{"id":64748,"date":"2025-04-04T15:14:06","date_gmt":"2025-04-04T12:14:06","guid":{"rendered":"https:\/\/bilimvegelecek.com.tr\/?p=64748"},"modified":"2025-04-04T20:18:09","modified_gmt":"2025-04-04T17:18:09","slug":"28-mart-2025-myanmar-mandalya-depreminin-7-7-kimligi-ve-sonuclari","status":"publish","type":"post","link":"https:\/\/bilimvegelecek.com.tr\/index.php\/2025\/04\/04\/28-mart-2025-myanmar-mandalya-depreminin-7-7-kimligi-ve-sonuclari","title":{"rendered":"28 Mart 2025 Myanmar (Mandalya) depreminin (7.7) kimli\u011fi ve sonu\u00e7lar\u0131"},"content":{"rendered":"

Haluk Eyido\u011fan<\/strong><\/p>\n

Myanmar Birli\u011fi Cumhuriyeti\u2019nin (Burma), G\u00fcneydo\u011fu Asya\u2019da Hindistan\u2019\u0131n do\u011fusunda yer almaktad\u0131r. \u00dclkenin g\u00fcney ve g\u00fcneybat\u0131da Andaman Denizi ve Bengal K\u00f6rfezi’ne k\u0131y\u0131s\u0131 vard\u0131r. Asya K\u0131tas\u0131\u2019n\u0131n en b\u00fcy\u00fck 10. \u00dclkesi olan \u00fclke Myanmar\u2019\u0131n n\u00fcfusu 60 milyon civar\u0131ndad\u0131r.<\/p>\n

Myanmar\u2019\u0131n uygarl\u0131k tarihi 9. y\u00fczy\u0131la kadar uzan\u0131r. 19. y\u00fczy\u0131lda ger\u00e7ekle\u015fen \u00fc\u00e7 \u0130ngiliz-Birman Sava\u015f\u0131 sonucunda \u00fclke\u00a0Britanya s\u00f6m\u00fcrgesi olmu\u015ftur. Myanmar II. D\u00fcnya Sava\u015f\u0131’nda\u00a0Japon\u00a0i\u015fgaline u\u011fram\u0131\u015ft\u0131r. 1945’te\u00a0M\u00fcttefiklerce\u00a0geri al\u0131nm\u0131\u015f ve 1948’de ba\u011f\u0131ms\u0131zl\u0131\u011f\u0131na kavu\u015fmu\u015ftur. 1962’deki bir asker\u00ee darbenin ard\u0131ndan asker\u00ee cunta y\u00f6netimi kurulmu\u015ftur. Myanmar\u2019da etnik grup aras\u0131nda \u00e7eki\u015fmeler ya\u015fanm\u0131\u015f ve i\u00e7 sava\u015flar 70 y\u0131l\u0131 s\u00fcrm\u00fc\u015ft\u00fcr. 2010 genel se\u00e7imlerinin ard\u0131ndan 2011’de asker\u00ee cunta feshedilmi\u015f ve sivil bir h\u00fck\u00fbmet iktidara gelmi\u015ftir. Myanmar ordusu 1 \u015eubat 2021’de\u00a0bir asker\u00ee darbe ger\u00e7ekle\u015ftirerek\u00a0y\u00f6netimi ele ge\u00e7irmi\u015ftir. Myanmar, do\u011fal kaynaklar bak\u0131m\u0131ndan \u00e7ok zengin bir \u00fclke olmas\u0131na ra\u011fmen, d\u00fcnyan\u0131n ekonomik bak\u0131mdan en e\u015fitsiz \u00fclkesi olarak bilinmektedir.<\/p>\n

Myanmar\u2019\u0131n Mandalya \u015fehrinin yak\u0131n\u0131nda 28 Mart 2025 tarihinde yerel saatle 12:50\u2019de 7.7 b\u00fcy\u00fckl\u00fc\u011f\u00fcnde y\u0131k\u0131c\u0131 bir b\u00fcy\u00fck deprem olmu\u015ftur. G\u00fcneydo\u011fu Asya\u2019da benzer b\u00fcy\u00fckl\u00fckte depremler milyonlarca y\u0131ld\u0131r s\u00fcremektedir. Nedeni, Hint Levhas\u0131* ile Avrasya Levhas\u0131 aras\u0131ndaki k\u0131tasal \u00e7arp\u0131\u015fman\u0131n (\u015eekil-1) sonucudur. B\u00f6lgenin jeolojik \u00f6zellikleri nedeniyle bu t\u00fcr depremler ne ilk ne de son olacakt\u0131r.<\/p>\n

