Testing Miocene remagnetization of Bey Dağları: timing and amount of neogene rotations in SW Turkey

DEKKERS, Mark J.; KOÇ, Ayten; VAN HINSBERGEN, Douwe J.J.

Testing Miocene remagnetization of Bey Dağları: timing and amount of neogene rotations in SW Turkey

Douwe J.J. VAN HINSBERGEN, (Palaeomagnetic Lab. ‘Fort Hoofddijk’, Fac. of Geosciences, Utrecht Univercity Budapestlaan 17, 3584 CD Utrecht, The Netherlands)

Mark J. DEKKERS, (Palaeomagnetic Lab. ‘Fort Hoofddijk’, Fac. of Geosciences, Utrecht Univercity Budapestlaan 17, 3584 CD Utrecht, The Netherlands)

Ayten KOÇ (ODTÜ Müh. Fakültesi, Jeoloji Müh. Bölümü, Ankara, Türkiye)

Turkish Journal of Earth Sciences

6 0

Yıl: 2010 Cilt: 19 Sayı: 2 Sayfa Aralığı: 123 - 156 Metin Dili: Türkçe İndeks Tarihi: 29-07-2022

Testing Miocene remagnetization of Bey Dağları: timing and amount of neogene rotations in SW Turkey

Öz:

Bu çalışma Ege oroklinalinin güneybatı Türkiye’deki doğu kanadı rotasyonunun zamanı ve miktarını yeniden değerlendirmektedir. Bu oroklinal için geçerli güncel model, Geç Kretase−Eosen yaşlı platform karbonatları ile Alt Miyosen filiş çökellerinin yüzlekler verdiği Beydağları bölgesinin saatin tersi istikamette 25−30°’lik bir açı ile döndüğü şeklindedir. Bu modele göre rotasyon Miyosen yeniden mıknatıslanmasından sonra meydana gelmiş olup, Ege oroklininin batı ve doğu kanatları rotasyonlarının farklı zamanlarda gerçekleşmiş olabileceği gerçeğini dışlamaz. Bu modeli test etmek amacıyla, Beydağları Alt Miyosen istiflerinde ayrıntılı paleomanyetik çalışma icra edilmiştir. Korkuteli ve Doğantaş civarında, Beydağları kireçtaşları ile uyumsuzluk gösteren Akitaniyen birimler ile başlayıp Üst Burdigaliyen–Alt Langiyen’a kadar uzanan Miyosen ön-ülke havza stratigrafisine sahip iki kompozit kesit örneklenmiş ve zengin bir paleomanyetik analiz veri gurubu elde edilmiştir. Akitaniyen kireçtaşları ile Burdigalian mavi renkli killerdeki Kalıntı Doğal Mıknatıslanma (KDM) baskın olarak magnetit ve ikincil olarak grigayt ile hematite bağlıdır. Pozitif Terselme Testi, kalıntı doğal mıknatıslanma (KDM) kazanıldıktan sonra yeğince kompaksiyona uğramış olan örneklerden elde edilen polarite verilerinin jeomanyetik polarite zaman çizelgesi ile uyumlu oluşu, güvenli bir şekilde paleo-seküler değişime atfedilebilecek KDM yönlerindeki saçılım ile son zamanlarda önerilen ve eşsıcaklık ısıl kalıntı mıknatıslanma (EIKM) kazanım eğrilerinin test edildiği Uç Eleman Model Test sonuçlarının pozitif olması hep birlikte Beydağları Platfomu Miyosen çökellerinin yeniden mıknatıslanma geçirmediği sonucuna işaret etmektedir. Var olan verilerin kısmen yeniden değerlendirilmesi yanında bizim sonuçlarımız, Beydağları bölgesinin Geç Kretase ile Geç Burdigaliyen arasında herhangi bir rotasyona uğramadığı, günümüzden 16 ile 5 My önce, yani Orta–Geç Miyosen aralığında ve daha önceden kaydedildiği üzere, Antalya’nın kuzeyindeki rotasyona uğramamış Pliyosen çökellerin depolanmasından önce ki dönemde, saatin tersi yönde 20°’lik bir rotasyona maruz kaldığına işaret etmektedir. Doğu kanat için önerdiğimiz 16−5 My’lik yeni yaş sınırlamamız ile (genel olarak) batı kanat için daha önceden yayınlanmış olan 15−8 My karşılaştırıldığında Ege oroklinalinin doğu ve batı kanatlarının eşzamanlı olarak rotasyona maruz kaldıkları sonucu ortaya çıkar. Beydağları’nın rotasyonu, muhtemelen güneyde Afrika levha sınırı ile, doğuda ise blok rotasyonlarına bağlı ortaya çıkan ve sağ yönlü transpresyonu paylaşan Aksu bindirmesi ile sağ yönlü Kırkkavak Fayı ile sınırlanmıştır. Batı Anadolu’nun Beydağları’nın kuzeyinde ve batısındaki rotasyonları ise gelecekteki yayınların konusu olacaktır.

