Türkiye Jeoloji Bülteni
Türkiye Jeoloji Bülteni

Türkiye Jeoloji Bülteni

1985 ŞUBAT Cilt 28 Sayı 1
COVER
View as PDF
COPYRIGHT PAGE
View as PDF
CONTENTS
View as PDF
Sedimentary Sequences and Tectonic Setting of Saros Gulf Area- Northeast Agean Sea, Turkey
Salih Saner
View as PDF

Abstract: There are three sedimentary sequences in the study area separated by erosional surfaces: 1- UpperCretaceous - Lower Eocene sequence with undefined bottom and regressive upper section. 2. Middle Eocene-Oligocenesequence starting with transgressive bottom and ending with regressive top. and 3, Mio-Pliocene-Quaternary shallowmarine sequence which starts with transgressive lower section. Among these only the Middle Eocene-Oligocene issedimentologically uniform to the north and south of Saros BayFive main structural features have been defined: 1- Hisarlidağ High, 2- Enez Graben, 3. Semadirek High, 4. SarosGraben, and 5. Gelibolu Block. The two highs and Gelibolu Block are pre-Miocene anticlinal structures. Enez andSaros grabens developed in synclines between the anticlines- Mio-Pliocene sequence makes transgressive onlaps onthe flanks of structural highs- Enez Graben was filled by Miocene and younger sediments, but Saros Graben is stillactive and deepening.Ganos Fault located on the extension of the right lateral North Anatolian Fault follows a pre-Middle Miocene(probably Upper Cretaceous-Lower Eocene) paleo-tectonic zone. Structures and the uniform Middle Eocene-Oligocene lithostratigraphic units on both sides of the Ganos Fault indicate no significant slip along the fault duringMiddle Eocene. However, at the end of Oligocene compres sional forces affected the area- Normal fualting and grabens show the domination of tensional forces following Miocene

  • Ganos Fault

  • Saros Gulf

  • North Anatolian Fault

  • anticlinal

  • synclinal

  • Ashland Oil of Turkey, 1972, Marine geophysical survey of offshore Turkey, Gulf of Saros, Ashland Oil of Turkey, by Ray Geophysical Division: Petrol îşleri Genel Md-, Rapor no. 2, 18 s.

  • Brineman, HJ, 1974, Relinquishment report: Gulf of Saros Area, Turkey, Ashland Oil of Turkey. Petrol îşleri Genel Md. Rapor no- 3, 22 s.

  • Bingöl, E, 1976, Batı Anadolunun jeotektonik evrimi: MTA Mecm, 86, 21 s.

  • Erol, V-, 1978, Enez civarı gravite ve manyetik değerlendirmesi ve sismik yorum ile karşılaştırması: TPAO Rapor no. 1274, 8 s.

  • Kellog, EH-, 1972, Geology and Petroleum prospects: Gulf of Saros and Vicinity Southwestern Thrace, Ashland Oil of Turkey: TPAO Rapor no. 902, 121 s.

  • Le Pıchon, X-, Francheteau, J-, Bonnin, X, 1973, Plate Tectonics: Elsevier Scientific Publishing Company, Amsterdam-London-New York, 300 s

  • Önem, Y-, 1974, Gelibolu yarımadası ve Çanakkale dolayının jeolojisi: TPAO Rapor no. 877, 30 s.

  • Saner, S-, 1982, Batı Pontidlerin ve komşu havzaların oluşumlarının levha tektoniği kuramiyle açıklanmasıM.T.A. Enst. Dergisi, 93/94, 19 s.

  • Sfondrini, G-, 1961, Surface geological report on AR/TGO/ 1/537, 538 Eceabat and Çanakkale areas, Turkish Gulf Oil Comp.: TPAO Rapor no. 1429, 9 s

  • N.V. Turkse Shell`in 1969, I No- lu Marmara petrol bölgesinde AR/NTS/837, 838, 839 hak sıra no. lu arama sahalarına ait terk raporu: TPAO Rapor no. 1408, 5

  • Distribution of Loftusia Anatolica Meriç in Neo-Tethys
    İbrahim Engin Meriç
    View as PDF

    Abstract: The distribution of Loftusia anatolica MERİÇ which is one of the typical organism of Maastrichtianin the Middle-East and Northeastern Mediterranean regions and principle agents which may play an importantrole on this distribution are discussed.Within the central part of the Neo-Tethyan domain two subzones can be discerned, viz the Middle-East and theNortheast Mediterranean on the basis of species differentiation of Loftusia`s, Loftusia anatolica MERİÇ has beendiscovered in both these subzones. Different Loftusia species and degree of diversity suggest that SE Turkey wasnear the equantor (0-15°N) during the Maastrichtian, whereas northern, western and central Turkey was farthernorth (15-30°N). These results are in good agreement with recent palaeotectonic/palaeogeographic reconstructions ofthe Mediterranean/Middle-East regions.

  • Loftusia anatolica

  • Meriç

  • Mediterranean

  • Akartuna. M- 1962 a. Çaycuma-Devrek-Yenice-Kozcağız bölgesinin jeolojisi: 1st- Üniv. Fen Fak. Monografileri. IV.

  • Akartuna, M., 1962 b, Izmir-Torbalı-Seferihisar-Urla bölgesinin jeolojik etüdü. 1st. Üniv. Fen Fak. Monografileri, 18-

  • Akartuna- M., 1968, Armutlu yarımadasının jeolojisi. 1stÜniv. Fen Fak- Monografileri: 20-

  • Akkuş. M-, 1970, Darende-Balaban Havzasındaki (Malatya ESE Anadolu) litostratigrafik birimler ve jipsli formasyonların yaşı hakkında yeni bilgiler: MTA Enst. Derg, 75, 1-14

  • Altınlı, İ- E-, 1954, Siirt güneydoğusunun jeolojisi: ÎÜF. F. Mecm.. seri B, 19 (D, 1-31.

