Integration of satellite data processing with seismic sections for tectonic interpretation and modeling for the breaks and omissions of continuous stratigraphic units

A tétel rövid nézete
dc.contributor.authorThannoun, Rayan Gh.
dc.contributor.authorFanoosh, Salim A.
dc.contributor.authorAdeeb, Hadeer Gh. M.
dc.contributor.statusnemhu_HU
dc.date.accessioned2021-04-01T06:45:06Z
dc.date.available2021-04-01T06:45:06Z
dc.date.issued2021-03-20
dc.description.abstractSatellite thematic maps in geological field studies are an important tool for the delineation, interpretation, representation, and visualization of geological processes, while the development of seismic sections offers an increasingly detailed analysis of subsurface geology and inferring and understanding the subsurface structure of the earth. This combination promoted a fast-growing research in the fields of morphotectonics and neotectonics. The area under investigation is one of the most significant Iraqi places which includes several oil fields. The study area is located in northern Iraq and administratively follows Kirkuk governorate. Landscapes in this area are characterized by asymmetrical, cylindrical and extended folds. Kirkuk, Bai-Hasan and Qarachuq Anticlines reflect these structural elements and their fold axis trends towards northwest-southeast within the Zagros folded zone. The main objective of this study is to use the visual and digital interpretation of Landsat image to discriminate the sudden breaks and omissions of rock beds in the study area. Therefore, a morphotectonic map was created, the accurate location of the sudden breaks was provided and the zones affected by tectonic deformation, which left its imprint on the successive lithological units were detected. Seismic data were used to assess the tectonic impact on subsurface formations and their reflections on exposure rocks. The seismic lines were selected based on the locations of the identified sudden breaks as interpreted from satellite images. The hypothesis derived from this study is that the sudden breaks in the study area were triggered by a series of faults. In addition, the region was affected by the vertical stresses resulting from these faults and morphological aspects of the region were determined by the temporal variations of the above stresses.hu_HU
dc.identifier.doi10.1556/1848.2020.00123hu_HU
dc.identifier.issn2062-0810
dc.identifier.issue1hu_HU
dc.identifier.jtitleInternational Review of Applied Sciences and Engineering
dc.identifier.urihttp://hdl.handle.net/2437/305048
dc.identifier.urlhttps://akjournals.com/view/journals/1848/12/1/article-p34.xmlhu_HU
dc.identifier.volume12hu_HU
dc.language.isoenhu_HU
dc.publisherAkadémiai Kiadóhu_HU
dc.subjectremote sensinghu_HU
dc.subjectmorphotectonicshu_HU
dc.subjectseismic sectionshu_HU
dc.subjectstructural breakshu_HU
dc.subjectkirkuk anticlinehu_HU
dc.titleIntegration of satellite data processing with seismic sections for tectonic interpretation and modeling for the breaks and omissions of continuous stratigraphic unitshu_HU
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International Review of Applied Sciences and Engineering