Levha Tektoni\u011fi ara\u015ft\u0131rmalar\u0131na g\u00f6re, 70 milyon \u00f6nce Hint Okyanusu\u2019nda kuzeye do\u011fru hareket eden Hint Levhas\u0131 10 milyon y\u0131l \u00f6nce Avrasya Levhas\u0131\u2019na bindirmi\u015f (\u00e7arpm\u0131\u015f) ve bug\u00fcn Himalaya Da\u011f\u0131 ad\u0131n\u0131 verdi\u011fimiz ve d\u00fcnyan\u0131n en y\u00fcksek tepelerine sahip devasa da\u011f s\u0131ralar\u0131n\u0131 ve Tibet Platosu\u2019nu olu\u015fturmu\u015ftur.<\/p>\n

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Hint Levhas\u0131\u2019n\u0131n kuzeye hareket h\u0131z\u0131, bindirme s\u0131n\u0131r\u0131 boyunca (\u015eekil-1) 29 mm\/y\u0131l ile 36 mm\/y\u0131l aras\u0131nda de\u011fi\u015fmektedir. Hint-Avrasya levhalar\u0131n\u0131n bindirme s\u0131n\u0131r\u0131n\u0131n uzunlu\u011fu do\u011fu-bat\u0131 y\u00f6n\u00fcnde 2.500 km civar\u0131ndad\u0131r ve Himalaya Bindirme S\u0131n\u0131r\u0131 (Cephesi) ad\u0131yla an\u0131l\u0131r. Bu s\u0131n\u0131r\u0131n kuzeyinde Tibet Platosu yer al\u0131r ve levhalar\u0131n \u00e7arp\u0131\u015fmas\u0131 yery\u00fcz\u00fcnde \u00e7ok karma\u015f\u0131k jeolojik ve tektonik yap\u0131lar olu\u015fturmu\u015ftur. Bu karma\u015f\u0131k jeolojik yap\u0131lar, Tibet Platosu\u2019nun bat\u0131s\u0131nda kuzey-g\u00fcney do\u011frultusunda uzanan S\u00fcleyman S\u0131rada\u011flar\u0131’n\u0131n etekleri, do\u011fuda Hint-Burma Yay\u0131 ve Hindistan’\u0131n kuzeyinde do\u011fu-bat\u0131 do\u011frultusunda uzanan yap\u0131lar ile kendini g\u00f6stermektedir. Tibet Platosu bir dizi b\u00fcy\u00fck (>1000 km) do\u011fu-bat\u0131 y\u00f6nl\u00fc, sol yanal, do\u011frultu at\u0131ml\u0131 fay taraf\u0131ndan kesilir. Bu b\u00f6lgedeki sa\u011f yanal, do\u011frultu at\u0131ml\u0131 faylar (sol yanal faylarla kar\u015f\u0131la\u015ft\u0131r\u0131labilir b\u00fcy\u00fckl\u00fckte) Karakurum, Red River ve Sagaing faylar\u0131n\u0131 kapsar.<\/p>\n

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Levhalar\u0131n hareketleri s\u00fcrmekte olup zaman zaman b\u00fcy\u00fckl\u00fc\u011f\u00fc 8\u2019e varan b\u00fcy\u00fck depremler b\u00f6lgede b\u00fcy\u00fck hasar ve can kay\u0131plar\u0131na neden olmaktad\u0131r. \u015eekil-2\u2019de USGS (2025) kay\u0131tlar\u0131na g\u00f6re 1900-2025 y\u0131llar\u0131 aras\u0131nda Avrasya ve Hint levhalar\u0131 \u00e7evresinde b\u00fcy\u00fckl\u00fc\u011f\u00fc 6.0 ve daha fazla olan 576 adet depremin d\u0131\u015f merkez da\u011f\u0131l\u0131mlar\u0131 g\u00f6r\u00fclmektedir.<\/p>\n

