Jeoloji Münendisliği Dergisi
Jeoloji Mühendisliği Dergisi

Jeoloji Mühendisliği Dergisi

1985 EKİM
COVER
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COPYRİHT PAGE
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CONTENTS
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TO OUR READERS
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 Statistical method about the determination of differentiation and •crystallization phases of a magmatic intrusion and the application of this method on c& model
Atilla Aykol
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ABSTRACT: It is widely known that the emplacement of magmatio infernsfons iid not take plae© in a single phase `tel; that ötey rather intruded anil were emplaced within or next ta each other in different phases,» ît Is also an accepted view that maginatie intrusions ol granitic origin, because of their low density, analogous »alt domes, tend to intrude in a diapric form and manner, Tli© opinion that a granitic mass was a product of a single intrusion, widely lost support« Slnee there are intrusions unplaced in different phases within or next to each other then ît is also probable that they also differentiated and crystallized independently in different times. In this work, the above view is© being discussed and Kırklareli Demirköy granodioritic mass, which bad bmn studied in detail taken as a model for calculations and statistical application ami imterprotattons of differentiation andı eaystal&atioii ftukxses.

  • Magmatic İntrusion

  • Crystallization Phases

  • Granitic

  • Kırklareli Demirköy

  • AYKOL, A. 1979 ; Kırklareli, Demirköy Sokulumu`nun Fetroloji ve Jeokimyası. İTÜ Maden Fakültesi Doçentlik Tezi.

  • AYKOL, A. 1980 : Kırklareli, Demirköy Sokulumu tçinde Major Elementlerin Dağılımı ve Yerkimyasımn Pertografi ve Fetroloji ile Yakın İlişkisi. TMMOB Jeoloji. Müh., Odası Bülteni 2..

  • BOWEN, ~N.lt. lfiöO1 : Le problème des- granites., Ree, 2 Edit., inst., lithol.

  • BURRI, C. 1959 : Petrochemical Calculations Bîrkhouser Verlang Basle Switzerland.

  • BÜRKÜT, Y. 1966: Kuzeybatı Anadolu`da Yer alan, Plutonlann Mukayeseli Jenetik Etüdü. İTÜ Mar den Fakültesi Doktora, Tezi.

  • BÜRKÜT, Y. 1.966 : Istranca Kristalin Masifinin Petrojenezi. Madencilik Cilt IH, Sayı, 4, 1,65-180.

  • BÜRKÜT, Y. 1975 : Kuzeybatı Anadolu. Granitik Plutonian İçindeki Ti,. P, Zr, Mn, Vım tayini ve dağılımı. MTA. Derg. Sayı. 84.

  • CASSIC, R.M. 1954 ; Some usesof probability paper in. the analysis of size frequency -distributions. Aust, J. Marine and .Freshwater Research v. 3, 51,3-522

  • CRAVEN, C.A.U 1.954 :; Statistical estimation of the accuracy of assaying, Trans;, instil., Min. Metall, 63 Sept. 551»

  • JAMES, C.H. 1970 ; A rapid method for calculating the statistical, precision, of geochemical prospecting

  • LEPELTIER, 1950 : A simplified statistical treatment of geochemical data by graphical representation. E:con,. Geol,. V. 643l No: 5 pp. 538-550,.

  • NÏGGLÏ, 1923 : Gesteins und Mineralprovinzen I Berlin Borntrager1 .

  • NOGKOLDS, S.R. 1.954 : Average chemical composition, of some igneous rocks., Geol. Soc. America Bull. 65, pp. 1007-1082.

  • PLATEN, V.H, 1985 ; Kristallisation granitiseher Schmelzen, 8el.tr. Minerologie und Petrogorapnie, vol 11, pp. 334-381,

