Research paperThe Kizilkaya ignimbrite — an unusual low-aspect-ratio ignimbrite from Cappadocia, central Turkey
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Cited by (52)
Diatom community and palaeoenvironmental properties of Karacaören diatomite deposits (Nevşehir, Central Anatolia, Turkey)
2017, Journal of African Earth SciencesCitation Excerpt :The study area was located in the Kracaören region of Ürgüp town near Nevşehir in central Anatolien (Fig. 1). The mineralogy, petrography, geochemistry of the volcanic and pyroclastic rocks, volcanism and the tectonics of the Cappadocia Volcanic Province (CVP) have been studied by many researchers (e.g., Beekman, 1963, 1966; Sassano, 1964; Pasquaré, 1968; Innocenti et al., 1975; Özkuzey and Önemli, 1977; Batum, 1975, 1978; Yıldırım and Özgür, 1981; Ekingen, 1982; Ercan and Yıldırım, 1988; Pasquaré et al., 1988; Ercan et al., 1989, 1990; Schumacher et al., 1990, 1992; Aydar, 1992; Temel, 1992; Göncüoğlu and Toprak, 1992; Aydar et al., 1994; Duritt et al., 1995; Bigazzi et al., 1993, 1997; Le Pennec et al., 1994, 2005; Schumacher and Mues-Schumacher, 1996; Toprak, 1994, 1996, 1998; Schumacher and Mues-Schumacher, 1997; Aydar and Gourgaud, 1998; Dhont et al., 1998; Froger et al., 1998; Kürkçüoğlu et al., 1998; Koçyiğit and Beyhan, 1998; Temel et al., 1998a,b; Gevrek and Kazancı, 2000; Dirik, 2001; Dönmez et al., 2003; Viereck-Göette et al., 2010; Göz et al., 2014). Further, the volcano-sedimentary rocks, associated palaeosols and caliches of this region and its vicinity have been studied by many researchers (Viereck-Göette and Gürel, 2003; Le Pennec et al., 2005; Kadir et al., 2006; Gürel and Kadir, 2006, 2008, 2010; Gürel et al., 2007, 2008).
Complex remanent magnetization in the Kızılkaya ignimbrite (central Anatolia): Implication for paleomagnetic directions
2017, Journal of Volcanology and Geothermal ResearchCitation Excerpt :The low aspect-ratio Kızılkaya ignimbrite defines flat structural surfaces on the plateau and usually occurs as a 10–30 m-thick (locally > 80 m) red-tinted and columnar-jointed unit (Pasquarè et al., 1988). In the eastern part of the Plateau, the > 180 km3 ignimbrite is underlain by a plinian pumice fall deposit (Le Pennec et al., 1994; Schumacher and Mues-Schumacher, 1996). The ignimbrite is commonly welded and sintered, and the degree of welding varies both vertically and laterally, with eutaxitic textures observed in some valley-ponded facies (e.g. Ihlara, Soğanlı, Fig. 1).
Vertical variation in the deuteric oxidation of titanomagnetites in an ignimbrite deposit: Kizilkaya Ignimbrite (Cappadocia, Turkey)
2015, Journal of Volcanology and Geothermal ResearchCitation Excerpt :This suggests an effect of the decreased effective grain sizes in the oxidized titanomagnetites on Js, especially for the uppermost zones of Kızılkaya ignimbrite where Fe-rich titanomagnetite hosts are surrounded by Ti-rich exsolution lamellae (Fig. 6). The exact location of the source area of the Kızılkaya ignimbrite is a matter of debate and several areas have been proposed by Pasquare et al. (1988), Le Pennec et al. (1994, 1998), Schumacher and MuesSchumacher (1996), Le Pennec (2000) and Agrò et al. (2015) using various methods. Among these, the studies that rely on magnetic data (Le Pennec et al., 1994, 1998; Le Pennec, 2000; Agrò et al., 2015) proposed the SW of the town of Derinkuyu as the probable source area of the Kızılkaya ignimbrite.