Yo\u011fun n\u00fcfus bar\u0131nd\u0131ran g\u00fcney Asya\u2019da olu\u015fan ve b\u00fcy\u00fck kay\u0131plara neden depremlere \u00f6rnek olarak; Bihar\u2019da 1934 y\u0131l\u0131nda 8.1, Kangra\u2019da 1905 y\u0131l\u0131nda 7.5 ve Ke\u015fmir\u2019de 2005 y\u0131l\u0131nda 7.6 b\u00fcy\u00fckl\u00fc\u011f\u00fcndeki depremleri g\u00f6sterebilir. Son iki deprem, bug\u00fcne kadar Himalaya ve Tibet Platosu civar\u0131nda olan depremler aras\u0131nda en y\u00fcksek \u00f6l\u00fcm oranlar\u0131na neden olmu\u015ftur. Bu depremlerde toplamda 100.000’den fazla can kayb\u0131 olmu\u015f ve milyonlarca ki\u015fi evsiz kalm\u0131\u015ft\u0131r. Deprem kay\u0131t\u00e7\u0131lar\u0131yla (sismograf) kaydedilen en b\u00fcy\u00fck Himalaya depremi, 15 A\u011fustos 1950’de do\u011fu Hindistan’daki Assam’da olmu\u015ftur. 8.6 b\u00fcy\u00fckl\u00fc\u011f\u00fcndeki deprem Orta Asya’n\u0131n geni\u015f bir b\u00f6lgesinde yayg\u0131n olarak alg\u0131lanm\u0131\u015f ve d\u0131\u015f merkezi \u00e7evresindeki k\u00f6ylerde b\u00fcy\u00fck hasara neden olmu\u015ftur.<\/p>\n

28 Mart 2025 tarihinde 7.7 b\u00fcy\u00fckl\u00fc\u011f\u00fcnde olan ve Myanmar ve \u00e7evresindeki \u00fclkeleri etkileyen deprem, kuzey-g\u00fcney do\u011frultusunda kesen ve b\u00f6lgedeki en b\u00fcy\u00fck faylardan biri olan Sagaing Fay\u0131 \u00fczerinde olmu\u015ftur (\u015eekil-2). Sagaing Fay\u0131, Sunda Levhas\u0131\u2019n\u0131n Shan Platosu’nu s\u0131n\u0131rlayan do\u011fu s\u0131n\u0131r\u0131n\u0131 belirler. Sagaing Fay\u0131 y\u0131lda 20 mm h\u0131zla sa\u011f y\u00f6nl\u00fc do\u011frultu at\u0131ml\u0131 kayma ile hareket eder. B\u00f6lgede yer alan t\u00fcm bu k\u0131r\u0131k ve faylar Hindistan ve Avrasya levhalar\u0131n\u0131n halen s\u00fcren bindirme hareketleriyle ili\u015fkili olarak yer kabu\u011funun bas\u0131n\u00e7 alt\u0131nda k\u0131salmas\u0131n\u0131n sonucudur. Ters faylar kuzey-g\u00fcney s\u0131k\u0131\u015fmay\u0131, normal ve do\u011frultu at\u0131ml\u0131 faylar ise do\u011fu-bat\u0131 geni\u015fleme hareketlerine neden olur. Myanmar, en son 28 Mart 2025 tarihinde \u00a0Mandalay b\u00f6lgesindeki 7.7 b\u00fcy\u00fckl\u00fc\u011f\u00fcndeki deprem gibi ge\u00e7mi\u015fte \u00e7ok say\u0131da y\u0131k\u0131c\u0131 depremlere maruz kalm\u0131\u015ft\u0131r (\u015eekil-2, \u00c7izelge-1).<\/p>\n

