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Статті в журналах з теми "Olarian Deformation"
Yeşil, Serkan. "Konya İli Ereğli İlçesi Domates Ekim Alanlarında Domateste Yaygın Olarak Bulunan Üç Virüsün Serolojik Tespiti." Turkish Journal of Agriculture - Food Science and Technology 10, sp1 (December 30, 2022): 2795–800. http://dx.doi.org/10.24925/turjaf.v10isp1.2795-2800.5746.
Повний текст джерелаGÜNERİ, Esra, and Yeliz YUKSELEN AKSOY. "Investigation of Volumetric Deformation and Shear Strength Behavior of Sand-Bentonite Mixtures under High Temperature in the Presence of Perlite Additive." Deu Muhendislik Fakultesi Fen ve Muhendislik 24, no. 72 (September 19, 2022): 717–23. http://dx.doi.org/10.21205/deufmd.2022247203.
Повний текст джерелаDemirsar Arlı, Belgin. "İznik Çini Fırınları Kazı Buluntularından Çini Örneklerin Değerlendirilmesi / Evaluation of Iznik Tiles Examples from Iznik Tile Excavation." Journal of History Culture and Art Research 7, no. 1 (March 31, 2018): 578. http://dx.doi.org/10.7596/taksad.v7i1.1450.
Повний текст джерелаZhumabay Yesbalayeva, Roza. "Müasir qazax nəsrində milli idrakın etnodeformasiyası". SCIENTIFIC WORK 82, № 9 (17 вересня 2022): 27–34. http://dx.doi.org/10.36719/2663-4619/82/27-34.
Повний текст джерелаKocalan, Mustafa, and Tansel Türkdoğan. "Çağdaş Sanatta Bir Yanılsama Tekniği: ‘Anamorfoz’ ve Felice Varini / An Illusion Technique in Contemporary Art: ‘Anamorphosis’ and Felice Varini." Journal of History Culture and Art Research 7, no. 1 (March 31, 2018): 527. http://dx.doi.org/10.7596/taksad.v7i1.1033.
Повний текст джерелаDENİZ, Şadiye, and Elif KORAP ÖZEL. "Google Journalism: SEO News as a ‘Necessary Evil’ in the Digital Age and the Deformation of News for the Sake of ‘Clicks’." Connectist: Istanbul University Journal of Communication Sciences, December 28, 2018, 77–112. http://dx.doi.org/10.26650/connectist2018-0007.
Повний текст джерелаДисертації з теми "Olarian Deformation"
Taylor, A. D. "Structural mapping adjacent to the “Woman-in-White” amphibolite in the Olary Domain, South Australia." Thesis, 1999. http://hdl.handle.net/2440/119337.
Повний текст джерелаA structural study of Palaeoproterozoic Willyama Supergroup rocks to the southeast of Old Boolcoomata approximately 20 kilometres north of Olary, South Australia, discloses a complex history of deformation. This includes an axial planar S1 schistosity and several intersecting locally developed subsequent planar fabrics. The main findings support previous unpublished company studies. Structural maps were produced at various scales in areas surrounding the ‘Woman-in-White’ amphibolite and all available observations were used to form a chronology of events and tectonic model for the geometric and kinematic evolution of the area. In a domain east of the 'Woman-in-White' amphibolite the S1 is parallel to the axial plane of a major isoclinal synform closing to the east. S2 is axial planar to tight to open class 2 and class 1c F2 folds that trend generally north to northeast. Regionally, and particularly in the vicinity of the 'Woman-in-White' amphibolite, a third deformation is very intensely developed generating two fabrics. The S3 schistosity is the axial planar fabric to tight to isoclinal F3 folds trending consistently east-west. The S3 fabric is also expressed as a crenulation of the S1 regional schistosity. These pre-Adelaidean structural elements are recognised as comprising the Olarian Deformation. Fold interference is present on all scales. Olarian deformation events two and three have given the flat lying western limb of the principal F1 synform a luniform, dome and basin morphology. Type 2 and type 3 interference patterns are the most common in the area mapped. The occurrence of the two interference patterns is due to the variable angle between OD2 and OD3 compressions, which is commonly approximately 40 in the west-southwest part of the mapped area. This work conforms closely in complexity to previous regional studies and has been supplemented by other new investigations of an important northeast-southwest trending shear zone corresponding to OD3, lying further to the north, and a geochemical investigation of the 'Woman-in-White' amphibolite indicating its probable mantle origin and possible emplacement before all deformations occurred.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1999
Brotodewo, A. "Constraints on Mesoproterozoic magmatism and deformation in the southern Gawler Craton, South Australia: magmatism and deformation in Yorke Peninsula." Thesis, 2016. http://hdl.handle.net/2440/120548.
Повний текст джерелаThe ca. 1600–1580 Ma time slice is recognised as a significant period of magmatism and deformation throughout eastern Proterozoic Australia. Within the northern Yorke Peninsula, this period was associated with the emplacement of multiple phases of the Tickera Granite; an intensely foliated orange granite, a white leucogranite and a red granite. These granites belong to the broader Hiltaba Suite that was emplaced at shallow crustal levels, throughout the Gawler Craton. Geochemical and isotopic analysis suggests these granite phases were derived from a heterogeneous source region. The orange and red granites were derived from the Donington Suite and/or the Wallaroo Group metasediments with slight contamination from an Archean basement. The white leucogranite is sourced from a similar but slightly more mafic/lower crustal source. Phases of the Tickera Granite were emplaced synchronously with deformation that resulted in development of a prominent northeast trending structural grain throughout the Yorke Peninsula region. This fabric is a composite of two fold generations; early isoclinal folds that were refolded by later open upright folds. Isoclinal folding may have occurred during the ca. 1730–1690 Ma Kimban Orogeny, or just prior to emplacement of the Tickera Granite at ca. 1597–1577 Ma. The upright fold generation was contemporaneous with the emplacement of the Tickera Granite. The Yorke Peninsula shares a common geological history with the Curnamona Province, which was deformed during the ca. 1600–1585 Ma Olarian Orogeny, and resulted in development of early isoclinal (recumbent) folds overprinted by an upright fold generation, a dominant northeast–trending structural grain and spatially and temporally related intrusions. This suggests an apparent correlation with the geological history of the Curnamona Province, and that the Olarian Orogeny may have also affected the southeastern Gawler Craton. Constraint on the timing of the earlier isoclinal fold generation in the Yorke Peninsula will allow further understanding of the similarities between the two regions.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2016