  • Altınlı, î- E-, 1963 a, 1/500000 ölçekli Türkiye Jeoloji Haritası, Erzurum Paftası

  • Altınlı, t E.. 1963 b, 1/50O-00O ölçekli Türkiye Jeoloji Haritası, Cizre paftası

  • Atan, O. R., 1969, Eğribucak-Karacaören (Hassa)-CeylanlıDazevleri (Kırıkhan) arasındaki Amanos dağlarının jeolosi: M-T-A. Enst. yayını no: 139-

  • Barron, E. J-, Harrison CG-A. Sloan II- J- L. ve Hay W. W., 1981, Paleogeography, 180 million years ago to the present. Eclogae geol. Helv., 74 (2), 443-470.

  • Baykal, F., 1942, Şile mıntıkasının jeolojisi İ-Ü-F-F- Mecm. seri B- 7, 166-233, 1-7-

  • Baykal, F., 1954, Eflani-Ulus arasındaki Kretase-Tersiyer arazisi ve ekzotik bloklar (kuzeybatı Anadolu): I-Ü. F.F. Mecm-, seri B, 19 (3), 191-201-

  • Baykal, F-, 1964, 1/500000 ölçekli Türkiye Jeoloji Haritası, Sivas paftası

  • Blumenthal, M. M-, 1942, Sinop vilayeti, Boyabat Havzası petrol yataklarının jeolojik tespiti: M.T.A. Enst, yayım, seri A, no: 6

  • Blumenthal, M- M., 1956. Yüksek Bolkardağm kuzey kenar bölgelerinin ve batı uzantılarının jeolojisi: M T-A- Enst- yayını, seri D, no: 7

  • Brinkmann, R- 1966, Abriss der geologie: Zweiter Band, Historische Geologie. Ferdinand Enke verlag, Stuttgart

  • Buser, S- ve Cvatic, S., 1973, Türkiye`deki Murgul bakır yatağı yöresinin jeolojisi M.T.A. Enst. Derg. 81, 22-45.

  • Cox, P-. 1937. The genus Leftusia in south western Iran. Eclogae geol. Helv-, 30, 431-450, 33-37.

  • Demirkol, C-. 1979, Üzüjnlü-Tuzakh (Bilecik) dolayının jeolojisi: Türkiye Jeol- Kur. Bült. 20 (1). 9-16.

  • Demirtaşlı, E- ve Pisoni, C-, 1965, Ahlat-Adilcevaz bölgesinin jeolojisi (Van gölü kuzeyi): M.T.A. Enst. Derg.. 64, 22-36.

  • Dilley. F. C, 1971, Cretaceccous foraminiferal biogeography; in Middlemiss, F. A- Rowson, P. F-, and Nevall, G. (ed-). Faunal provinces in space time. Geological Journal, Special Issue, 4, 169-190, Proceeding of the 17th International University Geological Congress. Seel House Press, Liverpol

  • Dizer, A. ve Meriç, E-, 1972, Kuzeybatı Anadoluda Kretase-Eosen sınırının mikroorganizmalar ile tespiti: TB-A.K- tarafından desteklenen 33 no`lu proje.

  • Dizer, A. ve Meriç, E-, 1983. Kuzeybatı Anadoluda Üst Kretase-Paleosen biyostratigrafisi: M-T.A. Enst. Lerg95-96, 149-163-

  • Erk, S-, 1942, Etude glologique de la region entre Gemlik et Bursa (Turquie): M-T.A. Enst. yayını, seri B, no 9.

  • Eroskay, S- O-, 1965, Geology of Paşalar george Gölpazarı Area. tÜ.F-F. Mecm- seri D. 30 (3-4), 135-175, 1-9

  • Gordon, W. A-, 1973, Marine life and ocean surface currents in the Cretaceous: Journal of Geology, 81. (3). 269-284.

  • Henson, F- R. S-, 1948. Larger imperforat foraminifera of south-western Asis- Families Lituolidae, Orbitolinidae and Meandropsinidae: Brit- Mus. Nat- History Mem-, London

  • Kalafatçıoğlu, A. ve Uysalh, H-, 1964, BeypazanNallıhan-Seben civarının jeolojisi: MTA. Enst. Derg. 62, 1-11.

  • Kalafatçıoğlu, A-, 1962, Tavşanlı-Dağardı arasındaki bölgenin jeolojisi ve serpantin ile kalkerlerin yaşı hakkında not: M.T.A. Enst-, Derg. 58. 38-46.

  • Kendiroğlu, Z- 1971, Hekimhan-Hasançelebi-Deveci bölgesinin jeolojisi (Malatya): Î.Ü-F-F. Yüksek Jeoloji Diploma çalışması.

  • Ketin, 1. 1947, Elazığ bölgesi jeolojisinin ana çizgileri: t Ü-F-F. Mecm- seri B. 12 (4). 255-267.

  • Ketin, I.. 1950. Ergani-Eğil bölgesinde yapılan jeolojik araştırmaların tektonik neticesi. ÎÜFF- Mecm-, seri B. 15 (2). 134-152.

  • Ketin, t-, 1955, Zonuldak doğusunda Ovacuma bölgesinin jeolojisi hakkında: I-Ü.F.F. Mecm., seri B, 20 (3). 147-154.

