Nazmi OTLU, Özlem GÜNEY, Matt HEIZLER, Raymond C. JONCKHEERE, Marion TICHOMIROWA, Durmuş BOZTUĞ

$^{207}Pb- ^{206}Pb$, $^{40}Ar- ^{39}Ar$ and fission-track geothermochronology quantifying cooling and exhumation history of the Kaman- Kırşehir region intrusions, Central Anatolia, Turkey

Kaman-Kırşehir yöresi granitik intrüzyonları, Torid-Anatolid platformu (TAP) ve yitim zonu üzerinde gelişen Orta Anadolu Ofiyolitini (OAO) içeren okyanusal ada yayı arasında Senomaniyen–Türoniyen’de gerçekleşen kıta-okyanusal ada yayı çarpışması sonrası gerilme rejiminde oluşmuşlardır. Bu granitoyidler, kuzeyden güneye doğru, Çamsarı kuvars siyeniti, Hamit kuvars siyeniti, Bayındır nefelin-kankrinit siyeniti, Durmuşlu nefelin-nozeyan-melanit siyenit porfiri ve Baranadağ kuvars monzoniti birimlerinden oluşur. Bu intrüzif kayaçlar, Orta Anadolu Kristalin Karmaşığına (OAKK) ait metamorfik kayaçlarla OAO’ne ait birimleri sıcak dokanakla keser ve Geç Paleosen–Erken/Orta Eosen yaşlı sedimanter birimler tarafından uyumsuz olarak örtülürler. Çamsarı kuvars siyenitinin tek zirkon $^{207}Pb- ^{206}Pb$ buharlaşma yaşı 95.7±5.1 My olarak bulunmuştur; Hamit ve Baranadağ birimlerinin yaşları ise birbirlerinden ayırt edilemeyecek derecede yakın olup, ağırlıklı ortalama yaşları 74.3±4.5 My olarak belirlenmiştir. Benzer şekilde, Hamit ve Baranadağ birimlerinin amfibol $^{40}Ar- ^{39}Ar$ yaşları da birbirlerinden ayırt edilemeyecek derecede yakındır ve ağırlıklı ortalama yaş 72.7±0.1 My olarak belirlenmiştir. Çamsarı, Hamit, Baranadağ ve Durmuşlu birimlerinin apatit fizyon izi yaş verilerinin (deniz düzeyinden) yüksekliğe göre değişimleri incelendiğinde, ~57 ve ~61 My aralığında oldukça hızlı bir yükselme hızıyla (> 1 km/My) yüzeylendikleri belirlenmiştir. Böyle bir yüzeylenme tarihçesi, aynı zamanda, fizyon izi uzunluk ölçümlerine dayalı zaman-sıcaklık modelleme çalışmalarıyla da desteklenmiştir. Apatit fizyon izi jeotermokronolojisi verileriyle belirlenen Erken–Orta Paleosen yaşlı bu hızlı yüzeylenmenin, İzmir-Ankara-Erzincan (İAE) okyanusunun kapanmasını takiben TAP ve Avrasya Levhası (AL) arasında gelişen kıta-kıta çarpışmasına bağlı sıkışma rejimiyle meydana geldiği ve hatta bu sırada Orta Anadolu önülke basenlerinin de (OAÖB) açıldığı ileri sürülmektedir.

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