Türkiye Jeoloji Bülteni
Türkiye Jeoloji Bülteni

Türkiye Jeoloji Bülteni

1972 AĞUSTOS Cilt 15 Sayı 2
COVER
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COPYRIGHT PAGE
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CONTENTS
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L’age Radiometrique Du Massif Granodioritique d`Orhaneli
Gürol Ataman
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Abstract: L`utilisation de la méthode géochronologique Rb-Sr a permisde mesurer un âge moyen de 50 M.A. sur six échantillons de laboratoireprovenant de quatre échantillons de terrain prélevés dans la massif d`Orhaneli (Bursa). Bien que l’âge radiometrique coincide avec l’âge proposé(Tertiaire) par un certain nombre de géologues de terrain d`autres chercheurs avancent un âge fort différent (Paléozoique).Dans le cadre de ce travail, il n`a pas été possible de savoir si ces 50M.A. correspondent à l’âge d`une intrusion (primaire), ou au rajeunissement (secondaire) d`un massif d`âge Paléozoique. Cependant, il est acquis que le massif granodioritque d`Orhaneli a subi, il y a 50 M.A. les effetspeut-être conjugués de l’un ou de l`autre de phénomènes géologiques telsque plutonisme, métamorphisme ou tectonique intense. Les travaux deterrains actuellement en cours dans le massif d`Orhaneli se poursuiventdans une optique géochronologique.

  • granodioritique d`Orhaneli

  • intrusion

  • L’age radiometrique

  • Aygen, T., 1956, Balya bölgesi jeolojisinin incelenmesi: M.T.A. Ens. Neş. D. 11.

  • Okay, A.C. 1948, Orhaneli bölgesi, Mustafa Kemalpaşa bölgesi, Çataldağ bölgesine ait izahname 54/2, 54/1, 53/2 paftaları: M.T.A. Rap. No, 2215.

  • Holzer, H., 1954, Beyce 54/4 ve Simav 71/1 paftalarının jeolojik löveleri raporu, M.T.A. Rap. No. 2366 (neşredilmemiştir).

  • Kaaden, G. van der, 1958 ,Saadet-Mesruriye-Safa-Durabey-Domaniç-Tiraz-Saadet köyleri arasındaki sahanın W-Zn-Cu ve Uludağ silsilesi; Orhaneli ve M. Kemalpaşa güneyinde W prospeksiyonu ile bölgenin jeolojik durumu ve evalüasyonu: M.T.A. Rap. No. 2645.

  • Kaaden, G. van der,1959, Anadolunun Kuzeybatısında yer alan metamorfik olaylarla magmatik faaliyetler arasındaki yaş münasebetleri: M.T.A. Bült., 52, 15-34.

  • Kalafatçıoğlu, A., 1964, Balıkesir-Kütahya arasındaki bölgenin jeolojisi Türkiye Jeoloji Kurumu Bülteni, IX: 46-62.

  • Vachette, M., Blanc, P. veDubertret, L., 1968, Determination de l’age d`une granodiorite d`Orhaneli, au Sud de Bursa (Anatolie); sa signification regionale: C. Rend. Ac. Sc. T. 267, Serie D. 927-930.


  • Ataman, G. (1972). Orhaneli Granodiyoritik Kütlesinin Radyometrik Yaşı . Türkiye Jeoloji Bülteni , 15 (2) , 125-130 . Retrieved from https://dergipark.org.tr/tr/pub/tjb/issue/55979/767582

  • Orthoklas-Mikroklin Transformation In Migmatiten Des Eğrigöz-Massivs
    Osman Özcan Dora
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    Abstract: Im Gebiet des Eğrigöz-Massivs wurden die Mineralfazies derregionalen Metamorphose untersucht und festgestellt, dass dieMetamorphose den Grad der Migmatisation erreichte. Das Auftreten der Indexmineralien Cordierit und Sillimanit in den hochgradig-metamorphen Serien beweisst, dass die regionale Metamorphose einen mittleren Typen zwischen Barrow und Abukumaeinnimmt. Radioaktive Altersbestimmungen aus dem Arbeitsgebiet und Vergleiche mit Angaben aus anderen Teilen des Menderes-Massivs ergaben, dass die hochgradige, bis zu Migmatisation angestiegene Metamorphose postliassich, also frühalpidischstattgefunden hat, dass aber das anatektische Eğrigöz-Massiv indie Deckschichten erst nach der Oberkreide eingedrungen ist.Die röntgenographischen Messungen der durch schwere Lösungen angereicherten K-Feldspäte aus der höchstgradig regionalmetamorphen Zone zeigten, dass sie auf der von 1 bis 10 eingeteilten Hoch Sanidin-Maximum Mikroklin Tabelle der 4. Reihe undsomit einem Strukturver-hältnis Or60oMi40 entsprechen. Andererseits steigt der Albitgehalt im K-Feldspat bis zu 20 % an. Setztman die ermittelten Werte in Diagramme ein, die aus Laborversuchen gewonnen wurden, so erhält man eine Transformationstemperatur von 500-550°C. Dieser Wert liegt aber weit unter derMigmatisationstemperatur von 680-700°C, die für eine hochgradige Metamorphose notwendig ist.Es ist daher möglich, folgende Überlegungen als AlternativVorschläge anzustellen :

