\u00fc\u011f\u00fc Jeoloji Et\u00fctleri Dairesi Ba\u015fkan\u0131 Do\u00e7. Dr. Selim \u00d6zalp ve MTA Genel M\u00fcd\u00fcrl\u00fc\u011f\u00fc Jeoloji Et\u00fctleri Dairesi Ba\u015fkanl\u0131\u011f\u0131 T\u00fcrkiye Paleosismoloji Ara\u015ft\u0131rmalar\u0131 Projesi Ba\u015fkan\u0131 ve Jeoloji Y\u00fcksek M\u00fchendisi Hasan Elmac\u0131, \u00e7al\u0131\u015fmalar hakk\u0131nda YEN\u0130D\u00dcZEN\u2019e bilgiler verdi, K\u0131br\u0131s\u2019\u0131n do\u011fu, kuzey ve bat\u0131 sahilleri boyunca s\u0131v\u0131la\u015fma potansiyeli bulundu\u011funu belirtti.<\/p>\n\n\n\n
\u201cKKTC\u2019de yer alan G\u00fczelyurt ve Gazima\u011fusa k\u00f6rfezlerinin Tsunami y\u00f6n\u00fcnden ara\u015ft\u0131r\u0131lmas\u0131 gerekmektedir\u201d de\u011ferlendirmesini yapan MTA Genel M\u00fcd\u00fcrl\u00fc\u011f\u00fc yetkilileri, KKTC genelini kapsayacak \u015fekilde Deprem Tehlike Haritalar\u0131\u2019n\u0131n olu\u015fturulmas\u0131n\u0131n da elzem oldu\u011funu ifade etti.<\/p>\n\n\n\n
Mesarya Havzas\u0131\u2019n\u0131n, gen\u00e7 \u00e7\u00f6kellerle oldu\u011funu kaydeden Do\u00e7 Dr. \u00d6zalp ve Jeoloji Y\u00fcksek M\u00fchendisi Elmac\u0131, \u201cKKTC deprem ve depremle tetiklenen s\u0131v\u0131la\u015fma, tsunami gibi jeodinamik s\u00fcre\u00e7lerin etkisi alt\u0131nda kalabilme potansiyeline sahiptir. Bu s\u00fcre\u00e7lerin her biri ada i\u00e7in ciddi risklere neden olabilecek jeolojik tehlike kaynaklar\u0131d\u0131r\u201d de\u011ferlendirmesini yapt\u0131.<\/p>\n\n\n\n
\u00c7al\u0131\u015fmalar hakk\u0131nda da bilgiler veren MTA Genel M\u00fcd\u00fcrl\u00fc\u011f\u00fc yetkilileri, Hendeklerde saptanan eski depremlerin tarihini belirlemek i\u00e7in \u00f6rnekler al\u0131nd\u0131\u011f\u0131n\u0131 belirterek, \u201ca\u00e7\u0131lan hendeklerde belirlenen eski depremlere ili\u015fkin yorumlamalar ise hendeklerden derlenen tarihlendirme \u00f6rneklerinin analiz sonu\u00e7lar\u0131 ile birlikte de\u011ferlendirilmekte ve raporun haz\u0131rlanmas\u0131na devam ediliyor\u201d \u015feklinde g\u00f6r\u00fc\u015f bildirdi. Son d\u00f6nemde ya\u015fanan sars\u0131nt\u0131lar\u0131 da de\u011ferlendiren yetkililer, bu depremlerin sars\u0131nt\u0131 d\u0131\u015f\u0131nda K\u0131br\u0131s\u2019a do\u011frudan bir etkisi olmad\u0131\u011f\u0131n\u0131 dile getirdi.<\/p>\n\n\n\n
\u201cHendeklerde saptanan eski depremlerin tarihini belirlemek i\u00e7in \u00f6rnekler al\u0131nd\u0131\u201d<\/strong><\/h2>\n\n\n\n
Soru: K\u0131br\u0131s ile ilgili deprem \u00e7al\u0131\u015fmalar\u0131nda nas\u0131l bir a\u015famaya gelindi? K\u0131br\u0131s bu konuda tehlikeli bir noktada m\u0131?<\/strong><\/p>\n\n\n\n
