Calibe KOÇ TAŞGIN, İbrahim TÜRKMEN, Cansu DİNİZ AKARCA

Bigadiç havzası (Balıkesir-Türkiye) Erken Miyosen göl çökellerinde sin-sedimanter deformasyon yapıları, taban kireçtaşı birimi

Batı Anadolu bölgesinde geç Oligosen – erken Miyosen’de başlayan genişleme ile ilişkilifaylarla sınırlı KD-GB, D-B doğrultulu havzalar gelişmiştir. Bu havzaların dolgularını volkanikve volkanoklastik ara seviyeli akarsu – göl çökelleri oluşturur. Bu çökeller yoğun uyumsuzluklarve yumuşak sediman deformasyon yapıları içermektedir. Söz konusu havzalardan birini oluşturanBigadiç Neojen Havzası’nın dolgusunu taban kireçtaşı birimi, alt tüf birimi, alt boratlı birim, üst tüfbirimi ve üst boratlı birim oluşturur. Kiltaşı, marn, kireçtaşı ve dolomitik kireçtaşı fasiyeslerindenoluşan taban kireçtaşı birimi derin göl ortamında çökelmiştir. Bigadiç güneyinde yüzeyleyentaban kireçtaşı biriminde yumuşak çökel deformasyon yapıları tanımlanmıştır. Bunlar; Kaymaoturma yapıları (slamplar), kaya düşmeleri, kaotik yapılar, klastik dayklar, sinsedimanter faylarve breşik kireçtaşlarıdır. Deformasyon mekanizması esas olarak tabakalarda eğim artışı, sıvılaşmave akışkanlaşma ile ilişkilidir. Çalışma alanının bölgesel tektoniği, sedimantolojik verileri vedeformasyon yapıları birlikte değerlendirildiğinde bu yapıların tektonik ve sismik (tektonik kökenlive depolanma ile eş yaşlı magmatik aktivitelerle ilişkili depremler) etkilerle (allojenik) oluştuğusonucuna varılmıştır.

Syn-sedimentary deformation structures in the Early Miocene lacustrine deposits, the basal limestone unit, Bigadiç basin (Balıkesir, Turkey)

In the Western Anatolian region, NE-SW, E-W directional basins were developed which were limited to the extension-related faults beginning in the late Oligocene to early Miocene. The fi llings of these basins consist of fl uvial – lacustrine deposits containing volcanic and volcaniclastic intercalations. These deposits include intensive local unconformities and soft sediment deformation structures. The fi lling of the Bigadiç Neogene Basin which is one of these basins, constitute base limestone unit, lower tuff unit, lower borate unit, upper tuff unit and upper borate unit. The base limestone unit composed of claystone, marl, limestone, dolomitic limestone facies was deposited in the deep lacustrine environment. The soft sediment deformation structures were defi ned in the base limestone unit, which outcroped in the south of Bigadiç. These are: slumps, rock falls, chaotic structures, clastic dykes, synsedimentary faults and breccia limestone. Deformation mechanisms are related essentially to the increase of slopes of layers, liquidization and fl uidization. In the study area; regional tectonics, sedimentological data, and deformation structures are evaluated together, it is concluded that these structures are formed by tectonic and seismic (earthquakes related to tectonic origin and syndepositional magmatic activities).

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