Anahtar Kelime:

Konular: Jeoloji

Beydağları’nın Miyosen’de yeniden mıknatıslanmasının test edilmesi: Türkiye güneybatısındaki neojen rotasyonlarının zamanı ve miktarı

Öz:

Here we reassess the timing and amount of rotation of the eastern limb of the Aegean orocline, located in SW Turkey. The current model for this orocline involves a 25−30° counterclockwise (CCW) rotation of the Bey Dağları region, which exposes upper Cretaceous to Eocene platform carbonates and lower Miocene flysch deposits. In this model the rotation has to postdate a Miocene remagnetization, which would not exclude non-synchroneity between rotations of the western and eastern limbs of the Aegean orocline. To test this model a detailed palaeomagnetic study was conducted on lower Miocene strata in the Bey Dağları area. Two (composite) sections were sampled near Korkuteli and Doğantaş, spanning the lower Miocene foreland basin stratigraphy from the Aquitanian unconformity with the Bey Dağları limestones to the uppermost Burdigalian−lowermost Langhian, and a wide array of palaeomagnetic analyses were obtained. The natural remanent magnetization (NRM) in the Aquitanian limestones and Burdigalian blue clays resides dominantly in magnetite with minor greigite and haematite. A positive reversals test, a correlation of obtained polarity patterns to the geomagnetic polarity timescale, showing significant compaction following acquisition of the NRM, a scatter in NRM directions that can be confidently attributed to palaeosecular variation and a positive recently-proposed end-member model test of the acquisition curves of isothermal remanent magnetization (IRM) all show that the Miocene sediments on the Bey Dağları platform have not been remagnetized. Our new results, combined with a partial reassessment of existing data, imply that the Bey Dağları region underwent no rotation between the late Cretaceous and late Burdigalian, and 20° counterclockwise rotation between 16 and 5 Ma, i.e. during the middle to late Miocene and prior to deposition of previously reported non-rotated Pliocene sediments north of Antalya. The two limbs of the Aegean orocline thus rotated simultaneously: our new age constraints of 16−5 Ma in the east, compare with (largely) 15−8 Ma in the west, as published previously. The rotation of the Bey Dağları was probably bounded in the south at the plate boundary with Africa, and in the east by the Aksu thrust and Kırkkavak dextral strike-slip fault, which together partitioned dextral transpression induced by the rotating block. Accommodation of the western Anatolian rotations to the north and west of the Bey Dağları will be the subject of a future publication.

Anahtar Kelime:

Konular: Jeoloji

Belge Türü: Makale Makale Türü: Araştırma Makalesi Erişim Türü: Erişime Açık

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APA	VAN HINSBERGEN D, DEKKERS M, KOÇ A (2010). Testing Miocene remagnetization of Bey Dağları: timing and amount of neogene rotations in SW Turkey. , 123 - 156.
Chicago	VAN HINSBERGEN Douwe J.J.,DEKKERS Mark J.,KOÇ Ayten Testing Miocene remagnetization of Bey Dağları: timing and amount of neogene rotations in SW Turkey. (2010): 123 - 156.
MLA	VAN HINSBERGEN Douwe J.J.,DEKKERS Mark J.,KOÇ Ayten Testing Miocene remagnetization of Bey Dağları: timing and amount of neogene rotations in SW Turkey. , 2010, ss.123 - 156.
AMA	VAN HINSBERGEN D,DEKKERS M,KOÇ A Testing Miocene remagnetization of Bey Dağları: timing and amount of neogene rotations in SW Turkey. . 2010; 123 - 156.
Vancouver	VAN HINSBERGEN D,DEKKERS M,KOÇ A Testing Miocene remagnetization of Bey Dağları: timing and amount of neogene rotations in SW Turkey. . 2010; 123 - 156.
IEEE	VAN HINSBERGEN D,DEKKERS M,KOÇ A "Testing Miocene remagnetization of Bey Dağları: timing and amount of neogene rotations in SW Turkey." , ss.123 - 156, 2010.
ISNAD	VAN HINSBERGEN, Douwe J.J. vd. "Testing Miocene remagnetization of Bey Dağları: timing and amount of neogene rotations in SW Turkey". (2010), 123-156.

APA	VAN HINSBERGEN D, DEKKERS M, KOÇ A (2010). Testing Miocene remagnetization of Bey Dağları: timing and amount of neogene rotations in SW Turkey. Turkish Journal of Earth Sciences, 19(2), 123 - 156.
Chicago	VAN HINSBERGEN Douwe J.J.,DEKKERS Mark J.,KOÇ Ayten Testing Miocene remagnetization of Bey Dağları: timing and amount of neogene rotations in SW Turkey. Turkish Journal of Earth Sciences 19, no.2 (2010): 123 - 156.
MLA	VAN HINSBERGEN Douwe J.J.,DEKKERS Mark J.,KOÇ Ayten Testing Miocene remagnetization of Bey Dağları: timing and amount of neogene rotations in SW Turkey. Turkish Journal of Earth Sciences, vol.19, no.2, 2010, ss.123 - 156.
AMA	VAN HINSBERGEN D,DEKKERS M,KOÇ A Testing Miocene remagnetization of Bey Dağları: timing and amount of neogene rotations in SW Turkey. Turkish Journal of Earth Sciences. 2010; 19(2): 123 - 156.
Vancouver	VAN HINSBERGEN D,DEKKERS M,KOÇ A Testing Miocene remagnetization of Bey Dağları: timing and amount of neogene rotations in SW Turkey. Turkish Journal of Earth Sciences. 2010; 19(2): 123 - 156.
IEEE	VAN HINSBERGEN D,DEKKERS M,KOÇ A "Testing Miocene remagnetization of Bey Dağları: timing and amount of neogene rotations in SW Turkey." Turkish Journal of Earth Sciences, 19, ss.123 - 156, 2010.
ISNAD	VAN HINSBERGEN, Douwe J.J. vd. "Testing Miocene remagnetization of Bey Dağları: timing and amount of neogene rotations in SW Turkey". Turkish Journal of Earth Sciences 19/2 (2010), 123-156.