  • Ketin, 1. 1962 1/500000 ölçekli Türkiye Jeoloji Haritası, Sinop paftası

  • Koçyiğit, A-, 1980. Hoyratı gölü yöresinin (Afyon-Isparta) stratigrafik ve tektonik özellikleri: Doçentlik tezi (yayımlanmamış)

  • Kummel. B-, 1970, History of the earth: W. H. Freemen and Company, San Fransisco

  • Kurtman, F-, 1973, Sivas-Hafik-Zara ve îmranlı bölgesinin jeolojik ve tektonik yapısı: MTA. Enst-, Derg-, 80. 1-32

  • Kurtman, F-, 1978, Gürün bölgesinin jeolojisi ve tektonik özellikleri: MT-A. Enst-, Derg- 91. 1-12

  • Lokman. K-, 1946. Kürzot petrol madeni ve havalisi: M. T.A. Enst- Derg., 35. 95-101.

  • Martin. C, 1969, Akseki bölgesindeki bir kısım Torosların stratigrafik ve tektonik incelenmesi. M-T-A. Enst. Derg-, 72, 158-175

  • Meriç, E- 1965 a- Kahta-Nemrut dağı arasındaki bölgenin jeolojik ve paleontolojik etüdü: Î.Ü-F.F. Mecm., seri B, 30 (1-2), 55-107, 1-20.

  • Meriç, E- 1965 b- Sur deux nouvelles especes de Loftusia et un nouveau genre Asterosomalina: Rev. de Micropaleont- 8 (1), 45-52, 1-2.

  • Meriç. E- 1967, Türkiye`yi bazı Loftusiidae ve Orbitoididae`ler hakkında: İÜ-F.F- Mecm-, seri B, 32 (1-2), 1-58, 1-36.

  • Meriç, E-, 1973, Mutki (Bitlis) güneyindeki sınırlı bir Üst Maestrihtiyen mostrasının varlığı hakkında: LÜ-FFMecm-, seri B, 38 (1-4), 49-51, 1.

  • Meriç, E-, 1974 a, Orbitoides apiculatus SCHLUMBEAGER pamiri n- ssp- du Maestrichtien superieur du Taurus Lycien (Turquie): Revista Espanola de Micropaleontologia, 6 (1), 135-144, 1-4.

  • Meriç, E-, 1974 b. Loftusia cinsinin Göynük (NW Türkiye) dolayında bulunuşu: İ-Ü-F-F. Mecm-, seri B, 39 (3-4), 227-232.

  • Meriç, E., 1975, Loftusiidae familyasının Türkiye`deki coğrafi dağılımı. TB.T A.K.V. Bilim Kongresi, İzmir, 161-169.

  • Meriç, E-, 1978, Dizerina, a new genus from the Upper Maastrichtian of north eastern Turkey: Miccropaleontology, 24 (1), 97-108, 1-4.

  • Meriç, E-, 1979, Loftusia katini (Foraminifere) nouvelle espece du Maestrichtian: Revista Espanola de Micropaleontologia, 11 (3), 509-516, 1-2.

  • Meriç, E-, 1980, Pseudomphalocyolus blumenthali. a new genus and species from the Upper Maastrichtian of southern Turkey: Micropaleontology, 26 (1), 84-89, 1-2.

  • Meriç, E-, ve Mojab, F-, 1977. World-wide geographical distribution of the species of the foraminiferal genus Loftusia: Î.Ü-F.F. Mecm-, seri B, 42 (1-4), 143-155.

  • Milovanovich, B-, 1935, Loftusia morgani. DOUVILLE iz Mastrihijena Istoncne Serbije: Geoloski an B. P. XII, 2, str. 246-252, Beograd.

  • Mintz L. W-, 1972, Historical Geology- The sciences of a dynamic earth: Cahrles E- Merril publishing Company, Ohio

  • Molinari, P- V., Tilia, Z. A. ve Meriç, E-, 1984, Donne`s biostratigraphiques sur la succession Senonienne des Monti Lepini. (Appenino Centre-meridonal) (Baskıda)

  • Önalan, M-, 1979, Elmalı-Kaş (Antalya) arasındaki bölgenin jeolojisi: 1st- Üniv. Fen Fak. Monografileri, no. 29.

  • Öztürk, A., 1981, Homa-Akdağ (Denizli) yöresinin stratigrafisi: Türkiye Jeol- Kur. Bült-, 24 (1), 75-84

  • Papp, A-, 1955, Orbitoides aus der Oberkreide der Ostalpen (Gosauschichten): Österr- Akad-, math, -naturwki-, Sitzber. Vienna, 164 (6-7), 303-315, 1-3.

  • Pisoni, O-, 1967, Kaş (Antalya ili) bölgesinin jeolojik etüdü: M.T.A. Enst, Derg-, 69, 42-49

  • Reichel, M-, 1949, Sur un nouveau Orbitoide du Cretace superieur hellenique: Eclogae geol- Helv-, 42 (2), 480- 485

  • Salaj, J- ve Amuel, O-, 1966, Foraminifera der Westkarpaten-Kreide (Slowakei): Bratislava.

  • Seymen, İ-, 1975 Kelkit vadisi kesiminde Kuzey AnadoluFay Zonunun tektonik özelliği. 1-192, Tez (yayımlanmamış)

  • Sirel, E-, 1973, Cide Maestrihtiyenindeki yeni Cuvillierina türünün tarifi: Türkiye Jeol. Kur. Bült-, 16 (2), 69` 76, 1-2-

  • Sirel, E- ve Gündüz, H., 1978, Sivas Maestrihtiyenindeki Sivasella n- gen- (Foraminifer) cinsinin tanımı: Türkiye Jeol. Kur. Bült. 21 (1), 67-75, 1-3.

  • Stchepinsky, V., 1946, Fossiles caracteristiques du Turquie: M-T-A. Enst-, yayını.