  • YILMAZ, Y.. 1979 : Granit. Magmasının Yerleşme sorunu, ÏJK (Özel Baskı).,

  • An example of manganese mineralisation in the Eastern Pontide : the Ocakh (Maçka-Trabzon) manganese prospect
    Mehmet Atasever Gedikoğlu Aydin Ali Van Işik Eyüboğlu Bülent Yalçinalp
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    ABSTRACT: OcaWi manganese ore deposits are placed In the volcanic and sedimentary formations of Upper Cretaceous age as the other manganèse occurrences in the Eastern Black Sea. Region, Voleanogenlc îıyirotherıııal lore solutions are placed In very siialtow depth, so the ©re body accordingly form tease like bodies and stockwosrk depositions, Because of the sliding- which is more or less at the same age with the deposition, the important part of the ore body Is in an alloehthonous massa Especlalyl braunite and bixybite iniaeraHasatioii are common. In these minera Üzation, SiO^, and P.CX contents a«r© no tic ably high and can b& considered as metallurgical ore type. The manganese ieposlte of the .Eastern Black Sea Region are enapfacecl in different levels xelafäv® to the sea floor. Accoordmg1 to canplaceıneııjfe level, deposition forma, mâıeıraloglcal and chemical `compositions of the ore bodies are different from each others. So three main &nb-types .are distinguished.

  • East Blacksea

  • mineralisation

  • Ocaklı(Maçka-Trabzon)

  • manganese prospect

  • Adamia, Sh, A., Lordkipanidaze, M.B., ve Zakariadze, G.S., 1977; Evolution of an Active: Continental Margin as Exemplified, by the Alpine History of the Caucosus. Tectonophysics, 40, p. 183-199.

  • Aslaner, M„, 1977; Türkiye. Bakır-Kurşun-ÇînkO` Yataklarının Jeolojik ve Bölgesel Sınıflamasıyla Plaka Tektoniği. Yönünden İncelenmesi. K.T.Ü,, Yer Bilimleri Fakültesi, Yayın No, 12, Trabzon,

  • Aslaner, M., Gedîkoğlu, A., ve Tülümen, E., 1982; Har- §it vadisi polimetalik .mineralizasyonlarmın ayrıntılı araştırılması^ TÜBİTAK Proje No: TBAG -390, (Yayınlanmamış).

  • Beus, A.A. 1978; Geochemistry of the Lithosphère, Mir Publishers

  • Bocalettî, M,, Manetti, P., and Peccarillo, A., 1074; Hypothesis on the Plate Tectonic Evolution of the Carpatho-Balkan Arcs. Earth and Planetary Science Letters, .23, p. 1.93-198,

  • Fleischer, MM and Richmond, W., 1943; The Manganese Okside Minerals: A preliminary report. Economie Geology;, No 4, p. 260-286.

  • Gedikoğlu, A., 1970; Etude Géologique de la Région de Gölköy (Province D`Ordu-Turquie), Thèse de Doctorat, Un, de Grenoble,

  • Gedikoğlu, .A..,, 19TO; Harşit Granit Karmaşığı ve Çevre Kayaçları (Giresun-Doğankent), KTÜ. Yer Bilimleri Fakülteis Doçentlik Tezi,, Trabzon, ( Yayınlanmamış ).

  • Gedikoğlu, A., Pelin, S. ve Özsayar, T., 1982; Gölköy (Ordu) Yöresinde bir Paleokaldera île Cevherleşmelerin Konumu Arasındaki İlişkiler, K,Ü. Yer Bilimleri Dergisi, Jeoloji, Cilt 2,. Sayı 1-2, S. 117-130, Trabzon...

  • Gedikoğlu, A..., Pelin, S,, and Özsayar, T., 1979; The Main, lines of the Eastern Pontids in Mesozoic era. Geooome-T Bildirisi, Abstracto, p. 68-69, Ankara

  • Gedikogrlu, A.} . ve Van, A,., 1983; Artvin yakın, yöresine ait Jeolojik Bulgular, 37 TÜK. .Bilimsel ve Teknik Kurultayı, Tebliği özetleri, s., 47-48, Ankara.

  • Koproviea, D., 1976;` Hopa-Arhavi Bölgesinin Jeolojisi, Yapısal özellikleri ile Sülfit ve Manganez Zuhurları (NEwTürkiye). MTA Dergisi,. Sayı 87, s,. 1-20, Ankara,,

  • Mitcelï, A.H.G., 1976; Tectonic Settings for Emplacement of Stibductionrelated Magmas and Associated. Mineral Deposits, in. Ctrong, D...F,.., Ed., Mefcallogeny and Plate Tectonics: Geol. Âssoc. Canada Spec, paper 14, p. 3-21.

  • MTA., 1965; Türkiye Manganez Yatakları, MTA,. Yayın No. 120, Ankara.