    1. Seit der letzten Metamorphose steigt derAl-Si-Ordnungsgrad der K-Feldspäte, d.h. ihre Triklinität erhöht sich.

    2. Bei der letzten Aufheizung erreichte die Temperatur im Gebiet um 500-550°C.Im Anbetracht der geologischen Verhältnisse scheint die zweite Überlegung einen höheren Grad der Wahrscheinlichheit zu haben. Es ist sehr Wahrscheinlich, dass bei dem Emporsteigen derMassive an der Kreide-Tertiärgrenze die Temperatur im Untersuchungsgebiet nur bis 500-550°C anstieg und die an den K-Feldspäten festgestellte Erhöhung der Al-Si-Ordnung (Orthoklas-Mikrolin-Transformation) zu dieser Zeit stattgefunden hat.

  • Orthoklas-Mıkrolın Transformatıon

  • Migmatiten

  • Eğrigöz-Massivs

  • Başarır, E., 1970 : Bafa Gölü doğusunda kalan Menderes Masifi güney kanadının Jeolojisi ve petrografisi.—Scien. Rep. of. Fac. of scien, Ege Univ, No: 102, İzmir.

  • Brinkmann, R., 1966 : Geotektonische Gliederung von Westanatolien.—N. Jb. Geol Pal. Mh. 603-618, 6 Abb.

  • Brinkmann, R., 1967 : Die Südflanke des Menderes-Massivs bei Milas, Bodrum und Ören.—Scien. Rep. of Fac. of Scien., Ege Univ., No: 43, Izmir.

  • Brinkmann, R., 1971 : Das kristalline Grundgebirge von Anatolien.—Geol. Rundschau, Bd. 60, 886-899.

  • Bürküt, Y., 1966 : Kuzeybatı Anadolu’da yer alan plütonların mukayeseli jenetik etüdü.—İ.T.Ü. Maden Fak. Yayını, İstanbul.

  • Deer, W.A., R.A. Howie, and J. Zussman, 1966 ; An introduction to the rock forming minerals.—London: Longmans.

  • Dora, Ö.O., 1969 : Petrologische und metallogenetische Untersuchungen im Granitmassiv von Karakoca.—Bull, of the Min. Res. and Expl. Inst, of Turkey, No: 73, .10-26.

  • Dora, Ö.O.,1971 : Kontakt-metasomatik ve hidrotermal çinkoblend yatakları ile bağıntılı olarak Fe-Zn-S sisteminin mineralojik incelenmesi.— Scien. Rep. of Fac. of Scien., Ege Univ. No: 122.

  • Goldsmith. R.J. and Laves, F., 1954 : The microcline-Sanidine stability relations.— Geochim et Cosmochim. Acta, V-5, 1-19.

  • Guidotti, C.V., 1963 ; Metamorphism of the pelitic schists in Bryan Font Quadrangle,. Maine.—Am. Mineralogist 48, 991-1023.

  • Holzer, H., 1954 : Beyce 54/4 ve Simav 71/2. paftalarının jeolojik löveleri raporu.— M.T.A. Rap. No: 2366 (Yayınlanmamış), Ankara.

  • İzdar, E., 1971 : Introduction to geology and metamorphism of the Menderes Massiv of western Turkey.—Geology and History of Turkey, Ed. Angus S. Campbell, Pet. expl. Soc. of Libya, 495-500.

  • Kaya, O., 1972 : Tavşanlı yöresi ofiolit sorununun ana çizgileri.— Bull. of. the geol. Soc. of Turkey. V XV, No: 1, 26-108.

  • Laves, F. and Viswanathan, K., 1967 : Relations between the optic axial angle and triclinicity of potash feldspars, and their significance for the definition of «stable» and «unstable» states of alkali feldspars.— Schweiz. Min. Petrogr. Mitt, t, 47, 147-161.