  • Şengör, A. M. C, Yılmaz, Y. ve Sungurlu, O-, 1984 Tectonics of the Mediterranean Cimmerides: Nature and Evolution of the western termination of PalaeoTethys: in J. E- Dixon and A.H.F. Robertson edts- Geological Evolution of the Eastern Mediterranea, Geol. Soc- London, Spec- pub., 13, 117-158

  • Smith, A- G., Hurley, A. M. ve Briden, J. C, 1981, Pharerozoic paleocontinental world maps: Cambridge University press, 1-102

  • Tansel, 1., 1980, Nallıhan ve dolayının biyostratigrafi incelemesi. Yerbilimleri, 5-6, 31-47

  • Terlemez, î. ve Yılmaz, A-, 1980, Ünye-Ordu-Koyulhisar-Reşadiye arasında kalan yörenin stratigrafisi: Türkiye Jeol. Kur. Bült, 23 (2), 179-191.

  • Ternek, Z-, 1953, Van gölü güneydoğu bölgesinin jeolojisi: Türkiye Jeol. Kur. Bült., 4 (2), 1-27.

  • Tokay, M-, 1955, Filyos çayı ağızı-Amasra-Bartm-Kozcağız-Çaycuma bölgesinin jeolojisi: M.T.A. Enst-, Derg.. 46-47, 58-70

  • Toker, V., 1976, Stratigraphical studies of the area located between Nallıhan and Bozyaka villages along the Sorgun river: Communications de la Faculte des Sciences de l`Univ- d`Ankara, seri C, 19. 1-63, 1-5.

  • Tolun, N-, 1962, 1/500000 ölçekli Türkiye Jeoloji Haritası Mardin paftası,

  • Tolun, N. ve Ternek, Z., 1952, Mardin bölgesinin jeolojisi: Türkiye Jeol. Kur- Bült, 3 (2), 1-14.

  • Tromp, S- W., 1941, The stratigraphical distribution of the genera Orbitoides and Omphalocyclus in S-E Turkey: M.T.A. Enst, Derg., 3/24, 361-370-

  • Üşenmez, Ş-, 1974, Çandır (Kalecik) civarının jeolojisi M-T-A. Enst. Der., 83, 30-46-

  • Yılmaz, O-, 1980, Daday-Devrekani masifi kuzeydoğu kesimi biostratigrafi birimleri ve tektoniği. Yerbilimleri, 5-6, 101-135-

  • Yüksel, S-, 1970, Etude geologique de la region d`Haymana (Turquie centrale). Tez (yay unlanmamış).

  • Geology of the Maden Magmatic Rocks, Southeast Malatya, and A Geochemical Approach to Their Tectonic Setting
    Mustafa Özçelik
    View as PDF

    Abstract: Rocks of the Maden Complex in the Poluşağı area (southeast Malatya) lie over the Pütürge Massifwith a tectonic contact. The Maden Complex of Middle Eocene age is locally composed from bottom to top oflimestone, calc-schist, red-schist, agglomerate, volcanics and the intruding hypabysssal rocksThe volcanic rocks which exhibit smooth chemical continuity are classified as basalt, andesite and minor dacite basedmainly on immobile trace element concentrations (Ti, Zr, Y, Nb, La, Ce). The hypabyssal rocks are gabbro andplagiogranite. The immobile trace and some major element chemistry of the Poluşağı magmatic rocks clearly demonstrates that the rock suite is typically tholeiitic The Poluşağı tholeiitic basalts and gabbros exhibit chemical characteristics of oceanic tholeiites as well as island arc tholeiites- The less differentiated basalts and gabbros are chemically more akin to oceanic tholeiites and the more evolved basalts and gabbros to island arc tholeiites.Geochemical and geological considerations lead to the conclusion that the Poluşağı rock suite was produced duringthe initial stages of an ensimatic immature island arc volcanism developed on the oceanic crust of the Middle Eocene Maden Marginal Basin located probably to the north of the Pütürge Massif.

  • limestone

  • calc-schist

  • agglomerate

  • Malatya

  • Baker. P.E-, 1968, Comparative volcanology and petrology of the Atlantic island-arcs: Bull- Volcanol-, 32, 189- 209.

  • Beccaluva, L-, Ohnenstetter, O- ve Ohnenstetter, M-, 1979, Geochemical discrimination between ocean-floor and islandarc tholeiites - application to some ophiolites. Can- J. Earth Sci., 16, 1874-1882.

  • Beccaluva, L., Ohnenstetter, D., Ohnenstetter, M. ve Venturelli, G-, 1977, The trace element geochemistry of Corsican ophiolites: Contrib- Mineral- Petrol-. 64, 11- 31.

  • Bickle, M-J- ve Nisbet, E-, 1972. TThe oceanic afinities of some alpine mafic rocks based on their Ti-ZrY contents: Jl- Geol- Soc, 128. 267-271.

  • Brunn, J-H-, 1983. Oceans, continents and orogens. Tectonophysics, 99, 1-29-

  • Carmichael, LS-E-, Turner, F-J- ve Verhoogen, J-, 1974, Igneous Petrology: McGraw Hill, N-Y-, 739 s

  • Church, W-R. ve Coish, R-A-, 1976, Oceanic versus island arc orighin of ophiolites: Earth and Planet, Sci- Lett-. 31, 8-14

  • Coats, R.R., 1968, Basaltic andesites: de: HH. Hess ve A. Poldervaart (Ld.), Basalts, 2, Interscience, N-Y-. 689- 736-

  • Coleman. R-G-, 1977, Ophiolites-Ancient oceanic lithosplıere?: Minerals and Rocks. No. 12, Springer-Veriag, 229 s.

