Diagenesis and very low-grade metamorphism of the Antalya unit: mineralogical evidence of Triassic rifting, Alanya-Gazipaşa, central Taurus belt, Turkey

Bozkaya, Ömer; Yalçın, Hüseyin

doi:10.1016/j.jseaes.2004.02.001

Cited by 23 publications

(18 citation statements)

References 32 publications

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“…GDAO'nun (Bozkaya ve Yalçın, 2013;Bozkaya ve diğ., 2009Bozkaya ve diğ., , 2011Tetiker ve diğ., 2015) ve özellikle Torid Kuşağı'nın (Çelik ve diğ.. 1991;Bozkaya ve Yalçın 2000, 2004a, 2004b, 2005, 2010, 2013Bozkaya ve diğ., 2002) PaleozoyikMesozoyik yaşlı birimlerinde diyajenetik/ metamorfik tarihçenin aydınlatıldığı birçok ayrıntılı çalışma gerçekleştirilmiştir. Bunları tamamlayıcı nitelikte olmak üzere, bu çalışmada GDAO'nun Uludere-Uzungeçit (Şırnak) bölgesinde yüzeyleyen Çığlı Grubu'na ait karbonat ve pelitik kayaçların mineralojik özellikleri ortaya konularak, Diyarbakır-Hazro yöresindeki eşdeğerleri ile karşılaştırılması ve sonuçta yanal olarak istiflere ait havzaların provenans, mineral birliktelikleri, diyajenetik/metamorfik evrimlerinin belirlenmesi amaçlanmıştır.…”

Section: şEkilunclassified

Uludere-Uzungeçit (Şırnak) yöresinde (Güneydoğu Anadolu Otoktonu Doğu Bölümü) Alt Triyas Yaşlı Çığlı Grubu Kayaçlarının Diyajenez/Metamorfizma Tarihçesi

Tetiker¹,

Yalçın²,

Bozkaya³

2016

Türkiye Jeoloji Bülteni / Geological Bulletin of Turkey

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Section: şEkilunclassified

Uludere-Uzungeçit (Şırnak) yöresinde (Güneydoğu Anadolu Otoktonu Doğu Bölümü) Alt Triyas Yaşlı Çığlı Grubu Kayaçlarının Diyajenez/Metamorfizma Tarihçesi

Tetiker¹,

Yalçın²,

Bozkaya³

2016

Türkiye Jeoloji Bülteni / Geological Bulletin of Turkey

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“…3). Higher diagenetic-metamorphic features of this formation were assumed as the result of higher heat Xow during the Triassic rifting (Bozkaya and Yalçín, 2005).…”

Section: Geological Backgroundmentioning

confidence: 99%

“…Microscopic investigations showed that the grades of diagenesis and metamorphism of this formation are higher than in the older Çakmak and Bíçkící formations. Higher diagenetic-metamorphic features of Çamlíca Formation are assumed to be the result of high heat Xow during Triassic rifting (Bozkaya and Yalçín, 2005).…”

Section: Geological Backgroundmentioning

confidence: 99%

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Lead and sulfur isotopic studies of the barite–galena deposits in the Karalar area (Gazipaşa–Antalya), Southern Turkey

Gökçe

Bozkaya

2007

Journal of Asian Earth Sciences

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“…The relationship between the cumulative frequency and b 0 values in Göksun, Afşin and Ekinözü regions (Demirtaş, Gazipaşa b 0 values:Bozkaya and Yalçın, 2005; Wales: …”

mentioning

confidence: 99%

Göksun, Afşi̇n Ve Eki̇nözü (Kahramanmaraş) Bölgesi̇nde Yüzeylenen Metamorfi̇k Masi̇fleri̇n Mi̇neraloji̇k Karakteri̇sti̇kleri̇

Hozatlıoğlu¹,

Bozkaya²,

Yalçın³

et al. 2019

Bulletin of the Mineral Research and Exploration

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This study aims to investigate and correlate the mineralogical-petrographic characteristics of Metamorphites in Göksun, Afşin and Ekinözü in the Southeast Anatolian Metamorphic Massifs. In this context, the optical microscopy and XRD investigations were performed on several samples. Göksun Metamorphites are constituted by phyllite, calcphyllite, marble and they contain mainly calcite, dolomite, quartz, feldspar, phyllosilicate. KI and b-cell dimension data reflect high anchizone-epizone and medium pressure conditions. Afşin Metamorphites are represented by phyllite, calcphyllite, calcschist, micaschist, amphiboleschist, marble. Phyllosilicates have consisted of illite/mica, IIb chlorite, mixed-layers, smectite. KI and b-cell dimension data correspond to the subgreenschist-greenschist facies conditions. Ekinözü Metamorphites are made of chloriteschist, amphiboleschist, micaschist, micagneiss in lower parts, while calcitic and/or dolomitic marbles are present in the upper parts. Mica is dioctahedral and trioctahedral, whereas chlorite tends to be trioctahedral. Based on mineral associations, Ekinözü Metamorphites belong to amphibolite facies in the lower parts, but the greenschist facies conditions at the upper parts. The coarse-grained biotite, muscovite and chlorite are accompanied by mixed-layers. According to mineral composition and degrees of metamorphism, Göksun and Afşin Metamorphites are similar to the Keban and Malatya Metamorphites; however, Ekinözü Metamorphites to Pütürge Metamorphites. The data show that metamorphics in the western extension of the Southeast Anatolian Metamorphic Massifs have different origin and/or lithologies according to the regions, increasing temperature-pressure conditions from Göksun to Ekinözü and have groups of rock with different geological evolutions.

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Diagenesis and very low-grade metamorphism of the Antalya unit: mineralogical evidence of Triassic rifting, Alanya-Gazipaşa, central Taurus belt, Turkey

Cited by 23 publications

References 32 publications

Uludere-Uzungeçit (Şırnak) yöresinde (Güneydoğu Anadolu Otoktonu Doğu Bölümü) Alt Triyas Yaşlı Çığlı Grubu Kayaçlarının Diyajenez/Metamorfizma Tarihçesi

Uludere-Uzungeçit (Şırnak) yöresinde (Güneydoğu Anadolu Otoktonu Doğu Bölümü) Alt Triyas Yaşlı Çığlı Grubu Kayaçlarının Diyajenez/Metamorfizma Tarihçesi

Lead and sulfur isotopic studies of the barite–galena deposits in the Karalar area (Gazipaşa–Antalya), Southern Turkey

Göksun, Afşi̇n Ve Eki̇nözü (Kahramanmaraş) Bölgesi̇nde Yüzeylenen Metamorfi̇k Masi̇fleri̇n Mi̇neraloji̇k Karakteri̇sti̇kleri̇

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