\u201cKKTC\u2019nin karadaki deprem kayna\u011f\u0131 olarak tan\u0131mlanabilecek Dardere (Ovgos) ve Koru\u00e7am Fay Zonlar\u0131 i\u00e7erisinde yer alan diri faylar\u0131n niteli\u011fini ve ge\u00e7mi\u015fte olu\u015fturdu\u011fu deprem veya depremleri ortaya koyabilmek i\u00e7in se\u00e7ilen alanlarda hendekli paleosismoloji \u00e7al\u0131\u015fmalar\u0131 yap\u0131ld\u0131. Aktif Faylar \u00fczerindeki depremlerin ara\u015ft\u0131r\u0131ld\u0131\u011f\u0131 Paleosismoloji \u00e7al\u0131\u015fmalar\u0131, KKTC ana karas\u0131nda haritalanm\u0131\u015f t\u00fcm faylar \u00fczerinde ger\u00e7ekle\u015ftirilen hava foto\u011fraf\u0131 analizleri ve jeolojik g\u00f6zlemler \u0131\u015f\u0131\u011f\u0131nda se\u00e7ilen alanlarda, yakla\u015f\u0131k 20-30 metre uzunlu\u011funda, ortalama 5 metre geni\u015fli\u011finde ve en derin yeri 4 metre olacak \u015fekilde kaz\u0131lan hendekler ile ger\u00e7ekle\u015ftirildi. Hendeklerde saptanan eski depremlerin tarihini belirlemek i\u00e7in \u00f6rnekler al\u0131nd\u0131. \u00d6rneklere ili\u015fkin sonu\u00e7lar ilgili laboratuvarlardan geldi, de\u011ferlendirilme \u00e7al\u0131\u015fmalar\u0131 ve rapor yaz\u0131m\u0131 devam ediyor\u201d<\/p>\n\n\n\n
\u201cKKTC Diri Fay Haritas\u0131 revize edilerek, bu faylar\u0131n deprem tarih\u00e7eleri ortaya konuldu\u201d<\/strong><\/h2>\n\n\n\n
Soru: Paleosismoloji Raporu nedir? Bu rapor ne zaman tamamlanacak?<\/strong><\/p>\n\n\n\n
\u201cKuvaterner (son 2,5 milyon y\u0131ll\u0131k zaman dilimi) d\u00f6nemi s\u00fcresince en az bir kez y\u00fczey k\u0131r\u0131\u011f\u0131 olu\u015fturacak \u015fekilde deprem \u00fcretmi\u015f faylara Aktif Fay ad\u0131 veriliyor. Paleosismoloji ise jeolojik ve jeomorfolojik verilerden yararlanarak diri faylar \u00fczerinde y\u00fczey k\u0131r\u0131\u011f\u0131 olu\u015fturmu\u015f eski depremlerin yeri, b\u00fcy\u00fckl\u00fc\u011f\u00fc ve zaman\u0131 hakk\u0131nda veri \u00fcretmeyi hedefleyen bir bilim dal\u0131d\u0131r. KKTC\u2019de 2023 y\u0131l\u0131n\u0131n Ekim-Aral\u0131k aylar\u0131 aras\u0131nda MTA Genel M\u00fcd\u00fcrl\u00fc\u011f\u00fc taraf\u0131ndan y\u00fcr\u00fct\u00fclen proje ile hem kentsel hem de sanayi-maden alanlar\u0131 i\u00e7in arazi planlamas\u0131na ihtiya\u00e7 duyulmas\u0131 nedeniyle KKTC\u2019de yap\u0131lacak olan b\u00f6lgesel planlamalar\u0131 y\u00f6nlendirici temel yerbilim verilerinin haz\u0131rlanmas\u0131 hedeflendi. S\u00f6z konusu ihtiyac\u0131 kar\u015f\u0131lamak \u00fczere KKTC\u2019de gen\u00e7 tektonik yap\u0131lar\u0131n karakteristiklerinin belirlenmesi, alansal