  • Müsaoğlu, A,, ve Akıncı, S.., 1.983; Grdu-Ulubey-Akoluk Manganez Cevherleşmesi Jeoloji Raporu, MTA, Maden Etild Dairesi,. Ar. Rap. No. 1875 (Yayınlanmamış)..

  • Nikko Bixp.. and Development öo,, 1977; Report on Geological Survey of Trabzon Area, Northestern Turkey (Consolidated. Report).

  • Nuffield, E.W., 1967; In Powder Diffraction File Joint Committee on. Powder Diffraction Standarte, Inorganic Vol.,. No PD15-105RB" Phildardelphia

  • Özbegîkçf, A..t Kırcı, If, Ye `Uysal,, 11, 1981; OrduGiresun-Gümüşhane Yöresindeki Manganez Zuhurlarına ait Proşpeksiyon raporu, MTA,, ifaden. Etüd Dairesi, Ar, Rap,,, No,. 1732 (Yayınlanmamış).

  • Özsayar, T.,,, Pelin, E,, ve Gedikoğlu, A,,, 1981; Doğu Pontidler`de Kretase, KTÜ. Yer Bilimleri Dergisi, Jeoloji,, Cilt 1, Sayı 2, s. 6&-114, Trabzon.

  • Öztunalı, Ö,3 , 1973; Maden Yatakları, Oluşumları ve Değerlendirilmesi, îs-tanbul.

  • Plimer, I.R., 1981; Water Depth-a Critical Factor for Exhalative Ore Deposits, BMH Journal of Australian Geology and Geophysics, Vol. 6,, p.293» 300.

  • Raindohr, P., 1080; The Ore Minerals and. Their Integrowths. Vol. 2,. Pergamon press.,

  • Roy, S..,, 1976; Ancient Mangenese Deposits in Wolf, K.H., Handbook of Strata-Bound and. Stratiform Ore Deposits Vol, 7, p. 395-477

  • Sillitoe, RJBL, 19-81; Ore Deposits in. Cordilleran and Island-arc setteings, In Dickinson, W..R, and Payne,. W.D.Ed,,, Relations of Tectonics to Ore Deposits In the Southern Cordillera, Arizonageological soc, digest,. Vol. JXIV, p. 49-69

  • Staaten,. RVL, 1972; Ore Petrology, Mc-Graw-Hili Book Com.pa.ny.

  • Şengör A...M...C.., 19S0; Türkiye`nin Neotektoniginin Esasları TJK.. Yayım,, Ankara.

  • Şengör A.M.C., Yılmaz, Y., 1983; Türkiye`de Tetis`in `Evrimi :: `Levha Tektoniği Açısından bir yaklaşım.. TJK, Yerbilimleri Özel Dizisi, No. 1,, An. kara

  • Tokel, S. r 1977; Doğu Karadeniz Bölgesinde `Eosen. Yaşlı Kalkalkalen Andezitler ve Jeoktektonizma, Cilt 20, sayı, 1, s. 49-54, Ankara

  • Tokel, S», 1981; Plaka Tektoniğinde Magmatik Yer» leşimler ve^ Jeokimya, Türkiye`den Örneklert Ye-ryuvarı ve insan.,. Cilt 6, Sayı, 3-4, s. 53-66, Ankara.

  • Üyede, S., 1981; Subdustion Zort.es and Back Are Basıııs-A. Rewîew, Geol, Rundsch. y Band 70, Heft .2, p. 552-569..

  • Van, A,., 1978; Doğu Karadeniz Bölgesi Demir Ruhsat ve Manganez Mekşuf Sahaları Ttûd Raporu MTA, Rap. No. 1137, Ankara (Yayınlanmamış)

  • Villiers de F..R,., Herbstein F.H. 1967; Distinction Between two Members of the Braunite Group. Tlie American min. Val, 52, Jan-Feb. 1967

  • Wedepohl, K.H., 1975;: The Contribution of Chemical Data to Assumptions About the Origin of Magmas from, the Mantle:, Fortschr. Miner,, 52/2, p. 141-172,, Stutgart.