  • Coleman. R-G- ve Peterman, Z-E-, 1975, Oceanic plagiogranite: J. Geophys. Res-, 80, 1099-1108

  • Dewey, J-F-, 1974, Continental margins and ophiolite obduction. Appalachian Caledonian system: de: C-A. Burk ve CL- Drake (Ed), The geology of continental margins. N.Y., Springer, 933-950

  • Dewey, J-F-, 1976, Ancient plate margins-some observavations: Tectonophysies, 33, 379-385

  • Dewey, J-F- ve Bird, J.M-. 1971, Origin and emplacement of the ophiolitic suite; Appalachian ophiolites in Newfoundland: J- Geophys. Res., 76, 3179-3206.

  • Engel, CF- ve Fisher, R.L, 1975, Granitic to ultramafic rock complexes of the Indian Ocean ridge system, western Indian Ocean: GeoL Surv. Am. Bull-, 86, 1553-1578

  • Erdoğan, B., 1977, Geology, geochemistry and genesis of the sulphide deposits of the Ergani-Maden region. SE Turkey: Yayımlanmamış doktora tezi, New Brunswick Üniversitesi, Kanada- 288 s.

  • Erdoğan, B-, 1982, Ergani-Maden yöresindeki Güneydoğu Anadolu Ofiyolit Kuşağının jeolojisi ve volkanik kayaları: Türkiye Jeol- Kur- Bült-, 25, 49-59

  • Ewart, A- ve Bryan, W-B-, 1972, Petrology and geochemistry of the igneous rocks from Eua, Tongan islands. GeolSoc Am- Bull-, 83. 3281-3298

  • Floyd, P-A- ve Winchester, J-A-. 1975, Magma type and tectonic setting discrimination using immobile elements: Earth and Planet, Sci- Lett-, 27, 211-218.

  • Floyd. P-A- ve Winschester, J-A-. 1978, Identification and discrimination of altered and metamorphosed volcanic rocks using immobile elements: Chem- Geol-. 21. 291-306

  • Gill, J-B;, 1970, Geochemistry of Viti Levu, Fiji, and its evolution as an island arc: Contr- Mineral- Petrol. 27, 179- 203.

  • Hawkins, J-W-, 1976, Petrology and geochemistry of basaltic rocks of the Lau Basin: Earth and Planet- Sci- Lett-, 28, 283-297

  • Hawkins, J.W-, 1980. Petrology of back-arc basins and island-arcs: their possible role in the origin of ophiolites: de A. Panayiotou (Ed), Ophiolites. proceedings of international ophiolite symposium, Cyprus. Minist. Agric- Nat. Resour- Geol. Surv. Dept. Nicosia, Cyprus, 244-254.

  • Hempton, M.R.. 1984, Results of detailed mapping, near Lake Hazar, Eastern Taurus mountains: de: O. Tekeli ve M.C Göncüoğlu (Ed-). Geology of Taurus BeltProceedings Int. Symp. Geol. Taurus belt, 26-29 Sept1983. Ankara. Turkey, 223-228

  • Irvine, T-N- ve Baragar. W-R-A-, 1971, A guide to the chemical classification of the common volcanic rocks: Can- J. Earth Sci, 8. 523-548-

  • îleri, S-, Salancı, B-, Bitem, M- ve Doğan. R-, 1976, Ergani (Maden) bakır yatağı ve plaka tektoniği: Bült, 19, 133 -142,

  • Jakes. P- ve Gill, J-, 1970. Rare earth elements and the island arc tholeiitic series. Earth and Planet. Sci- Lett-, 9, 17-28-

  • Jakes, P. ve White, A.J.R., 1972, Major and trace element abundances in volcanic rocks of orogenic areas: GeolSoc Am- Bull-, 83, 29-40

  • Jensen, L-S-, 1976, A new cation plot for classifying subalkaliç volcanic rocks: Ontario Dep. Mines-, Misc-, Paper, 66, 22 s

  • Karig, D|.E-, 1971, Origin and development of marginal basins in the western Pacific: J- Geophys- Res-, 76, 2542- 2561

  • Karslıoğlu, Y-. 1978, Malatya ili, Pütürge ilçesi, Poluşağı bakır sahasına ait jeoloji raporu: Yayımlanmamış rapor. MTA Arş. No: 1742. 14 s

  • Kuno, H-, 1960, High alumina basalt- J. Petrol. 1, 121-145-

  • Kuno, H-, 1965, Fractionnation trends of basalt magmas in lava flows: J. Petrol, 6, 302-321-

  • Kuno, H-, 1968, Differentiation of basaltic magmas: de: HH. Hess ve A- Poldervaart (Ed-), Basalts, 2, Interscience, N-Y-, 623-688

  • Kushiro, I-, 1979, Fractional crystallisation of basaltic magma-, de: H.S. Yoder Jnr- (Ed-), The evolution of igneous rocks, 50 th arm- perspectives, Princeton Univ. Press, N-Y-, 171-204.

  • Laurent, R-, Delaloye. M-, Vaugnat, M. ve Wagner, J-J-, 1980, Composition of parental basaltic magma in ophiolites: de. A. Panayiotou (Ed), Ophiolites: proceedings of international ophiolite symposium. SyprusMinist- Agric- Nat. Resour. GeoL Surv. Dept-, Nicosia, Cyprus. 172-181-

  • Mac Donald. GA-. 1968. Composition and origin of Hawiian lavas: Geol. Soc- Am- Mem-, 116. 477-522

  • Mac Donald, G-A- ve Katsura, T-, 1964, Chemical composition of Hawaiian lavas: J- Petr-, 5. 82-133-

  • Manşon, P-, 1968, Geochemistry of basaltic rocks: Major elements: de: H-H. Hess ve A. Poldervaart (Ed-), Basalts, 2, Interscience, N-Y-, 215-269

  • Michard, A-, Whitechurch, H-, Ricou, L.E-. Montigny, R. ve Yazgan, A-, 1982, Tauric subduction (Malatya-Elazig provinces) and its bearing on tectonics of the Tethyan Realm in Turkey. Paper presented at the symposium on the Geological evolution of the Eastern Mediterranean, Sept- 1982, Edinburgh.