da\u011f\u0131l\u0131mlar\u0131n\u0131n ortaya konulmas\u0131, kinematik analizlerinin yap\u0131lmas\u0131, \u00f6zellikle deprem tehlikesi i\u00e7in \u00f6nemli olan neotektonik d\u00f6nem yap\u0131lar\u0131n\u0131n T\u00fcrkiye’de yap\u0131lan \u00e7al\u0131\u015fmalardaki standartlar kapsam\u0131nda haritalanarak, paleosismolojik kaz\u0131 \u00e7al\u0131\u015fmalar\u0131 detayland\u0131r\u0131lm\u0131\u015ft\u0131r. Bu kapsamda KKTC Diri Fay Haritas\u0131 revize edilerek, bu faylar\u0131n deprem tarih\u00e7eleri ortaya konmu\u015ftur. A\u00e7\u0131lan hendeklerde belirlenen eski depremlere ili\u015fkin yorumlamalar ise hendeklerden derlenen tarihlendirme \u00f6rneklerinin analiz sonu\u00e7lar\u0131 ile birlikte de\u011ferlendirilmekte ve raporun haz\u0131rlanmas\u0131na devam ediliyor.\u201d<\/p>\n\n\n\n<\/figure>\n\n\n\n
\u201cDepremlerin K\u0131br\u0131s\u2019a sars\u0131nt\u0131 d\u0131\u015f\u0131nda do\u011frudan bir etkisi yok\u201d<\/strong><\/h2>\n\n\n\n
Soru: Ge\u00e7ti\u011fimiz Cuma ak\u015fam\u0131 Antalya\u2019da ger\u00e7ekle\u015fen depremin adaya etkisi ne oldu?<\/strong><\/p>\n\n\n\n
\u201cK\u0131br\u0131s Adas\u0131, d\u00fcnyadaki en \u00f6nemli iki deprem ku\u015fa\u011f\u0131ndan birisi olan Alp-Himalaya Deprem Ku\u015fa\u011f\u0131 \u00fczerinde yer al\u0131yor. 29.11.2024 tarihinde 22:13\u2019te Gazipa\u015fa (Antalya) a\u00e7\u0131klar\u0131nda meydana gelen 4,8 b\u00fcy\u00fckl\u00fc\u011f\u00fcndeki deprem, Alp-Himalaya Deprem Ku\u015fa\u011f\u0131 \u00fczerindeki \u00f6nemli deprem kaynaklar\u0131ndan birisi olan K\u0131br\u0131s Yay\u0131\u2019n\u0131n veya Dardere (Ovgos) Fay Zonu\u2019nun denizdeki devam\u0131 \u00fczerinde olu\u015ftu\u011fu yorumlanmaktad\u0131r. Antalya K\u00f6rfezi\u2019nde meydana gelen bu ve benzeri depremlerin sars\u0131nt\u0131 d\u0131\u015f\u0131nda KKTC\u2019ye do\u011frudan bir etkisi olmamakla birlikte, bu faylardan kaynakl\u0131 deprem tehlikesinin oldu\u011funu g\u00f6stermektedir. Ayr\u0131ca b\u00f6lgedeki sismik aktivitenin devam etti\u011fini g\u00f6stermesi bak\u0131m\u0131ndan da \u00f6nemlidir.\u201d<\/p>\n\n\n\n
\u201cDardere (Ovgos) Fay\u0131 y\u0131k\u0131c\u0131 etkisi y\u00fcksek olabilecek en \u00f6nemli diri fay\u2026\u201d<\/strong><\/h2>\n\n\n\n
