The stratigraphy of alibonca formation and its relationship with Malatya volcanites in the Southwestern Arapgir (Malatya, Turkey)

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dc.contributor.authorSönmez, Mustafa
dc.contributor.authorAksoy, Ercan
dc.date.accessioned2024-11-07T10:39:26Z
dc.date.available2024-11-07T10:39:26Z
dc.date.issued2017
dc.departmentNiğde Ömer Halisdemir Üniversitesi
dc.description17th International Multidisciplinary Scientific Geoconference, SGEM 2017 -- 29 June 2017 through 5 July 2017 -- Albena -- 130787
dc.description.abstractThe main purpose of this article is to reveal the age of Alibonca Formation and Malatya Volcanites, their formational environment and the contact relationship between these two units. The units that cropped out in the study area are Keban Metamorphites (Permo-Trias), Alibonca Formation (Lower Miocene), Malatya Volcanites (Lower-Upper Miocene), Meteristepe formation (Lower Pleistocene), Yoncalı formation (Upper Pleistocene), talus and alluviums (Holocene-current). Alibonca Formation is composed of medium-thick bedded limestone that is the product of carbonate platform. The unit also comprises mudstone containing clay-rich limestone, marl and coal strata that deposited on the lagoons connected to the Miocene Sea that the limestone deposited on. The unit unconformably overlying different bases was formed in the Aquitanian- Burdigalian period when the region fell under transgression effect. The Lower-Upper Miocene aged Malatya Volcanites are composed of agglomerate, tuff lapilli and lava flows with dacitic, andesitic and basaltic composition crossing them. There is a transitional and concordant contact between Alibonca Formation and Malatya Volcanites. The volcanism leading to the formation of Malatya Volcanites began in the last phases of the sedimentation of Alibonca Formation that deposited on a transgressive sea in the Lower Miocene. © SGEM2017. All Rights Reserved.
dc.description.sponsorshipFırat University
dc.identifier.doi10.5593/sgem2017/11/S01.085
dc.identifier.endpage678
dc.identifier.isbn978-619740826-3
dc.identifier.issn1314-2704
dc.identifier.issue11
dc.identifier.scopus2-s2.0-85032465420
dc.identifier.scopusqualityN/A
dc.identifier.startpage671
dc.identifier.urihttps://doi.org/10.5593/sgem2017/11/S01.085
dc.identifier.urihttps://hdl.handle.net/11480/10959
dc.identifier.volume17
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherInternational Multidisciplinary Scientific Geoconference
dc.relation.ispartofInternational Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.snmzKA_20241106
dc.subjectAlibonca formation
dc.subjectMalatya
dc.subjectMalatya volkanites
dc.subjectStratigraphy
dc.titleThe stratigraphy of alibonca formation and its relationship with Malatya volcanites in the Southwestern Arapgir (Malatya, Turkey)
dc.typeConference Object

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