  • Mitchell, A-H-, ve Reading, H.G., 1971, Evolution of island arcs: J. Geol.. 79, 253-284

  • Miyashiro, A., 1973. The Troodos ophiolite complex was probably formed in an island arc: Earth and Planet. Sci. Lett-, 19, 218-224.

  • Miyashiro, A-, 1974, Volcanic rocks series in island arcs and active continental margins: Am- J. Sci-, 274, 321-355

  • Miyashiro, A- 1975, Classification, characteristics and origin of ophiolites: J- Geol-, 83, 249-281

  • Miyashiro, A. ve Shido, F-, 1975, Tholeiitic and calc-alkaline series in relation to the behaviours of titanium, vanadium, chromium and nickel: Am. J- Sci-. 275. 265-277

  • Özçelik, M-, 1982, The petrology and geochemistry of volcanic rocks and associated sulphide deposits of the S-E- Anatolian ophiolite belt, near Malatya, Turkey: Yayımlanmamış doktora tezi- Durham Univ. İngiltere, 453 s-

  • Özçelik. M., 1984 a, Maden volkanizmasma ait Poluşağı toleyitik kayaç topluluğunun oluştuğu tektonik ortam T.J-K. 38- Bilim. Tekn. Kurult- bildiri özetleri, 62-63

  • Özçelik, M-, 1984 b. Düşük dereceli ayrışma koşullarında element hareketlenmesi ve jeokimyasal verilerin kullanımı: T.J.K. 38- Bilim. Tekn. Kurult, bildiri özetleri, 85-86.

  • Pearce, J-A., 1975, Basalt geochemistry used to investigate past tectonic environments on Cyprus: Tectonophysics, 25. 41-67

  • Pearce, JA-, 1980, Geochemical evidence for the genesis and eruptive setting of lavas from Tethyan ophiolites: de: A. Panayiotou (Ed), Ophiolaites: proceedings of international ophiolite symposium, Cyprus- Minist. Agric. Nat- Resour- Geol- Surv- Dept. Nicosia, Cyprus261-272

  • Pearce, J-A- ve Cann-, J-R-, 1971, Ophiolite origin investigated by discriminant analysis using Ti, Zr and Y: Earth and Planet. Sci- Lett., 12, 339-349

  • Pearce, J-A- ve Cann J-R-, 1973, Tectonic setting of basic volcanic rocks determined using trace element analysis.e Earth and Planet. Sci. Lett-, 19, 290-300

  • Pearce, JA- ve Gale, G-H-, 1977, Identification of ore-depositon environment from trace element geochemistry of associated igneous host rocks: Geol. Soc- LondSpec. Pub-, 7, 14-24

  • Perinçek, D-, 1979, Interrelations of the Arab and Anatolian plates: «Guide Book, Excursion B», First Geol. Congr. Middle East, Ankara. 34 s

  • Perinçek, D. ve Özkaya L, 1981, Arabistan levhası kuzey kenarı tektonik evrimi: Yerbilimleri, 8, 91-101.

  • Prinz., M-, 1968, Geochemistry of basaltic rocks: trace elements: de: H-H. Hess ve A- Poldervaart (Ed), Basalts, 1, Interscience, N.Y., 271-323

  • Saunders, A.Ü-, Tarney, J-, Stern, CR. ve Dalziel, I-W-D-, 1979, Geochemistry of Mesozoic marginal basin floor igneous rocks from Southern Chile. Geol. Soc- AmBull, part 1, 90, 237-258

  • Saunders, A-D-, Tarney, J-, Marsh, NG- ve Wood, D-A-, 1980, Ophiolites as ocean crust or marginal basin crust; A geochemical approach: de: A- Panayiotou (Ed), Ophiolites: proceedings of international ophiolite symposium, Cyprus- Minist. Agric- Nat- Resour. Geol. Surv- Dept-, Nicosia, Cyprus, 193-204.

  • Smith, R-E- ve Smith, SE-, 1976, Comments on the use of Ti, Zr, Y, Sr, K, P and Nb in the classification of basaltic magmas: Earth and Planet- Sci- Lett-, 32, 114- 120-

  • Spooner, E.T.C-, 1976, The strontium isotopic composition of seawater and seawater-oceanic crust interaction: Earth and Planet. Sci. Lett-, 31, 167-174

  • Şengör, A.M.C ve Yılmaz, Y-, 1981. Tethyan evolution of Turkey, A plate tectonic approach: Tectonophysics, 75, 181-241.

  • Upadhyay, ED. ve Neale, E-R.W-, 1979, On the tectonic regimes of ophiolite genesis: Earth and Planet- Sci. Lett-, 43, 93-102

  • Winchester, J-A- ve Floyd, P-A-, 1977, Geochemical discrimination of different magma series and their differentiation products using immobile elements: ChemGeol., 20, 325-343

  • Yazgan, E-, 1972, Etude geologique et petrographique du complexe ophiolitique de la region situee au sud-est de Malatya (Taurus oriental, Turquie) et de sa couverture volcanosedimentaire: These no: 1575, Univ. Geneve- 236 s

  • Yazgan, E., 1981, Doğu Toroslar`da etkin bir paleo-kıta kenarı etüdü (Üst Kretase-Orta Eosen) Malatya-Elazığ, Doğu Anadolu: Yerbilimleri, 7, 83-104.