\u201cDardere (Ovgos) Fay Zonu, KKTC ana karas\u0131 i\u00e7inde haritalanm\u0131\u015f ve y\u0131k\u0131c\u0131 etkisi y\u00fcksek olabilecek en \u00f6nemli diri fayd\u0131r. Gerek MTA ve gerekse di\u011fer bilim insanlar\u0131 taraf\u0131ndan yap\u0131lan \u00e7al\u0131\u015fmalarda bu zona ait olan en \u00f6nemli bulgu, her biri farkl\u0131 derecede deformasyon ge\u00e7irmi\u015f farkl\u0131 kaya birimlerinin Dardere (Ovgos) Fay Zonu taraf\u0131ndan yan yana getirilmi\u015f olmas\u0131d\u0131r. Fay zonu \u00fczerinde ger\u00e7ekle\u015ftirilen paleosismoloji \u00e7al\u0131\u015fmalar\u0131na g\u00f6re Kuvaterner akitvitesi belgelenmi\u015ftir. Bu nedenle diri fay olarak de\u011ferlendirilmektedir.\u201d<\/p>\n\n\n\n<\/figure>\n\n\n\n
\u201cKKTC, deprem, s\u0131v\u0131la\u015fma, tsunami gibi jeodinamik s\u00fcre\u00e7lerin etkisi alt\u0131nda kalabilme potansiyeline sahiptir\u201d<\/strong><\/h2>\n\n\n\n
\u201cK\u0131br\u0131s Adas\u0131 Afrika-Anadolu levhalar\u0131 aras\u0131nda y\u00fcksek deprem aktivitesine sahip dalma-batma zonu i\u00e7inde bulunmas\u0131, hem Dardere (Ovgos) Fay Zonunun geli\u015fmesine ve hem de do\u011fu-bat\u0131 uzan\u0131ml\u0131 di\u011fer faylara ko\u015fut uzanan gen\u00e7 s\u0131rada\u011flar\u0131n kuzey ve g\u00fcney yama\u00e7lar\u0131n\u0131n y\u00fcksek e\u011fimli olmas\u0131na neden olmu\u015ftur. Da\u011fl\u0131k alanlar d\u0131\u015f\u0131nda kalan Mesarya Havzas\u0131, Kuvaterner\u2019de olu\u015fmu\u015f gen\u00e7 \u00e7\u00f6kellerle kapl\u0131d\u0131r. Dolay\u0131s\u0131yla, KKTC deprem ve depremle tetiklenen s\u0131v\u0131la\u015fma, tsunami gibi jeodinamik s\u00fcre\u00e7lerin etkisi alt\u0131nda kalabilme potansiyeline sahiptir. Bu s\u00fcre\u00e7lerin her biri Ada i\u00e7in ciddi risklere neden olabilecek jeolojik tehlike kaynaklar\u0131d\u0131r.\u201d<\/p>\n\n\n\n<\/figure>\n\n\n\n
\u201cDo\u011fu, kuzey ve bat\u0131 sahilleri s\u0131v\u0131la\u015fma potansiyeline sahiptir\u201d<\/strong><\/h2>\n\n\n\n
Soru: Kuzey K\u0131br\u0131s\u2019ta Gazima\u011fusa ve Karpaz\u2019a kadar olan do\u011fu g\u00fcneydo\u011fu sahillerinde ve G\u00fczelyurt Ovas\u0131\u2019n\u0131n sahil kesimlerinin s\u0131v\u0131la\u015fmaya e\u011fimli alanlar oldu\u011fu s\u00f6yleniyor. Bu tespit hakk\u0131nda neler s\u00f6ylenilebilir, ger\u00e7ekten b\u00f6yle bir \u015fey var m\u0131?<\/strong><\/p>\n\n\n\n
\u201cS\u0131v\u0131la\u015fma, deprem s\u0131ras\u0131nda yerin yo\u011fun bir \u015fekilde sars\u0131lmas\u0131 sonucu topra\u011f\u0131n dayan\u0131kl\u0131l\u0131\u011f\u0131n\u0131 kaybederek kat\u0131dan \u00e7ok s\u0131v\u0131 gibi davranmaya ba\u015flamas\u0131d\u0131r. Bu olay, binalar\u0131n alt\u0131nda ger\u00e7ekle\u015fti\u011finde, zemin yap\u0131lar\u0131n temelini destekleme \u00f6zelli\u011fini yitirir. Sonu\u00e7 olarak, binalar ve di\u011fer yap\u0131lar devrilebilir, kayabilir veya yan yatabilir. 