  • Marmo, V., Hytönen. K., and Vorma, A., 1963 : On the occurrence of potash feldspars of inferior triclinicity within the Precambrian rocks in Finland. Compt. Rend. Soc. Geol. Finlande, 221: 34.

  • Okrusch, M., 1969 Die Gneishornfelse um Steinach in der Oberfalz. Eine Phasenpetrologische Analyse.—Beitrage zur Mineralogise und Petrologie, V. 22, No: 1, 32-72.

  • Orville, M.P., 1963 : Alkali ion exchange between vapor and feldspar phases — Am Journal of science, V. 261, 201-237.

  • Orville, M.P., 1967 : Unit-cell parameters of the microcline-low albite and thesanidine-high albite solid solution series.—The Am. Mineralogist, V. 52. No: 1-2, 55-86.

  • Öztunalı, Ö., 1965 : Petrographie und Entstehung der Uraniumvorkommen der Umgebung von Demirtepe-Çavdar und Osmankuyu-Kısır (Çine-Massiv). —Bull. of the Min. Res. and expl. Inst, of Turkey. No, 65, 119-132.

  • Öztunalı, Ö., 1967 . Flabilitationsarbeit. (Im Druck).

  • Read, H.H., l957 ; The granit controversy. Murby, London, 430 pp.

  • Schuiling, R. D., 1958 A zirkon-study of an augengneiss in the Menderes massive, —Bull of the Min. Res. and expl. Inst of Turkey, No: 51.

  • Schuiling, R. D., 1962 : On the petrology, age and structure of the menderes migmatite complex. Bull. of the Min. Res. and exph Inst of Turkey, No: 59, 71-84.

  • Scotford, M.D., 1963 : Metasomatic augen gneiss in greenschit fasies, western Turkey., Geol. Soc. of America Bull., V, 80, 1079-1094.

  • Steiger, H.R. and S.R. Hart, 1987 : The microcline-orthoclase transtion within a contact aureole.—The Am. Mineralogist, V. 52, No: 1-2, 87- 116.

  • Tomisaka, T., 1962 ; On order-disorder transformation and stability range of microcline under high water vapour pressure —Mineralogical Journal, V. 3, No. 5-6, 261-281.

  • Wjppern, J., 1964 : Die Stellung des Menderes-Massivs in der alpidischen Gebirgs- bildung.—-Bull. of the min. ros. and expl. Inst, of Turkey, No- 62.

  • Winkler, H.G.F., 1966 : Der Prozess Anatexis: Seine Bedeutung für die Genese der Migmatite.—Tschermaks Min. u. Pet. Mitt. Bd, XI, H, 3-4 236-287.

  • Winkler, H.G.F., 1967 : Petrogenesis of metamorphic rocks—Springer-Verlag. Berlin.Heidelberg. New York.

  • Wright L.T., and D.B. Stewartr 1988 : X-Ray and optical study of alkali feldspar, I. Determination of composition and structural state from refined unitcell parameters and 2V.—The Am. Mineralogist, V. 53, No: 1-2, 38-87.

  • Wright, L.T., 1967 : The microcline-orthoclase transformation in the contact aureole of the Eldora Stock; Colorado.—The Am. Mineralogist, V. 52, Nos. 1-2, 117-137.

  • Wright, L.T., 1968 : X-Ray and optical study of alkali feldspar: II. An X-ray method for determining the composition and structural state from measurement of 2θ values for three reflections.—The Am. Mineralogist, V. 53, No: 1-2, 88-104.

  • Zeschke, G., 1953 : 1953 yaz mevsimi löveleri raporu. M.T.A. Rap. No, 2249 (Yayınlanmamış), Ankara.


  • Dora, O. Ö. (1972). (German) Orthoklas-Mikroklin Transformation in Migmatiten des Eğrigöz-Massivs . Türkiye Jeoloji Bülteni , 15 (2) , 131-152 . Retrieved from https://dergipark.org.tr/tr/pub/tjb/issue/55979/767699

  • The Physico-Mechanical Properties of Turkish Marbles and Proposals for Their Classifications
    Kemal Erguvanli Erdoğan Yüzer Kemal Güleç Caner Zanbak
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    Abstract: It is apparent from works of art that marbles and other coloured stones had a special place in the architecture of the different civilizations throughout Turkish history.In Turkey, past and present, approximately 90 % of the stones that canbe scientifically described as marbles, come from Afyon and the Island ofMarmara.In view of this fact, a detailed researah project has been initiated bythe Applied Geology Department of the İ.T.Ü. Mining Faculty to investigatethe geological and physico - mechanical properties of these marbles.The physico-mechanical and technological properties of the abovementioned marbles have been evaluated both in the field and the laboratory. Also, apart from criteria such as colour, and where it is to be used,in the classification of marbles other functional and numerical items likecrystal dimensions, degree of weathering and mechanical anisotropyhave been proposed. At the moment further investigation related to theclassification of other marbles and coloured stones with regard to the numerical criteria used for Afyon and Marmara marbles is being carried out.