  • Yazgan, E-, 1983. A geotraverse between the Arabian Platform and the Munzur Nappes: Int. Symp. Geol. Taurus Belt, 26-29 Sept-, Ankara, Guide Book for Excursion V.

  • Yazgan, E., 1984, Geodynamic evolution of the Eastern Taurus (Malatya-Elazığ area, Turkey). O. Tekeli ve MC Göncüoğlu (Ed), Geology of Taurus Belt-, Proceedings Int. Symp. Geol. Taurus Belt, 26-29 Sept-. 1983, Ankara, Turkey, 199-208-

  • Yazgan, E-, Michard, A-, Whitechurch, H. ve Montigny, R-, 1983, Le Taurus de Malatya (Turquie orientale), element de la suture sud tethysienne: Bull- Soc geol. France, no: 1, 59-69

  • Pb-Zn Occurrences of the Göktepe (Ermenek-Konya) District
    Mustafa Kuşcu
    View as PDF

    Abstract: The Alanya Unit, Muzvadi complex slice and the Aladağ Unit occur in the study area which are formedin different environmental conditions- The ore occurrences are divided in two groups on the base of their mineralparagenesis, alterations, stratigraphic and geographic positions- These are the Northern Pb-Zn occurrences (Sarıpınar) and the Southern Pb-Zn occurrences (Muzvadi-Berem).The Northern occurrences are found in the Mizzia bearing limestones of Upper Permian Dumlugöze Formation andin the oolitic-stromatolitic [limestones of Lower-Middle Triassic Haydar Formation and also along the contacts of bothformations. The ores occur mostly as veins and in some cases as stratabound lensesThe Southern occurrences in the Muzvadi area are found in the Jurassic Akpmar dolomitic limestones as stockworktype mineralization. In the Berem area, however, the mineralization is situated in the brecciated and fractured zonesof Jurassic, Upper Triassic and Permian formations of the Aladağ Unit.The ores of the Southern part do not contain fluorite minerals while the ores of the Northern part are rich in fluorite.The ore deposits consist of primary sulfide minerals of sphalerite, galena, pyrite, marcasite, and secondary mineralsof dolomite, fluorite, calcite, quartz, barite, smithsonite, cerussite, hydrozincite and limonite. The Pb-Zn deposits arecommonly related to the, NW-SE and NE-SW striking tectonic lines, and were formed after the emplacement of theabove mentioned unitsA magmatic-hydrothermal origin for the Pb-Zn mineralization seems unlikely. Field and laboratuary observationsindicate an epigenetic character for the lead-zinc deposits- The lead-zinc ores were formed either by the formationwaters, by the concentration of ore-forming elements which were primarily dispersed in sedimentary rocks- bymeteoric waters, ground waters. These concentrated elements then migrated and precicpitated in the fracturedzones and open spaces of the various units.

  • fluorite

  • brec

  • pyrite

  • dolomite

  • Konya

  • Ayhan, A-, 1982, Burhan Mahallesi-Yuları köyü arasında bulunan galenitli barit yatakları (Gazipaşa-Antalya): Türkiye Jeol- Kur. Bült, 25-2, 105-116

  • Blumenthal, M- M-, 1951. Batı Toroslar`da Alanya ard ülkesinde jeolojik araştırmalar: MTA Yayını, Seri D, 5, 135 s

  • Blumenthal- M. M., 1952, Das taurische Hochgebirge des Aladağ, neuer e Forschungen zur seiner Geographic Stratigraphie und Tektonik: MTA Yayını, Seri D, 6, 136 s

  • Brown, J. S., 1970, Mississippi Valley type lead-zinc ores: Min. Deposita, 5, 103-109

  • Brunn, J. H., Argyriadis, L, Marcoux, J., Monod, O-, Poisson, A. ve Ricou, L-, 1973, 50- Yıl Yerbilimleri kongresi, 58-69 s

  • Bürküt, Y., 1979, Uygulamalı Jeokimya: İTÜ Yayını, İstanbul, 236 s

  • Craig. J. R- ve Vaughan, D- J-, 1981, Ore microscopy and petrography: Willey-Interscience Publication, New York, 259-265

  • Demirtaşlı, E., Gedik, 1- ve İmik, M., 1978, Ermenek batısında Göktepe-Dumlugöze ve Tepebaşı arasında kalan sahanın jeolojisi: Türkiye Jeol. Kur- Bildiri özetleri, 9 s

  • Gedik, A-, Birgili, S., Yılmaz, Y. ve Yoldaş, R.. 1979, MutErmenek-Silifke yöresinin jeolojisi ve petrol olanakları: Türkiye Jeol. Kur. Bült, 22, 7-26.

  • İnan, A- ve Uğur, M-, 1981, Konya-Hadim (Kızılgeriş)-Bozkır (Küçüksu) ve Antalya-Gazipaşa (Muzvadi-Berem) yörelerindeki çinko-kurşun cevherleşmelerine ait jeoloji raporu: MTA Enst, Maden Etüd Rp-, 1754, 56 s, yayımlanmamış.

  • Kuşçu, M-, 1983. Göktepe-Ermenek (Konya) yöresinin jeolojisi ve Pb-Zn yatakları: Doktora tezi (Yayımlanmamış), Selçuk Univ., 181 s.

  • Kuşçu- M-, 1984, Göktepe (Ermenek-Konya) kuzey kesimi Pb-Zn zuhurlarmdaki floritlerin Y (yitriyum) içerikleri; Türkiye Jeol. Kur. Bült, 27, 57-60-

  • Özgül, N-, 1971, Orta Toroslar`m kuzey kesiminin yapısal gelişiminde blok hareketlerin önemi: Türkiye Jeol. Kur- Bült- 14, 85-101.