\u00c7izelge-1<\/em>. Myanmar ve \u00e7evresinde 1950-2025 y\u0131llar\u0131 aras\u0131nda b\u00fcy\u00fckl\u00fckleri 8.6 ile 7.6 aras\u0131nda de\u011fi\u015fen depremlerin listesi.<\/em><\/p>\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n
Y\u0131l, Konum, B\u00fcy\u00fckl\u00fck <\/strong><\/td>\n<\/tr>\n
1950, Assam-Tibet, 8.6<\/td>\n<\/tr>\n
1934, Nepal, 8.0<\/td>\n<\/tr>\n
1941, Bamboo-Flat India, 8.0<\/td>\n<\/tr>\n
2008, Tianpeng China, 7.9<\/td>\n<\/tr>\n
1912, Taunggyi Myanmar, 7.9<\/td>\n<\/tr>\n
1937, Qinghai China, 7.8<\/td>\n<\/tr>\n
2015, Bharatpur Nepal, 7.8,<\/td>\n<\/tr>\n
1951, Nagqu China, 7.7,<\/td>\n<\/tr>\n
1988, Jinghong China, 7.7,<\/td>\n<\/tr>\n
2025, Mandalay Myanmar, 7.7,<\/td>\n<\/tr>\n
1946, Myanmar, 7.6,<\/td>\n<\/tr>\n
1931, Sarupathar India, 7.6,<\/td>\n<\/tr>\n
1947, Qinghai-Sichuan border region China, 7.6<\/td>\n<\/tr>\n
1930, Pyu Myanmar, 7.5<\/td>\n<\/tr>\n
2009, Bamboo-Flat India, 7.5<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n

28 Mart 2025 depremi s\u0131ras\u0131nda Sagaing Fay\u0131\u2019n\u0131n 200 km uzunluktaki b\u00f6l\u00fcm\u00fc hareket etmi\u015f ve fay \u00fczerinde 6 metre civar\u0131nda kaymalar olmu\u015ftur (\u015eekil-3a, b). \u015eekil-3a,b; Sismolojik ve Jeodezik y\u00f6ntemlerin bir arada kullan\u0131lmas\u0131yla yap\u0131lan modelleme sonucu elde edilen deprem kayna\u011f\u0131ndaki hareket modelidir. \u015eekil-3a\u2019da uzunlu\u011fu 500 km\u2019ye, derinli\u011fi 10 km\u2019ye eri\u015fen fay\u0131n \u00fczerinde olu\u015fan kayma hareketinin da\u011f\u0131l\u0131m\u0131, \u015eekil 3b\u2019de ise fay\u0131n \u00fczerindeki kayma yerde\u011fi\u015ftirmesinin zamana g\u00f6re de\u011fi\u015fimi (kaynak fonksiyonu) g\u00f6sterilmektedir. \u015eekil-3a\u2019daki k\u0131rm\u0131z\u0131 alanlar kayman\u0131n en b\u00fcy\u00fck oldu\u011fu fay kesimlerini g\u00f6sterir. \u015eekil-3a\u2019da faylanma hareketi d\u00f6rt ard\u0131\u015f\u0131k fay modeli y\u00fczeyi \u00fczerinde g\u00f6sterilmi\u015ftir. Faylanma, Mandalay \u015fehrinin kuzeyinde ba\u015flam\u0131\u015f ve g\u00fcney do\u011fru h\u0131zla ilerlemi\u015ftir. Kayma hareketinin en y\u00fcksek de\u011feri 4.5 metrelik kayma ile kuzeydeki 150 km uzunlu\u011fundaki b\u00f6l\u00fcmdedir. \u015eekil-3b\u2019de faylanman\u0131n ger\u00e7ekle\u015fmesi s\u0131ras\u0131nda olu\u015fan kayman\u0131n zaman i\u00e7erisindeki davran\u0131\u015f\u0131 g\u00f6r\u00fclmektedir. Deprem ba\u015flad\u0131ktan 20 saniye sonra sarsma g\u00fcc\u00fc en y\u00fcksek d\u00fczeye \u00e7\u0131km\u0131\u015f, ilerleyen zamanda azalarak s\u00fcrm\u00fc\u015f ve toplam deprem s\u00fcresi 100 saniye olmu\u015ftur.<\/p>\n