  • marble

  • anisotropy

  • Afyon Marbles

  • Turkey

  • Afyon Valiliği, 1967, Afyon İl Yıllığı. Doğan Kardeş Matbaası. İstanbul.

  • Arıkan, M. 1968, Mermer ve Mermercilik. Ankara Basımevi, Ankara.

  • ASTM 1961, Standard Methods of Tests for Exterior and Interior Building Marble. ASTM Committe C-18. Philadelphia.

  • Bain, G.W. 1941, Measuring Grain Boundries in Crystalline Rocks. The Jour. of Geology Vol. XLIX, No: 2, pp. 199-206 Nevalank.

  • Bowles, O. 1968, Marble. Bureau of Mines Inf. Circ. 7829. Denver. U.S.A.

  • Cheung, Y.K. - STAGG, K.G. - ZIENKIEWICZ, O.C, 1966, Stresses in Anisotropic Media with Particular Reference to Problems of Rock Mechanics. Jour. of Strain Analysis. Vol. 1, No: 2, pp. 172-182.

  • Chilingar, G.W. -BISSELL, H.J. -FAIRBRIDGE, R.W. 1967, Carbonate Rocks. Physical and Chemical Properties, Part A and Part B. Elsevier Comp. Amsterdam

  • Donath, F.A. 1964, Strength Variation and Deformational Behavior in Anisotropic Rock- State of Stress in the Earth’s Crust. Elsevier Pub. Co. pp. 281-300, Amsterdam.

  • Grigg, D.T. 1951, Deformation of Yule Marble. Part: I. Effects at 150°C. Bull, Geol. Soc. Am. Vol: 62. pp.

  • Mc. Williams, J.R. 1966, The Role of Microstructure in the Physical Properties of Rocks. Twin Cities Mining Res. Center. Paper No: 102, Minneapolis, Minnesota.

  • M.T.A. 1961, Exterior Marble. Marble Institute of America, New York.

  • M.T.A. 1964, American Standarts Specifications for Interior Marble. Marble Institute of America New York.

  • Ramez, M.R.H. -MURREL, S.A.F, 1964, A Petrofabric Analysis of Carrara Marble. Int. Jour. Rock. Mech. Mining Sci, Vol: 1, Pergamon Press.

  • Sayar, M. -Erguvanlı, K, 1962, Türkiye Mermerleri ve İnşaat Taşları. İ.T.Ü, Yayını. Kağıt ve Basım İşleri A.Ş. İstanbul.

  • Yalman, B. 1969, Afyon Mermerlerinin Arkeolojik Araştırılması (Afyon Müzesinde Yayınlanmamış Rapor).

  • Yüzer, E. 1971, Marmara Adası Mermerlerinin Mühendislik Jeolojisi ve Anizotropik Özelliklerinin Araştırılması. Doçentlik Tezi. (İ.T.Ü. Maden Fakültesi Ofset Atölyesi).

  • M.T.A. 1966, Türkiye Mermer Envanteri. M.T.A. Enstitüsü Yayını, No: 134 Ankara.

  • T.S.E. 1969, Doğal Yapı Taşlan Muayene ve Deney Esasları Türk Standartları. (TS 699), UDK 691.2. Türk Standartları Enstitüsü, Ankara.

  • T.T.S.O.B. 1961, Türkiye Mermerleri, T. Ticaret ve Sanayii O. Birl. Yayını Ankara.


