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Artículos, Encontrados 3 registros
Artículos Encontrados 3 registros  
1.
20 p, 4.8 MB Metamorphic-hosted pyrophyllite and dickite occurrences from the hydrous Al-silicate deposits of the Malatya-Pütürge region, central eastern Anatolia, Turkey / Bozkaya, Ömer (Cumhuriyet University. Department of Geological Engineering) ; Yalçin, Hüseyin (Cumhuriyet University. Department of Geological Engineering) ; Başibüyük, Zeynel (Cumhuriyet University. Department of Geological Engineering) ; Bozkaya, Gülcan (Cumhuriyet University. Department of Geological Engineering)
Hydrous Al-silicate deposits are found to the south of Pütürge in Malatya city, Turkey. The surrounding rocks consist of mylonitic granitic gneiss overlain by muscovite gneiss with kyanite-bearing metabasic schist lenses on top which are cut by silica veins containing prismatic tourmaline and specularite. [...]
2007 - 10.1346/CCMN.2007.0550409
Clays and Clay Minerals, Vol. 55, Núm. 4 (2007) , p. 423-442  
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2.
23 p, 3.4 MB Geochemistry of mixed-layer illite-smectites from an extensional basin, Antalya Unit, Southwestern Turkey / Bozkaya, Ömer (Cumhuriyet University. Department of Geological Engineering) ; Yalçin, Hüseyin (Cumhuriyet University. Department of Geological Engineering)
The Antalya Unit, one of the allochthonous units of the Tauride belt, is of critical, regional tectonic importance because of the presence of rifting remnants related to the break-up of the northern margin of Gondwana during Triassic time. [...]
2010 - 10.1346/CCMN.2010.0580505
Clays and Clay Minerals, Vol. 58, Núm. 5 (2010) , p. 644-666  
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3.
18 p, 3.4 MB Mineralogy and geochemistry of Paleocene ultramafic- and sedimentary-hosted talc deposits in the southern part of the Sivas Basin, Turkey / Yalçin, Hüseyin (Cumhuriyet University. Department of Geological Engineering) ; Bozkaya, Ömer (Cumhuriyet University. Department of Geological Engineering)
Talc deposits, located mainly in three areas of north-central Turkey, are present in the ophiolitic series of the Cretaceous and in siliciclastic rocks of the Paleocene. Talc deposits related to ophiolites are between tectonite and cumulate occuring as beds and/or lenses and 0. [...]
2006 - 10.1346/CCMN.2006.0540305
Clays and Clay Minerals, Vol. 54, Núm. 3 (2006) , p. 333-350  
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3 Yalçin, Hüseyin
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