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Fay\u0131n yery\u00fcz\u00fcne yak\u0131n alanlar\u0131nda yarat\u0131\u011f\u0131 yer k\u0131r\u0131lmalar\u0131 etkileri yan\u0131 s\u0131ra, olu\u015fan y\u00fcksek sarsma \u015fiddeti nedeniyle de yollar, k\u00f6pr\u00fcler ve di\u011fer alt yap\u0131 unsurlar\u0131 \u00f6nemli hasarlara u\u011fram\u0131\u015ft\u0131r. 7.7 b\u00fcy\u00fckl\u00fc\u011f\u00fcndeki depremin maksimum hasar \u015fiddeti 10 d\u00fczeyine ula\u015fm\u0131\u015ft\u0131r. \u015eekil-4a\u2019da depremi olu\u015fturan Sagaing Fay\u0131 boyunca olu\u015fan deprem \u015fiddetinin da\u011f\u0131l\u0131m\u0131n\u0131 (koyu k\u0131rm\u0131z\u0131 alan \u015fiddetin 10 oldu\u011fu alan\u0131) ve \u015eekil-4b\u2019de ise e\u015f\u015fiddet alanlar\u0131n\u0131 ve fay boyunca s\u0131v\u0131la\u015fma tehlikesi y\u00fcksek b\u00f6lgeleri (koyu renkli alanlar) g\u00f6stermektedir.<\/p>\n

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\u015eekil-4b\u2019de g\u00f6r\u00fclece\u011fi gibi \u00e7ok uzakta olan Bangkok\u2019ta depremin ivme \u015fiddeti %0.1 g\u00a0 gibi olduk\u00e7a k\u00fc\u00e7\u00fck bir de\u011ferde olmas\u0131na ra\u011fmen \u015fehirde hasarlar g\u00f6zlenmi\u015f ve bir g\u00f6kdelen \u00e7\u00f6km\u00fc\u015ft\u00fcr.<\/p>\n

Myanmar\u2019daki Sagaing Fay\u0131 \u00fczerinde olan b\u00fcy\u00fck depremle ilgili bas\u0131n haberlerine g\u00f6re 3 Nisan 2025 tarihi itibar\u0131yla b\u00f6lgede eri\u015filebilen noktalarda can kayb\u0131 say\u0131s\u0131 3.000\u2019i ge\u00e7mi\u015ftir. B\u00f6lgedeki yo\u011fun n\u00fcfus ve g\u00f6zlenen a\u011f\u0131r hasar durumu g\u00f6z\u00f6n\u00fcne al\u0131nd\u0131\u011f\u0131nda can kayb\u0131 say\u0131s\u0131n\u0131n daha da artabilece\u011fi olas\u0131l\u0131\u011f\u0131 vard\u0131r. \u00c7\u00fcnk\u00fc, 7\u2019den b\u00fcy\u00fck depremler b\u00f6lge depremleridir ve \u00e7ok geni\u015f alanlarda hasar ve can kayb\u0131na neden olurlar. Bunun en son ve a\u011f\u0131r kay\u0131plara neden olan 6 \u015eubat 2023\u2019de Kahramanmara\u015f depremlerinde ya\u015fam\u0131\u015ft\u0131k. Deprem merkezine uzakl\u0131klar\u0131na ve n\u00fcfuslar\u0131na g\u00f6re b\u00f6lgedeki \u015fehirlerin bir b\u00f6l\u00fcm\u00fc \u00c7izelge-2\u2019de s\u0131ralanm\u0131\u015ft\u0131r.<\/p>\n

\u00c7izelge-2. 28 Mart 2025 Myanmar, Mandalay deprem merkezinin baz\u0131 \u015fehirlere uzakl\u0131\u011f\u0131 ve n\u00fcfuslar\u0131.<\/em><\/p>\n\n\n\n\n\n\n\n
Sagaing<\/td>\nSagain<\/td>\n16.1 km, N\u00fcfus: 78.739<\/td>\n<\/tr>\n
Mandalay<\/td>\nMandalay<\/td>\n17.2 km, N\u00fcfus: 1.208.099<\/td>\n<\/tr>\n
Kyaukse<\/td>\nMandalay<\/td>\n50.4 km, N\u00fcfus: 50.480<\/td>\n<\/tr>\n
Pyin Oo Lwin<\/td>\nMandalay<\/td>\n55.3 km, N\u00fcfus: 11.303<\/td>\n<\/tr>\n
Shwebo<\/td>\nSagain<\/td>\n66 km, N\u00fcfus: 88.914<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n