  • Erguvanlı, K. , Yüzer, E. , Güleç, K. & Zanbak, C. (1972). Türkiye Mermerlerinin Fiziko-Mekanik Özellikleri ve Mermerlerin Sınıflandırılmaları Hakkında Düşünceler . Türkiye Jeoloji Bülteni , 15 (2) , 153-170 . Retrieved from https://dergipark.org.tr/tr/pub/tjb/issue/55979/767705

  • The Relationship Between the Degree of Weathering and the Physico-Mechanical Properties of Marbles
    Kemal Güleç
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    Abstract: The effect of weathering on the physical and mechanical properties of marbles has been studied. Prior to the experiments fresh marble specimens were subjected to laboratory weathering. Water absorbtioncapacity of the weathered and fresh specimens was determined as weight percent (Wn, Wo) and a relationship has been established with thedegree of weathering (Dw ) as;

    Dw = Wn—Wo / Wo

    It is observed that with the increase of (Dw) water absorbtion capacity,porosity and unit volume increases but unit weight and compressionalstrength decreases. 

  • Degree of Weathering the Marbles

  • Engineering Geology

  • Accelerated Weathering Experiments

  • Güleç, K., 1970 -Taşların ayrışması ve ayrışmanın ölçülmesi: Madencilik dergisi, C: 9, sayı: 10, Mad. Müh. Oda.,Yay. Ankara.

  • Hamrol, A., 1961 - Quantitative classification of the weathering and weatherability of rocks: 5, Int. Conf. on soil Mech. and Found. Eng. Paris.

  • Iliev, I.G., 1966 -n attempt to estimate the degree of weathering of intrusive rocks from their physico - mechanical properties: I. Int. Cong. of Rock Mech. Proceed. Lisboa.

  • Kessler, D.W., 1949 - A new durability test for marble; ASTM Bull.

  • Kossev, N.W., 1970 - Corrélations entre les caractéristiques physiques et mécaniques de certains roches, ayant égard au degréde l`altération des roches: Pro. of the sec. Cong. of Int. Rock Mech. Beograd.

  • Özuygur, M., 1963 - Ayrışma ve toprak teşekkülü: Umumi Jeoloji II. İTÜ yayını, İstanbul.

  • Ollier, C., 1965 -Weathering: Ollier and boy, Edinburg.

  • Richordson, B.A., 1971 -Chosing stone for the minster: Stone Industries. March-April, London.

  • Schaffer, R.J., 1955 - The weathering, preservation and restoration of stone building. London.

  • Winkler, E.M., 1966 - Important agent of weathering for building and monumental stone. Engineering Geol. Vol: 1 (5).


  • Güleç, K. (1972). Mermerlerin Ayrışma Derecesi İle Fiziko -Mekanik Özelikleri Arasındaki İlişkiler . Türkiye Jeoloji Bülteni , 15 (2) , 171-179 . Retrieved from https://dergipark.org.tr/tr/pub/tjb/issue/55979/767712

  • Stratigraphy of Upper Cretaceous - Lower Tertiary Strata of Yahşıhan Area, East of Ankara
    Teoman Nuriddin Norman
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    Abstract: During the Upper Cretaceous-Lower Tertiary time a continuous (3200 m) sedimentation, mainly consisting of submarine slumps,olistostromes and turbidity currents, was taking place in the western halfof the area. Meanwhile, in the eastern half, a granit complex plutonic intrusion was emplaced (Early Paleocene) in a formation, dominantly consisting of basic submarine lavas and tuffites. Uplift, erosion and subsidence of the eroded surface was followed by a marine transgression nearthe closing of Paleocene times. Following the deposition of neritic andpartly littoral sediments (700 m), towards the end of Eocene (post Lutetian) a regression developed over the whole area, causing the depositionof mainly red colored rudite, arenite and lutite, as well as lagoonal whitelimestone and gypsum.Horizontal Neogene clastics rest with an angular unconformity onthe folded, uplifted and eroded sediments of Late Cretaceous-EarlyTertiary age.

  • turbidity current

  • olistostrome

  • transgression

  • regression

  • Ankara Yahsihan Area

  • Abbate, E., Bortolotti, V. ve Passerini, P., 1970 Olistostromes and olistoliths: Sedimentary Geology, 4, s. 521-558.

  • Arni, P., 1942, Anadolu ofiolitlerinin yaşlarına mütedair malümat; M.T.A. Enstitüsü Dergisi, 3/28, s. 472-488.

  • Ayan, M. 1959, Contribution a I’étude petrographique de la région située au nord- est de Kaman (Turquie). (Tez, Nancy): M.T.A. Enstitüsü Yayınları no. 115.

  • Bailey, E.B. ve Mc Sallien, W.C. 1950, Ankara Melanjı ve Anadolu Şaryajı M.T.A. Enstitüsü Dergisi, 40, s. 12-22.

  • Baykal, F. 1943, Kırıkkale-Kalecik ve Keskin-Balâ Mıntıkalarındaki Jeolojik Etüdler. M.T.A. Enstitüsü Derleme Raporu, no. 1448.

