STRATIGRAPHY OF THE REGİON ERBAA (TOKAT)

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dc.contributor.authorToprak, Özlem
dc.contributor.authorAkyazı, Mehmet
dc.date.accessioned2025-01-21T14:28:51Z
dc.date.available2025-01-21T14:28:51Z
dc.date.issued2017
dc.description.abstractThe 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.
dc.identifier.dergipark350831
dc.identifier.doi10.29137/umagd.350831
dc.identifier.issn1308-5514
dc.identifier.issue3-136
dc.identifier.startpage146
dc.identifier.urihttps://dergipark.org.tr/tr/download/article-file/403394
dc.identifier.urihttps://dergipark.org.tr/tr/pub/umagd/issue/33339/350831
dc.identifier.urihttps://doi.org/10.29137/umagd.350831
dc.identifier.urihttps://hdl.handle.net/20.500.12587/20371
dc.identifier.volume9
dc.language.isoen
dc.publisherKırıkkale Üniversitesi
dc.relation.ispartofUluslararası Mühendislik Araştırma ve Geliştirme Dergisi
dc.relation.publicationcategoryMakale - Ulusal Hakemli Dergi
dc.rightsinfo:eu-repo/semantics/openAccess
dc.snmzKA_20241229
dc.subjectErbaa
dc.subjectGeneral Geology
dc.subjectStratigraphy
dc.titleSTRATIGRAPHY OF THE REGİON ERBAA (TOKAT)
dc.typeArticle

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