 <\/p>\n

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Tayland\u2019\u0131n ba\u015f\u015fehri Bangkok deprem merkezine 1.000 km uzakta olmas\u0131na ra\u011fmen olu\u015fan \u00f6nemli derecedeki hasarlar g\u00f6z\u00f6n\u00fcne al\u0131nd\u0131\u011f\u0131nda (\u015eekil-5), Mandalay\u2019a yak\u0131n olan yerle\u015fimlerdeki hasar\u0131n daha y\u00fcksek olma olas\u0131l\u0131\u011f\u0131 olduk\u00e7a y\u00fcksektir. \u00d6n\u00fcm\u00fczdeki g\u00fcnlerde bu b\u00fcy\u00fck depremin neden oldu\u011fu hasar ve can kay\u0131plar\u0131 ile ilgili bilgiler de\u011fi\u015fecektir. Nitekim baz\u0131 yard\u0131m kurulu\u015flar\u0131, uzak b\u00f6lgelerdeki bilgi kesintileri nedeniyle can kayb\u0131 say\u0131lar\u0131n\u0131n \u00f6nemli \u00f6l\u00e7\u00fcde artaca\u011f\u0131n\u0131 tahmin ediyor.<\/p>\n

Myanmar\u2019da 28 Mart 2025 tarihindeki Mandalay merkezli ve 7.7 b\u00fcy\u00fckl\u00fc\u011f\u00fcndeki deprem, b\u00fcy\u00fck depremlerin olduk\u00e7a uzak alanlarda hasarlar yaratabilecek b\u00f6lge depremleri oldu\u011funu, hareket eden faydan uzak bile olsa yap\u0131 \u00fcretiminde yetersiz m\u00fchendislik, malzeme ve denetim sorunlar\u0131 olan yerle\u015fim alanlar\u0131nda, depremden yay\u0131lan sismik dalgalar\u0131n yap\u0131lardaki hatalar\u0131 bulup y\u0131kt\u0131\u011f\u0131n\u0131 ve ac\u0131 sonu\u00e7lar olu\u015fturdu\u011funu 6 \u015eubat 2023 Kahramanmara\u015f depreminden sonra bize yeniden hat\u0131rlatan bir deprem olmu\u015ftur.<\/p>\n

* Yery\u00fcz\u00fcnde hareket eden k\u0131talar yerbilimlerinde \u201ctektonik levha\u201d olarak adland\u0131r\u0131l\u0131r.<\/p>\n","protected":false},"excerpt":{"rendered":"

Haluk Eyido\u011fan Myanmar Birli\u011fi Cumhuriyeti\u2019nin (Burma), G\u00fcneydo\u011fu Asya\u2019da Hindistan\u2019\u0131n do\u011fusunda yer almaktad\u0131r. \u00dclkenin g\u00fcney ve g\u00fcneybat\u0131da Andaman Denizi ve Bengal K\u00f6rfezi’ne k\u0131y\u0131s\u0131 vard\u0131r. Asya K\u0131tas\u0131\u2019n\u0131n en b\u00fcy\u00fck 10. \u00dclkesi olan \u00fclke Myanmar\u2019\u0131n n\u00fcfusu 60 milyon civar\u0131ndad\u0131r. Myanmar\u2019\u0131n uygarl\u0131k tarihi 9. y\u00fczy\u0131la kadar uzan\u0131r. 19. y\u00fczy\u0131lda ger\u00e7ekle\u015fen \u00fc\u00e7 \u0130ngiliz-Birman Sava\u015f\u0131 sonucunda \u00fclke\u00a0Britanya s\u00f6m\u00fcrgesi olmu\u015ftur. Myanmar II. […]<\/p>\n","protected":false},"author":1575,"featured_media":64754,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[19],"tags":[5479,10104,10105],"class_list":["post-64748","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-bilim-gundemi","tag-haluk-eyidogan","tag-myanmar","tag-myanmar-mandalya-depreminin"],"acf":[],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/bilimvegelecek.com.tr\/index.php\/wp-json\/wp\/v2\/posts\/64748","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=64748"}],"version-history":[{"count":0,"href":"https:\/\/bilimvegelecek.com.tr\/index.php\/wp-json\/wp\/v2\/posts\/64748\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/bilimvegelecek.com.tr\/index.php\/wp-json\/wp\/v2\/media\/64754"}],"wp:attachment":[{"href":"https:\/\/bilimvegelecek.com.tr\/index.php\/wp-json\/wp\/v2\/media?parent=64748"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/bilimvegelecek.com.tr\/index.php\/wp-json\/wp\/v2\/categories?post=64748"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/bilimvegelecek.com.tr\/index.php\/wp-json\/wp\/v2\/tags?post=64748"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}