  • Blumenthal, M., 1948, Bolu civarı ile Aşağı Kızılırmak mecrası arasındaki Kuzey Anadolu silsilelerinin jeolojisi: M.T.A. yayınları, Seri B, no. 13 Ankara.

  • Boccaletti, M. ve Bortolotti, V. Sağrı, M. 1966, Richerche sulle ofioliti delte Catene- Alpine: 1 — Osservazioni sull’Ankara Mélange nella zona di Ankara.. Boll. Soc. Geol. It., 85, s. 485-508.

  • Bouma, A.H., ve Brouwer, A. 1964, Turbidites Elsevier, Amsterdam, 254 s.

  • Brinkmann, R., 1968, Einige geologische Leitlinien von Anatolien: Geol, et Palaont., 2, s. 111-119, Marburg.

  • Buchardt, W.S., 1958, Orta Anadolu’da 1:100:000 ölçekli Jeolojik Harita çalışmaları hakkında rapor: (Çeviren: Z. Bengi). M.T.A. Derleme Raporu, no. 2675.

  • Chaput, E., 1936, Türkiye’de Jeolojik ve Jeomorfolojik tetkik seyahatları (Çeviren: A. Tanoğlu, 1947): İstanbul Üniversitesi Yayınlarından, no. 324.

  • Dobkins, J.E., ve Folk, R.L. 1970, Shape development on Tahiti-Nui: Jour. Sed. Pet., 40, s. 1167-1203.

  • Dott, Jr. R.H., 1963, Dynamics of subaquaeous gravity-depositional processes: Bull. Amer. Assoc. Petrol. Geol., 47, 104-128.

  • Dzulynski, S., ve Walton E.K 1965, Sedimentary features of flysch and greywackes: Developments in sedimentology, no. 7, Elsevier, Amsterdam, 274 s.

  • Egeran, E.N. ve Lahn, E. 1948, Türkiye Jeolojisi Ankara, 190 s.

  • Egeran, E.N. ve Lahn, E. 1951, Kuzey ve Orta Anadolu’nun tektonik durumu hakkında not: M.T.A. Enstitüsü Dergisi, no. 41, s. 23-27.

  • Erk, A.S., 1957, Ankara civarı petrol ihtimalleri: M.TA. Enstitüsü Raporu, no. 2608 (Yayınlanmamış).

  • Erol, O., 1954, Ankara civarının jeolojisi hakkında rapor, M.T.A. Enstitüsü Raporu, no. 2491.

  • Erol, O., 1955, Kalecik-Hasayaz-Termeçay civarı jeolojisi hakkında rapor: M.T.A. Derleme Raporu, no. 2310.

  • Erol, O., 1956, Ankara güneydoğusundaki Elma Dağı ve çevresinin jeolojisi ve jeomorfolojisi üzerine bir araştırma:

  • Erol, O., 1958, 41/3, 41/4, 42/3, 42/4, 43/3 numaralı paftalar sahasının jeolojik revizyon ve korelasyonu hakkında rapor: M.T.A. Derleme Raporu, no.

  • Erol, O., 1961, Ankara bölgesinin tektonik gelişmesi: T.J.K. Bülteni, 7, s. 57-85.

  • Erol, O., 1938, Ankara çevresinde Paleozoik arazisinin bölümleri ve Paleozoik-Mesozoik sınırı hakkında: TJ.K. Bülteni, 9, s. 1-20.

  • Erol, O., 1969, Tuzgölü havzasının jeoloji ve jeomorfolojisi: T.B.T.A.K. Raporu (Yayınlanmamıştır),

  • Fiske, R.S. ve Matsuda, T., 1934, Submarine equivalents of ash flows in Tokiwa Formation, Japan: Amer. Jour. Sci., 232, s. 76-106.

  • Folk, R.L., 1968, Petrology of Sedimentary rocks: Hemphill`s. Austin. Texas. 170 s.

  • Gansser, A., 1959, Ausseralpine Ophioloth probleme: Ecl. Geol. Helv., 52, s. 659-680.

  • Gökçen, S.L., 1971, Keşan bölgesi türbiditlerinde siklik sedimentasyon: Hacettepe Fen ve Müh. Bil. Derg., 1, s. 26-40.

  • Hendry, H.E., 1972, Breccias deposits by mass flow in the Breccia Nappe of the French pre-Alps: Sedimentology, 18, s- 227-292.