  • Cfeochemistry of rare earth elements in Bayındır (KAMAN) ßuorite veins
    Süleyman Servet Yaman
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    ABSTRACT: Bayındır fluorite veins appear mithin tho syenites and gabbros formations which belong to Upper Ps^eccene intrusions of Kırşehir Massif, It lias been found that these fluorite-s, which air© greenf whit© and yellow in colour originate«! in varias stages of the hydrothermal perod (Yamam, 1084) in the 8 fluorite samples the total REE eontens varies between 8 and 89 ppm. The dark coloured flaorites contain more BEE. It is seen from the chondrite normalised SEE diagrams that the green fluorites show positive and the yellow ones negative anomalies, Plate on the Tb`La versus Tb/Ca diagram implies that the green fJuorites ?re hydro termal in origin, tat the» yellow fluorites may be produced from the solutions which were affected bj marine water. Hie REE confettis of tîıp green fuorStes formed from hydrotersnal Solutions show « similar REE patterns to that of feldspars. The distribution of KEE in the green and yellow fluorites show that, they were not originated in similar conditions. Ttiese conclusions are in agreement with the data which, were previously obtained from fluid inclusions. Basecl on the geochemical data, it may be said that the evolution of the flmorite veins were related to the basins which developed, after Upper Paleocene time.

  • Bayındır(Kaman)

  • ßuorite Veins

  • Rare Earth Elements

  • Geochemistry

  • Ayan, M., 1963, Contribution a pétrographique de la region située au NE de Kaman (Turquie) : Maden Tetkik Arama Ens.. Yayınları 115, 332 s

  • Bratter, F., Heint, J.K., Joahim, I»., Moeller, P., Roesick, IT. ve Szackî, W., 1972. Fractionation of the rare elements in fluorites: `Erz. Metall. 25„ 380-394

  • Bucrardt, W!, 1953, Orta Anadolu`nun Jeolojisi.. Maden Tetkik Arama Enst. Rapor1 No: 267.5
  • Coryel, C.} Chase, J.t Winchester, J., 1963, A. Procedure for geochemical interpretation of terrestrial earths abondance patterns : J. Oeophys1 . Resc. 68, 559-566.

  • Courtois,, C. ve Deprairies, A., 1978, Les terres rares et. quelques éléments de transition dans les. .minéraux argileux. ISSUS` de denk processus d`altération des; roches basiques:. C.R. Somm,, Soc. Geol., 5, 242-24:5..

  • Dumonceau, J., Bigot,. S., Treuil, M., Faucherre, J.f 1978, Dêtétmination des constantes de formation des carbonato lanthanodates. 0.A..A..S,,, 287, C-329 (Paris).

  • Bills, A,, ve Manon, W.W., 1964,, Natural hot hydrothermal systems and experimental hat water/ rocks -interactrons. Geochim. cosmochixn. acta. 28, 1323*1357

  • Ferrand, A. ve TMMéroz, J,, 1978, Les gites de flu- • orine de l`ouest de la province astuiienne (Arlos, villabona Cucona) „ Bull. B..R..G..M.,, 4y 335- • 355..

  • İskit, M., 1966, Bayındır-Kaman radyoaktif fluorit zuhurları ve civar kay açlarının petrografik etüdü: Maden Tetkik Arama Enst. Dergisi, 66, 149-166.

  • Grappin, C.., Treuil, M., Yaman, S., Touray, J.C., 1979, Le spectre des teıres rares de la fluorine en tant que marqueur des propriétés du milieu de dépôt et des interactions entre solution niineralisantes et roches sources: Mineralium Deposita, 14, 297-309.

  • Guichard, F.,,, 1974,, Contribution à l`étude de la distribution des lanthanides dans la `barytîne: Thèse Université de Paris VI. 103.` s.

  • Marchand, L»., 1976, Contribution à l`étude de la distribution des lanthanides dans la .fluorine: Thèse •Université d`Orléans, 92 s.

  • Ronov, A., Balashov, Y,, Miodisov, A.., 1967, Geochemistry of the. rare earths, in the sedimentary cycle: Geochemistry International, 4, 1-17,

  • Scheider, H.J., Möller, P., Parekh, P.P., 1975, Rare earth elements distrdubution in fluorites and. carbonate sediments of the East-Alpine in the. `Nördlich. Kalkalpen Mineral. Deposita, 10, 330- 344

  • Shepherd, J.T,, Derbyshire, D., Moore, G.., Greenwood, D..., 1982, Rare eath element .and isotopis geochemistry of the North Pennine ore .Deposits: Bcs.ll. Boll... B.R.G.M., 4, 371-377

  • Seymen, Î., 1981, Kaman (Kırşehir) dolayında Kırşehir masifinin stratigrafisi: TBrkiye Jeol. Kur., Bült., 24, 101-108.

