TÜRKİYE İÇ ANADOLU KRİSTALİN KOMPLEKSİ (KIRŞEHİR BLOK) İÇİN AEROMAGNETİK VERİLERLE YAPISAL TRENDLERİNİN İNCELENMESİ

Yıl 2021, Cilt: 8 Sayı: 15, 498 - 507, 31.12.2021

Ezgi Erbek Kıran

https://doi.org/10.54365/adyumbd.997085

Öz

Bu çalışmanın temel amacı, Türkiye'deki Orta Anadolu Kristalin Kompleksindeki (Kırşehir Bloğu), bozucu kaynakların yer altı yapısal özelliklerini ve derinliklerini aeromanyetik verilerden belirlemektir. Bu amaçla aeromanyetik verilere spektral analiz tekniği, analitik sinyal (AS) ve tilt açısı yöntemi uygulanmıştır. Bozucu kaynakların derinliklerinin 8,48 km ile 1,60 km arasında değiştiği tespit edilmiştir. AS ve tilt açısı yöntemi bölgesel anomalilere uygulanmış ve saha gözlemiyle tanımlanan jeolojik birimlerin yüzeyin altında daha derin bir köke sahip olduğunu görülmüştür. Ayrıca jeolojik haritanın merkezinde manyetik özelliklere sahip kayaçlar olmamasına rağmen tilt haritasında manyetize bir yapının varlığı tespit edilmiştir. Bu olgu, bölgede kıtasal kırıntılı kayaçlarla kaplanmış olabilecek yüksek oranda manyetize olmuş bir birimin varlığı olarak değerlendirilebilir.

Anahtar Kelimeler

Analitik sinyal, Tilt- derinlik yöntemi, havadan manyetik veri

INVESTIGATION OF THE STRUCTURAL TRENDS THROUGH AEROMAGNETIC DATA FOR THE CENTRAL ANATOLIAN CRYSTALLINE COMPLEX (KIRSEHIR BLOCK), TURKEY

Öz

The main goal of this study is to delineate the subsurface structural features and depths of the causative sources in the Central Anatolian Crystalline Complex (Kirsehir Block), Turkey from aeromagnetic data. To this end, spectral analysis technique, analytic signal (AS) and tilt angle method were applied to the aeromagnetic data. The depths of causative sources were founded to vary between 8.48 km and 1.60 km. The AS and tilt angle method was implemented to regional anomalies and it was seen that the geological units defined by the field observation have a deeper root below the surface. In addition, although there are no rocks that have magnetic properties in the center of the geological map, the existence of a magnetized structure in the tilt map was determined. This phenomenon can be evaluated as the existence of a highly magnetized unit in the region that may have been covered by continental clastic rocks.

Anahtar Kelimeler

Analytic signal, tilt-depth method, aeromagnetic data, Analytic signal, tilt-depth method, aeromagnetic data

Kaynakça

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