  • Ketin, İ., 1954, Yozgat Bölgesinin jeolojik lövesi hakkında memuar; M.T.A. Enstitüsü Derleme Rapor, no. 2141.

  • Ketin, İ., 1955, Yozgat Bölgesinin Jeolojisi ve Orta Anadolu Masifinin Tektonik Durumu: T.J.K. Bülteni, 6, s. 1-28.

  • Ketin, İ., 1959, Türkiye’nin orojenik gelişmesi: M.T.A. Enstitüsü Dergisi, 53, s. 78-86.

  • Ketin, İ., 1961, Türkiye’de magmatik faaliyet; TJ.K. Bülteni, 7, s. 1—15.

  • Ketin, İ., 1963, Türkiye Jeoloji Haritası (1:500.000), Kayseri izahnamesi: M.T.A. Yayınlarından, Ankara.

  • Ketin, İ.,1966, Anadolu’nun tektonik birlikleri-: MT.A. Enstitüsü Dergisi, 66 s. 20-34.

  • Kuenen, PH.H., 1967, Emplacement of flysch-type sand beds: Sedimentology, 9, s. 203-243.

  • Lahn, E., 1949, Orta Anadolu`nun Jeolojisi Hakkında: TJ.K. Bülteni, 2, 90- 107.

  • Lokman, K. ve Lahn, E. 1946, Haymana bölgesi jeolojisi: M.T.A. Enstitüsü Dergisi, 2/36, s. 292-299.

  • Maucher, A., 1937, Ankara vilayetinin Keskin kazasında Hüseyinbeyobası mevkiinde molibdenit ve povelit zuhuru: M.T.A. Derleme Rap. no. 635 (Yayınlanmamıştır).

  • Middleton, G.V., 1966, Experiments on density and turbidity currents, I. Motion of the head: Canadian Jour. Earth Sci., 3, s. 523-546.

  • Mitchell, A.H.G. and Reading, H.G. 1969, Continental margins, geosynclines and ocean floor spreading: Jour. Geol., 77, s. 629-646.

  • Mitchell, A.H.G., 1970, Fades of an early Miocene volcanic arc, Malekula Island, New Hebridies: Sedimentology, 14, s. 201-243.

  • Natland, M.L., ve Kuenen, PH.H. 1951, Sedimentary history of the Ventura Basin California, and the action of turbidity currents. Soc. Econ. Paleon. Min. Spec. Publ. no. 2, s, 76-107.

  • Norman, T., 1972, Ankara doğusunda Yahşıhan bölgesinde Üst Kretase - Alt Tersiyer yaşlı Arazinin Jeolojisi (Tez): Orta Doğu Teknik Üniversitesi Jeoloji Müh. Bl. Ankara.

  • Pettijohn, FJ., 1957( Sedimentary Rocks: Harper, New York, 689 s.

  • Pettijohn, F.J., Potter, P.E. ve Siever, R. 1972, Sand and Sandstone: Springer-Verlag, Berlin, 600 s.

  • Reckamp, J.U., 1959, Preliminary report on the petroleum possibilities of the Çankırı licenses: AR/TGO/II/471-472 Petrol Dairesi Teknik Arşivi.

  • Reckamp, J.U., Özbey, S. 1960, Supplementary Report on the Petroleum possibilities of the Çankırı Area: AR/TGO/II/471-472 Petrol Dairesi Teknik Arşivi.

  • Rich, J.L., 1951, Three critical environments of deposition and criteria for recognition of rocks deposited in each of them: Geol. Soc. Amer. Bull., 62, s. 1-20.

  • Rigo de Righi, M. ve Cortesini, A. 1960, Regional studies. Central Anatolia Basin. Progress Report. 1 — Stratigraphy, 2 — Structure. Petrol Dairesi T.A. Turkish Gulf Oil Co. 11/11-12 (Yayınlanmamıştır).

  • Rigo de Righi, M. ve Cortesini, A. 1964, Gravity tectonics in foothills structure belt of SE Turkey: A.A.P.G., 48, s. 1911-1937.

  • Schmidt, G.C., I960, Geological evaluation of the licences 360-363 and 365-367, District II: Petrol Dairesi, Ankara (Yayınlanmamıştır).

  • Stchepinsky, V., 1942, Bursa ile Tercan arasındaki bölgenin mukayeseli stratigrafisi M.T.A., Enstitüsü Dergisi. 2/27, s. 290-321.

  • Walker, R.G., 1967, Turbidite sedimentary structures and their relationship to proximal and distal depositional environments: Jour. Sed. Pet., 37, s. 25-43.