  • Treuil, M., Jaffrezic, H., Deschamps, N.., Derre, C, Guichard, F., Joron, J.} , Pelletier, B., Novotny, ,S.„ CourtO`is, C, 1973, Analyse des- Lanthaniäes

  • Hf, Se, Cr, Mn, Co, Cu, Zn dans les minéraux et les. roches, par activation neutronique : Radionalytical chemistry, Special Issue, 18, 55-6$.

  • Turner, T., 1973, 0
  • Yaman, S., 1982, Pluoritte nadir toprak elementleri spektrumıı ve jeokimyasal iz: olarak, kullanılması: Türkiye Jeol, Kur, .36,. Türkiye Bilimsel Ye Teknik Kurultayı, Bildiri Özetleri 98-99

  • Yaman, S., 1984, Bayındır (KAMAN) fluorit filonlarının termo-optik `analizi: Yerbilimleri 11, 23-30.

  • Zeschke, C, 1956,, Kaman kazası radyoaktif fluorit zuhuru hakkında rapor: Maden Tetkik Arama East., Rapor No: 3 17 s. (Yayınlanmamış).

  • Heavy minerals of fltmiatile sedimentary rocks in the Yeşilyurt (Alaşehir) area
    Hüseyin Yilmaz
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    ABSTRACT: Basement metamorphiç rocks in the- Yeşilyurt area are ol Paleozoic age- and consist mainly of mica schist, gneiss and granitic gneiss» Finviatile oetlimieiitary` rocks of Neogene age .`range from, anmature to very immature` and the sandstones are primarily littiie arkose to arkose which are derived from the adjacent matamorptiic complex, -`Sandstone and. conglomerate` were deposited, in an alluvial fan-braided diver environment. One heavy mineral association lias been recognized in Miocene sands from the Yeşilyurt area. Detailed optical .and x-ray diffraction studies revealed that heavy minerals` were derived from the nearby low -grade metainorphic basement. Because no- magmatic, with the exception of metamorphosed granite named here as granitic gneiss, and sedimentary rock types older than, the Miocene sediments are identified In or close to the -study area, the main source of the heavy minerals is from purely metainorphic terrains,,. Thus, the heavy minerals` assemblage typical of metamorphie rocks, seen here is hoped to be an important guide for Meffl.ölica.tî.oıı of unknown source rocks

  • Yeşilyurt(Alaşehir)

  • Fltmiatile Sedimentary

  • Heavy Minerals

  • Magmatic Rocks

  • Folk, R.L., 1974, Petrology of sedimentary rocks, University of Texas, .Austin: Hemphill Pub., Co.

  • Force, E.R., 1980, Provenance of rutile,, Jour.. Sed. Petrology, 50,, 4S5-4.88.

  • Hutton, CJ>,, 1950, Studies of heavy detrital minerals, Bull. Geol. Soc. Ame. 61, 635-716,

  • Müller, G,, 1967, Methods in sedimentary petrology, Germany: Hafner1 Pub. Co

  • Morton,, A.C., 1982, Heavy minerals of Hampshire Paleogene strata,. Geol. Mag.f 119 (5>, 463-476.

  • ttijohn, E.J., Potter, P.E. and. Siever, R.,,, 1973 Sand, and .sandstone. Berlin: Springer-Verlag

  • Yılmaz, H., 1984, Yeşilyurt. (Alaşehir/MANiSA) uranyum ınineraHzasyonu içeren Neojen yaşlı tortulların petrolojisi, minerolojisi ve jeokimyası içinde metamorfik. kayaların mineralojisi ve petrografisi, Bölüm XV. Türkiye Bilimsel ve Teknik. Araştırma Kurumu, Teknik Raporlar Dizisi, Ankara, TBAG 460, 186 p.