2014-2016 y\u0131llar\u0131 aras\u0131nda MTA Genel M\u00fcd\u00fcrl\u00fc\u011f\u00fc taraf\u0131ndan y\u00fcr\u00fct\u00fclen bir proje kapsam\u0131nda KKTC s\u0131n\u0131rlar\u0131 i\u00e7erisinde kalan alan\u0131n Kuvaterner Jeolojisi Haritas\u0131 haz\u0131rlanm\u0131\u015f ve bu haritadan yararlan\u0131larak literat\u00fcrde kabul g\u00f6ren ve yayg\u0131n olarak kullan\u0131lan y\u00f6ntemlere g\u00f6re b\u00f6lgesel s\u0131v\u0131la\u015fma yatk\u0131nl\u0131k haritalar\u0131 olu\u015fturulmu\u015ftur. Bu haritaya g\u00f6re Kuvaterner d\u00f6neminde Mesarya havzas\u0131 ve etraf\u0131nda al\u00fcvyon yelpazesi \u00e7\u00f6kelleri, d\u00f6k\u00fcnt\u00fc-etek \u00e7\u00f6kelleri ve akarsu ortam\u0131 \u00e7\u00f6kelleri geli\u015fmi\u015ftir. Buna g\u00f6re KKTC\u2019nin do\u011fu, kuzey ve bat\u0131 sahilleri boyunca kumul ve plaj \u00e7\u00f6kelleri yayg\u0131n olarak izlenmektedir ve bu alanlar\u0131n s\u0131v\u0131la\u015fma potansiyeli bulunmaktad\u0131r.\u201d<\/p>\n\n\n\n<\/figure>\n\n\n\n
Soru: Depremle ilgili nas\u0131l \u00e7al\u0131\u015fmalar yap\u0131lmal\u0131, \u00f6nerileriniz nelerdir?<\/strong><\/p>\n\n\n\n
\u201cMTA taraf\u0131ndan ger\u00e7ekle\u015ftirilen jeolojik tehlikelere y\u00f6nelik y\u00fcr\u00fct\u00fclen projeler sonras\u0131nda, \u00f6zellikle diri faylar\u0131n ge\u00e7ti\u011fi alanlarda, heyelan, tsunami ve s\u0131v\u0131la\u015fmaya yatk\u0131n kesimlere y\u00f6nelik planlama yap\u0131labilmesi i\u00e7in b\u00fcy\u00fck \u00f6l\u00e7ekli (1:1.000, 1:5.000, 1:10.000) \u00e7al\u0131\u015fmalar\u0131n yap\u0131lmas\u0131 \u00f6nemlidir. Ayr\u0131ca KKTC\u2019de yer alan G\u00fczelyurt ve Gazimagusa k\u00f6rfezlerinin Tsunami y\u00f6n\u00fcnden ara\u015ft\u0131r\u0131lmas\u0131 gerekmektedir. KKTC genelini kapsayacak \u015fekilde Deprem Tehlike Haritalar\u0131\u2019n\u0131n olu\u015fturulmas\u0131 elzemdir. Bu haritalar\u0131n olu\u015fturulabilmesi i\u00e7in gereken altl\u0131k veriler; Temel Jeolojik veri, Diri Fay Haritas\u0131, Kuvaterner Jeolojisi Haritas\u0131, S\u0131v\u0131la\u015fma Yatk\u0131nl\u0131k Haritalar\u0131, Paleosismolojik veri, Tsunami Ara\u015ft\u0131rmlar\u0131 ve Kabuk kal\u0131nl\u0131\u011f\u0131 gibi verilere ihtiya\u00e7 duyulmaktad\u0131r. Deprem \u00f6ncesi \u00e7al\u0131\u015fmalar kapsam\u0131nda KKTC genelinde yap\u0131lmas\u0131 gereken en \u00f6nemli \u00e7al\u0131\u015fma Tsunami ve Kabuk Kal\u0131nl\u0131\u011f\u0131n\u0131n belirlenmesi \u00e7al\u0131\u015fmalar\u0131ndan sonra KKTC Deprem Tehlike Haritas\u0131\u2019n\u0131n olu\u015fturulmas\u0131d\u0131r.\u201d<\/p>\n\n\n\n<\/figure>\n\n\n\n<\/figure>\n\n\n\n
