Investigating the geophysical characteristics of gypsum through GPR

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Özet

Gypsum crops out widely in the areas where the urbanization is intense in Sivas city center. In this study, in an appropriate selected area, geophysical characteristics and structure of gypsum have been investigated by applying geophysical methods of GPR (Ground Penetrating Radar). GPR measurements have been taken as 11 profiles with a Ramac GPR device by using 250 MHz shield-antenna. The distance between each profile has been taken as 2m and the length of each profile has been taken as 50m. All the area has been surveyed and ground radar sections have been obtained by GPR method. Gathering all the data, it has been found out that the areas with strong reflections (for the first 5m. depth) revealed in ground radar sections are not homogeneous massive gypsum bodies as presented in geological studies and contain different size and position fill material (clastic material). In addition, investigating such areas through GPR method has enabled to reveal the geophysical characteristics of the region as gypsum contains fractures-cracks, fillings and dissolution spaces.

RDL Kalıcı Bağlantı (PID)
https://rdlopen.rawdatalibrary.net/r/gumushane/15687Resmi atıflarda kullanılan kalıcı adres
DOI
https://doi.org/10.3997/2214-4609.201414189Yayıncı resmi DOI adresi
Tam Kayıt
AlanDeğerDil
dc.contributor.authorSari, M.S.
dc.contributor.authorBektaş, Ö.B.
dc.date.accessioned2026-10-22T10:24:23.173283494Z
dc.date.available2026-10-22T10:24:23.173283494Z
dc.date.issued2015
dc.description.abstractGypsum crops out widely in the areas where the urbanization is intense in Sivas city center. In this study, in an appropriate selected area, geophysical characteristics and structure of gypsum have been investigated by applying geophysical methods of GPR (Ground Penetrating Radar). GPR measurements have been taken as 11 profiles with a Ramac GPR device by using 250 MHz shield-antenna. The distance between each profile has been taken as 2m and the length of each profile has been taken as 50m. All the area has been surveyed and ground radar sections have been obtained by GPR method. Gathering all the data, it has been found out that the areas with strong reflections (for the first 5m. depth) revealed in ground radar sections are not homogeneous massive gypsum bodies as presented in geological studies and contain different size and position fill material (clastic material). In addition, investigating such areas through GPR method has enabled to reveal the geophysical characteristics of the region as gypsum contains fractures-cracks, fillings and dissolution spaces.
dc.identifier.doi10.3997/2214-4609.201414189
dc.identifier.isbn978-946282166-8
dc.identifier.scopus2-s2.0-85086951803
dc.identifier.urihttps://rdlopen.rawdatalibrary.net/r/gumushane/15687
dc.language.isoen
dc.publisherEuropean Association of Geoscientists and Engineers, EAGE
dc.relation.conference8th Congress of the Balkan Geophysical Society, BGS 2015
dc.relation.ispartof8th Congress of the Balkan Geophysical Society, BGS 2015
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subject.otherAntennas
dc.subject.otherGeological surveys
dc.subject.otherGeophysics
dc.subject.otherGround penetrating radar systems
dc.subject.otherGypsum
dc.subject.otherCity centers
dc.subject.otherClastic materials
dc.subject.otherDifferent sizes
dc.subject.otherFill materials
dc.subject.otherGeophysical methods
dc.subject.otherGPR (ground penetrating radar)
dc.subject.otherGround radars
dc.subject.otherGeophysical prospecting
dc.titleInvestigating the geophysical characteristics of gypsum through GPR
dc.typeConference Object
dspace.entity.typePublication
rdl.citation.openalex0
rdl.citation.scopus0
rdl.conference.date5 October 2015 through 8 October 2015
rdl.conference.placeChania
rdl.oa.statusclosed
rdl.source.indexSCOPUS