{"id":2706,"date":"2018-12-03T16:36:14","date_gmt":"2018-12-03T14:36:14","guid":{"rendered":"http:\/\/journal.phaselis.org\/uncategorized\/pha-0080"},"modified":"2018-12-03T16:59:28","modified_gmt":"2018-12-03T14:59:28","slug":"pha-0080","status":"publish","type":"post","link":"http:\/\/journal.phaselis.org\/en\/2018-en\/pha-0080","title":{"rendered":"Phaselis Antik Kenti K\u00fc\u00e7\u00fck Hamam\u2019\u0131 ve Latrina\u2019s\u0131nda Kullan\u0131lan Yap\u0131ta\u015flar\u0131 ve Bu Yap\u0131ta\u015flar\u0131n Bozu\u015fmalar\u0131"},"content":{"rendered":"

The Cut-Stones Used in the Small Bathhouse and the Latrina of Phaselis and the Alteration of These Stones<\/em><\/strong><\/p>\n

Ferda \u00d6NER<\/strong><\/p>\n

<\/div>\n

PHASELIS<\/em> IV (2018) 351-360<\/strong>
\nDOI<\/strong>: 10.18367\/Pha.18021<\/a>
\nReceived Date<\/strong>: 05.10.2018 \u00a0 | Acceptance Date<\/strong>: 21.11.2018
\nOnline Publication Date<\/strong>: 03.12.2018
\nCopyright \u00a9 PHASELIS Disiplinleraras\u0131 Akdeniz Ara\u015ft\u0131rmalar\u0131 Dergisi, 2018<\/p>\n

<\/div><\/div>\n
\n\t
\n\t\t\n

\"pdf\"\u00a0 Get PDF<\/strong><\/a><\/p>\n

\"references\"\u00a0<\/strong> View PDF<\/strong><\/a><\/p>\n

\"info\"<\/a>\u00a0 References<\/a><\/b><\/p>\n\n\t\t

<\/div>\n\t<\/div>\n<\/div>\n<\/div>
<\/div>\n

\u00d6z:<\/strong> Phaselis antik kenti Antalya\u2019n\u0131n g\u00fcneybat\u0131s\u0131nda Kemer ile Tekirova aras\u0131nda deniz k\u0131y\u0131s\u0131nda yer almaktad\u0131r. Kentin tarihinin M\u00d6 691 y\u0131llar\u0131na kadar gitti\u011fi s\u00f6ylenmektedir. Kentin jeolojik yap\u0131s\u0131nda, \u00dcst Kretase okyanus taban\u0131 magmatik kaya\u00e7lardan en son jeolojik d\u00f6nemde (Kuvaterner) olu\u015fmu\u015f traverten \u2013 traverten bre\u015fi (Fanglomera) birimlerine kadar de\u011fi\u015fen birimler g\u00f6zlenmektedir. Antik kentin ilksel ana yap\u0131 malzemesi (kesilmi\u015f, boyutland\u0131r\u0131lm\u0131\u015f bloklar) traverten bre\u015fleridir. Jura ya\u015fl\u0131 kire\u00e7ta\u015flar\u0131 (Tekeda\u011f\u0131 formasyonu kire\u00e7ta\u015flar\u0131) neotektonik d\u00f6nemde (Plio-Kuvaterner) y\u00fckselmi\u015f ve bunlar\u0131n \u00f6n\u00fcne d\u00fc\u015fen kaya\u00e7 par\u00e7alar\u0131, faylardan gelen karbonatl\u0131 sularla ta\u015fla\u015farak traverten bre\u015flerini (Fanglomera) olu\u015ftur\u00admu\u015ftur. Ayr\u0131ca antik kentin yerle\u015fim alan\u0131nda kalkarenitler ve gabrolar da g\u00f6r\u00fclmektedir. Phaselis antik kentinde ilksel olarak \u00e7evredeki kaya\u00e7lar (traverten bre\u015fleri, travertenler, kalkarenitler, serpantinler ve gabrolar), sonraki d\u00f6nemlerde ise d\u0131\u015far\u0131dan getirilmi\u015f mermerler, limra ve limra bre\u015fleri de kullan\u0131lm\u0131\u015ft\u0131r. Traverten bre\u015fleri ve di\u011fer yap\u0131 malzemeleri tarih boyunca de\u011fi\u015fik bozu\u015fmalara maruz kalm\u0131\u015ft\u0131r. Traverten bre\u015flerindeki bozu\u015fmalar, \u015fehrin ana yap\u0131 unsuru oldu\u011fundan \u00f6nemlidir. Traverten bre\u015flerinin bozu\u015f\u00admas\u0131ndaki ana unsur bre\u015flerin \u00e7imentosu olan malzeme ile ilgilidir. \u00c7imento tamamen karbonattan olu-\u015fur\u00adsa bloklar olduk\u00e7a dayan\u0131kl\u0131 olur, fakat bu b\u00f6lgede \u00e7imentoya kar\u0131\u015fan kil malzemesi hava \u015fartlar\u0131ndan et\u00adkilenerek bozu\u015fmalara neden olmu\u015ftur. \u0130leride restorasyon yap\u0131lmas\u0131 d\u00fc\u015f\u00fcn\u00fcl\u00add\u00fc\u00ad\u011f\u00fcnde, \u00e7evreden \u00fcre\u00adtilecek traverten bloklar\u0131n\u0131n \u00e7imentosuna bu anlamda \u00f6zellikle dikkat etmek gerekecektir.<\/p>\n

Anahtar S\u00f6zc\u00fckler:\u00a0<\/strong>Phaselis, Yap\u0131ta\u015flar\u0131, Bre\u015f, Limra, Mermer, Bozu\u015fma<\/p>\n

Top<\/a><\/div>\n

Abstract:\u00a0<\/strong>The ancient city of Phaselis lies on the seafront between Kemer and Tekirova, southwest of Antalya. It is said that the city\u2019s history dates back to 691 B.C. Geological feature of the city is formed ranging from the Upper Cretaceous magmatic rocks to in the last geological period (Quaternary) to the travertine – travertine breccia (Fanglomera) units. The primary main building material of the ancient city is the travertine breccias. The Jurassic limestones (Tekeda\u011f\u0131 formation limestones) have been elevated during the neotectonic period and Plio-Quaternary rocks, which were petrified with carbonated waters from the faults, and the travertine breccias (Fanglomera) were formed. Also calcarenites and gabbros are observed in the settlement area of the ancient city. In the ancient city of Phaselis, the surrounding rocks (travertine breccias, travertines, calcarenites, serpentines and gabbros) were firstly used, in later periods marbles, limestone and limra breccia were also used. Travertine breccias and other building materials have been subject to various alteration throughout the history. Alterations in travertine breccias are important because they are the main building element of the city. The main factor in the degradation of the travertine breccias is related to the cement material of the breccias. If the cement is completely carbonated, the blocks are highly resistant. However, the clay material added to the cement is affected by the weather conditions. Considering the future restoration, particular attention will be paid to the cement of the travertine blocks to be produced from the environment.<\/p>\n

Keywords:\u00a0<\/strong>Phaselis, Cut-Stones, Breccia, Limra, Marble, Alteration<\/p>\n

<\/div>\n

<\/a>