  • New observations- on the stratigraphicàl development of Besni Formation to the northwest of Alidam% (Kahta-Adıyaman)
    Engin Meriç Fazil Y. Oktay Sacit Özer
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    ABSTRACT: Until now, in previous studies, Besni Fërmafion, which constitutes a characteristic fitosttsatigraphical unit of the Upper Greaceoiis-Ijasen. aged sedimentary secpieiifie öf Southeast Anatolia^ has bee» :èescrïfee*l as a leefal Hnnesfone ooncordontfy developed with Antak andı Gesmav formations. It has been again, said that; the Antak and Gennav formations follow each-otfaer wîthont ittterftngroing- ami. An-" tak, Besnii ani Gennav formations wllefe ^cûnsfitato^ the lower part: of the sedimentary sequence aro always see» in the same stral%iaphlcal order to tine area.,, To- the .Northwest AUdami (ICalita-JLiiyaiBaii) however, it is abservedl that AnÉak and .Besai fO`rmaMons^ eadhite an interfingerJng1 stratigrapMbal devApmemt andf place, Antak Formatio-n İla ooocordant^f oveilaln toy the Gennav Formation as different from the sofar known»

  • Besni Formation

  • Alidamı(Kahta-Adıyaman)

  • Stratigraphicàl Development

  • Limestone

  • DUNHAM,, R,. J., 1962, Classification of carbonate rocks according to. depositions!, texture,, Mem.. Ass., Petrol Geol, 1, 108.121, 1-7, Tülsa.

  • EMBRY, A.. P. ve KliOVAN, J. G., 1971, A late Devonian reef tract on Northeastern Banks Islands,, Northwest Territories. Cam. Petrol Geology Bull, Ig, 730L781

  • PERÎNÇBK, D., 1979, Geological investigation of the Çelikhan-Sincik-Koçali area (Adıyaman province). I.Ü.F.F. Mecm.,. ; ,, seri B, cilt 44, 127-147.

  • SUNGURLU, O., 1974, Yi Bölge kuzey sahalarının jeolojisi» Türkiye tkinci Petrol Kongresi, 85-107

  • TUNA, D.,, 1973, VI Bölge litostratigrafi birimleri adlamasının, açıklayıcı raporu,. T.P.A.O., Ankara

  • YALÇIN, N., 1977, Geology of the Naıince-Gerger area (Adıyaman province) woA its petroleum. possiMliti.es. tÜJF.F,. Mecm., seri Br cilt 41 (1,-4), 57-82,.

  • Delineation of Underground Cavities;, `Landslide mmd Fractures in Karstie Rocks JBj Using Geotechmicul and Combined Geophysical Technics, Yacht Earbomry Antalya.
    Ahmet Ercan İsmet Özer İrfan Atilgan Mehmet İbrahimiye
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    ABSTRACT: Tie travertines observed along; shore Une of Antalya consists mî three steplike terraces between sea level and SO© meters height. The fourth on© of these terraces takes place below the sea level and e`tends afc least 90 Bieters seaward. There are karstic cavities, veins and Hndiergroiind water channels, caused by chemical dissolution., fractures and gravitational slips in the pliocene aged travertine covers, which have estimated thickness of 300 meters, Theree`iat domestic and touristic buildings over andin front of the travertine cliff which is about SO meters high altong1 the shore Une. Under the influence of the additional weight stack of contractions ami that of waste water, rate of fracturig, breaking off, folding*, block sMpiiig and su&sidencing wr oaimg in are enhanced and them distraction clanger comes off, In order to determine locations and dimensions of such occnrrances combined geophysical (resistivity, natural polarization and seismic refraction), geological surveys, drillings ani laboratory e`peiiments on rock samples were compleded. Opening of gracteres are between 0.1 to SO ein and sosue of them empty and some of them saturated` with water. Travertene is hihly porous and COB tains caves In the rang« from 1 -10 mJ, Geophysical anomaK.es of cracks, fractures and cavities have lower seisin!** wave velocity, lower resistivity If saturated and higher resistivity If empty and larger ionization. The main fractore along` the harbour street has a slop of Si to 80° to tibe srarth and oils disieontifetil^ty m in;t©rseefed. by th& secondsury fa.nlts m NS direction, Sliping rate- of eß to 1 cm/year was Interpreted ft© secandary fractures

  • Karstie Rocks

  • Landslide

  • Combined Geophysical

  • Geotechnical

  • Yacht Earbomry Antalya.

  • Ercan, A. 1982 Doğru Akını Elektrik Özdireng Yöntemleri I.T.Ü. lf,ed, Fak, yayınları, 200 s.

  • Recep Kiliç
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    Recep Kiliç
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