  • Walker, R.G., 1970, Review of the geometry and facies organisation of turbidites and turbidite-bearing basins: Geol Assoc. Canada, Spec, paper no. 7, s. 219-251.

  • Yücel, T., 1953, Kızılırmak-Yeşilırmak arasında kalan bölgenin jeolojisi hakkında rapor; M.T.A. Derleme Raporu, no. 2001.

  • Yücel, T., 1954, Deveci dağları-Kalecik arasında Kuzey Anadolu dağlan ile Iç Anadolu intikal alanının jeolojisine dair rapor: M.T.A. Derleme raporu, no. 2295.

  • Yüksel, S., 1970, Etude Géologique de la Region D`Haymana (Turquie Centrale). Thèse. Faculté des Sciences de L`université de Nancy, France.


  • Norman, T. (1972). Ankara Yahşıhan Bölgesinde Üst Kretase - Alt Tersiyer İstifinin Stratigrafisi . Türkiye Jeoloji Bülteni , 15 (2) , 180-276 . Retrieved from https://dergipark.org.tr/tr/pub/tjb/issue/55979/767726

  • Systematic Study of New Species of the Genera Fabularia and Kathina From Paleocene
    Ercüment Sirel
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    Abstract: Systematic study of new species of the genera Fabularia andKathina with associated Foraminifera in Paleocene of Kars Region (NETURKEY), are given.

  • Fabularia

  • Kathina

  • foraminifera

  • Kars Region

  • Cole,W.S., 1947 - The internal structure of some Floridan Foraminifera. Bull. Amer. Paleont., v. 31, p. 225-254.

  • Cole,W.S., 1958 - The Genera Miscellanea and Pellatispirella. Bull. Amer. Paleont., v. 36, p. 237-254.

  • Davies, L.M., 1927 - The Ranikot Beds at Thai (NW Frontier Provinces of India). Quart. J. Geol. Soc. London v, 83/2, p. 260-290,

  • Davies, L.M., & Pinfold, E.S. 1937 - The Eocene Beds of the Punjab Salt Range. Paleont. Indica n. ser., 24, p. l-79.

  • Grimsdale, T.F., 1952 - Cretaceous and Tertiary Foraminifera from the Middle East. Bull, of the Brit. Muse. (Nat. Hist.) Geol., v. 1/8, p. 224.

  • Hanzawa, S., 1962 - Upper Cretaceous and Tertiary three-layered Foraminifera and their allied forms. Micropaleontology v. 8/2, p. 129-186.

  • Hottinger, L., 1960 - Recherches sur les Alveolines du Paleocène et de l`Eocene. Mémoires Suisses de Paleontologie v. 75/76.

  • Kaever, M., 1970 - Die AIttertiären Grossforaminifer Südost Afghanistans unter besoderer Berücksichtigung der Nummulitiden Morfologie, Taxonomie und Biostratigraphie. Geologie in Münster.

  • Pfender, J., 1934 -A propus du Siderolites vidali Douv., Bull. Soc. Geol. France, S.4, p. 225-236.

  • Reichel, M., 1931 - Etude sur la Alvéolines. Mem. de la Société paleontologique Suisse, v. LVII.

  • Reichel, M. & Sigal, J., 1969- Description d`une Lacazina nouvelle (Foraminifères Miliolidés) dans le Paléocène du Taurus de Beyşehir (Turquie). Rev. Espanola de Micropal., vol. 1, p. 317.

  • Schlumberger, C. 1894 - Note sur Lacazina wichmanni n. sp.. Bull. Soc. Geol. France., ser. 3, T. 22, fas. 5, p. 296-298.

  • Smout, A.H., 1954 - Lower Tertiary Foraminifera of the Qatar Peninsula. Brit. Mus. (Nat. Hist.) p. 1-96, p|. I-XV

  • Vaughan, T.W., 1929 - Additional new species of Tertiary larger Foraminifera. J. Paleont. v. 3, p. 337.

  • Vaughan, T.W. & Cole, W.S., 1941 - Preliminary report on the Cretaceous and Tertiary Foraminifera. Geol. Soc. Amer. Spec, paper, p.1-137, pl. 1-46.


  • Sirel, E. (1972). Systematic Study of New Species of The Genera Fabularia and Kathina from Paleocene . Türkiye Jeoloji Bülteni , 15 (2) , 277-294 . Retrieved from https://dergipark.org.tr/tr/pub/tjb/issue/55979/767734

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