STRATIGRAPHY OF THE REGİON ERBAA (TOKAT)
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Tarih
2017
Yazarlar
Dergi Başlığı
Dergi ISSN
Cilt Başlığı
Yayıncı
Kırıkkale Üniversitesi
Erişim Hakkı
info:eu-repo/semantics/openAccess
Özet
The Permo-Triassicbasement rocks form the basis of the study area, which is located on the NorthAnatolian Fault and immediate vicinity of the Erbaa District on the north. Theprimary covering units overlying the basement rocks consist of a thick deposit,deposited in the depression in front of the Eurasian continent during theLiassic-Upper Eocene time interval. The first cover units, unconformably overlyingthe basic rocks, are overlaid by conglomerate, sandstone, mudstone, marl andoolitic limestones and Lower-Middle Jurassic rocks composed of volcano-clasticrocks, Upper Jurassic-Lower Cretaceous aged neritic and pelagic clayeylimestones, the Santonian-Campanian aged sedimentary rocks in the pyroclasticcharacter accompanied by the volcanic-volcanosedimentary rocks formed by thesubmarine volcanic activity in the Upper Cenomanian, Maestrichtian-Paleocenesandy limestones, Lower-Middle Eocene conglomerate, volcanogenic sandstone,sandy limestone and nummulites limestones and Upper Eocene basalt, pillowlavas, andesite, tuff, tuffite, aglomera, sandstone and siltstone intercalationunconformably. Secondary cover units, composed of loosely adhered conglomeratesand sandstones that collapse during terrestrial atmospheric conditions indepressions formed along the North Anatolian Fault zone, are covered by theQuaternary aged alluvium, slope rubble and deposit cones, which constitute theyoungest units of the study area.
Açıklama
Anahtar Kelimeler
Erbaa, General Geology, Stratigraphy
Kaynak
Uluslararası Mühendislik Araştırma ve Geliştirme Dergisi
WoS Q Değeri
Scopus Q Değeri
Cilt
9
Sayı
3-136