MTA Genel M\u00fcd\u00fcrl\u00fc\u011f\u00fc Jeoloji Et\u00fctleri Dairesi Ba\u015fkan\u0131 Do\u00e7. Dr. Selim \u00d6zalp ve MTA Genel M\u00fcd\u00fcrl\u00fc\u011f\u00fc Jeoloji Et\u00fctleri Dairesi Ba\u015fkanl\u0131\u011f\u0131 T\u00fcrkiye Paleosismoloji Ara\u015ft\u0131rmalar\u0131 Projesi Ba\u015fkan\u0131 ve Jeoloji Y\u00fcksek M\u00fchendisi Hasan Elmac\u0131, YEN\u0130D\u00dcZEN’in sorular\u0131n\u0131 yan\u0131tlad\u0131… <\/em><\/strong><\/p>\n\n\n\n
H\u00fcseyin \u00d6ZBARI\u015eCI Son d\u00f6nemde art\u0131\u015f g\u00f6steren deprem sars\u0131nt\u0131lar\u0131 devam ederken, 2023 y\u0131l\u0131nda K\u0131br\u0131s i\u00e7in deprem ara\u015ft\u0131rmas\u0131 yapan T\u00fcrkiye\u2019deki Maden Tetkik ve Arama Genel M\u00fcd\u00fcrl\u00fc\u011f\u00fc (MTA) \u00e7al\u0131\u015fmalar\u0131n\u0131 s\u00fcrd\u00fcr\u00fcyor. MTA Genel M\u00fcd\u00fcrl\u00fc\u011f\u00fc Jeoloji Et\u00fctleri Dairesi Ba\u015fkan\u0131 Do\u00e7. Dr. Selim \u00d6zalp ve MTA Genel M\u00fcd\u00fcrl\u00fc\u011f\u00fc Jeoloji Et\u00fctleri Dairesi Ba\u015fkanl\u0131\u011f\u0131 T\u00fcrkiye Paleosismoloji Ara\u015ft\u0131rmalar\u0131 Projesi Ba\u015fkan\u0131 ve Jeoloji Y\u00fcksek M\u00fchendisi […]<\/p>\n","protected":false},"author":1,"featured_media":2054,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[5],"tags":[],"class_list":["post-2053","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-gundem"],"amp_enabled":true,"_links":{"self":[{"href":"https:\/\/dikdurus.com\/index.php\/wp-json\/wp\/v2\/posts\/2053","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/dikdurus.com\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/dikdurus.com\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/dikdurus.com\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/dikdurus.com\/index.php\/wp-json\/wp\/v2\/comments?post=2053"}],"version-history":[{"count":1,"href":"https:\/\/dikdurus.com\/index.php\/wp-json\/wp\/v2\/posts\/2053\/revisions"}],"predecessor-version":[{"id":2055,"href":"https:\/\/dikdurus.com\/index.php\/wp-json\/wp\/v2\/posts\/2053\/revisions\/2055"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/dikdurus.com\/index.php\/wp-json\/wp\/v2\/media\/2054"}],"wp:attachment":[{"href":"https:\/\/dikdurus.com\/index.php\/wp-json\/wp\/v2\/media?parent=2053"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/dikdurus.com\/index.php\/wp-json\/wp\/v2\/categories?post=2053"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/dikdurus.com\/index.php\/wp-json\/wp\/v2\/tags?post=2053"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}
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