  • Özgül, N., 1976, Toroslar`m bazı temel jeoloji özellikleri: Türkiye Jeol. Kur. Bült, 19, 65-78.

  • Ramdohr, P-, 1975, Die Erzmineralien und ihre Verwachsungen: Akademie-Verlag, Berlin, 1277 s

  • Sangster, D. F-, 1976. Carbonate hosted lead-zinc deposits; K.H. Wolf-, (ed), Handbook of Stratabound and Stratiform Ore Deposits`de: Elsevier, Amsterdam-Oxford-New York, 6, 447-456.

  • Stanton, R. L., 1972, Some stratabound ores of sedimantary affilation: Ore Petrology, Mcgraw-Hill, New York, 541-551.

  • Şengün, M-, Acarlar, M., Çetin, F-, Doğan, Z. ve Gök, A-, 1978, Alanya masifinin yapısal sorunu: Jeoloji Müh. Derg-, 6, 39-44.

  • Wedepohl, K. H-, 1970, Zinc: Handbook of Geochemistry,Springer, Berlin, 11/2, 30 s.

  • Wedepohl, K. H-, 1972, Lead: Handbook of Geochemistry. Springer, Berlin, 82, ill s.

  • Ziegler, K. G. J-, 1938, Montangeologische Untersuchungen im Westlichen Taurus: Teil I; Ubersicht der geologischen wahrnehmungen im gebiet des westlichen Taurus-Unveröff. Ber-, MTA Yayını, 953, s.

  • Odontological Variations of the Hipparion Vertebrate Fauna in Kemiklitepe (Uşak-Eşme)
    Vahdet Tuna
    View as PDF

    Abstract: In this research, the odontology of hipparion found in Kemiklitepe vertebrate fauna bas been studiedand as a result of odontologic and biometric observations Hipparion matthewi Abel and Hipparion sp. are identified.From the faunal evidence and hipparion teeth it can be concluded that some dispersed savannah and lacustrinefluvial environments along with forests existed in the region- The corresponding time interval of the biozone isthought to be late Vallesian-early Turolian. 

  • Hipparion

  • savannah

  • lacustrine

  • fluvial

  • Uşak

  • Abel, O-, 1926, Die Geschicte der Equiden auf dem Boden Nord-Amerikas: Verh- Zool- Bot- Ges-, Wien, 74, 150- 164

  • Crusafont Pairo, M-, 1957, Los Girafidos fosiles de Eşme (Anatolia): -Nota preliminar- -Curs- y Conf-, 4: 80-81

  • Ercan, T-, Dinçel, T-, Metin, S-, Türkecan, A., Günay, E-, 1978, Uşak yöresindeki Neojen havzalarının jeolojisi: Türkiye JeoL Kur. Bült-, 21, 2, 97-107.

  • Forsten, A. M-, 1968, Revision of the Palearctic Hipparion. Açta Zool- Fennica, 119, 53

  • Ginsburg, L., 1968, L; evolution du climat au cours du Miocene en France: 1-5

  • Gromova, V-, 1952, Le genre Hipparion: Trav. Inst. Paleont. Acad- Sci- URSS, 36, 231

  • Matthew, W. D., 1926, The evolution of the horses: Quart. Rev- Biol-, 1 (2), 139-185.

  • Ozansoy, F-, 1957, Türkiye Tersiyer Memeli Faunaları ve Stratigrafik Revizyonları: MTA Ensts. Dergisi No: 49.

  • Ozansoy, F-,1961, Hyaena şenyüreki OZANSOY du Pliocene superieur (Sinap moyen) et la repartition verticale du genre Hyaena dans le systeme Pliocene de Turquie

  • Ozansoy, F-,1969, Ege Fosil Omurgalı Faunaları ve Hipparion`lu Faunaların dikey yayılımi: MTA Enstitüsü Dergisi No. 72.

  • Sickenberg, O-, Becker-Platen, J. D., Benda, L., Berg, DEngesser, B., Gaziry, W., Heissig, K-, Hunermann, K. A-, Sondaar, P- Y-, Schmitt-Kittler, N., Staesche, U-, Steffens, P-, Tobien, H., 1975, Die Gliederung des höheren Junteriârs und Altquartars in der Türkei nach ertebraten und ihre Bedeutung für die internationale Neogen-Stratigraphie: Geol- Jb-, B 15, 30-63-

  • Sondaar, P. Y., 1971, The Samos Hipparion I, II: Kon. NedAkad. Wet B, 74, 4, 417-441.

  • Staesche, U- ve Sondaar, P. Y., 1979, Hipparion aus dem Vallesium und Turolium (Jungstertiar) der Türkei: Geol- Jb- B 33, 35-79-

  • Şen, Ş-, Sondaar, P. Y., Staesche. U-, 1978, The biostratigrayhical applications of the genus Hipparion with special references to the Turkish representatives: Proc. Kon- Ned. Akad. Wet-, B, 81 (3), 370-385.

  • Tobien, H., 1938, Über das Gebiss des Hipparion matthewi Abel: Sonder?Abdruck aus dem Neues Jahrbuch fur Mineralogie etc Beil. Bd. 80. Abt- 3, 279-306.

  • Viret. J-, 1958, Perissodactyla. Trait`e de Paleontologie, VI. 2, 368-475,

  • Wehrli, H-, 1941, Beitrag zur Kenntnis der Hipparionen von Samos: Pal. Zeitschr, Bd. 22, 321-386.

  • Yalçınlar, I-, 1946, Eşme civarında Miyosen`e ait bir omurgalılar faunası: İ-Ü-FF. Mec- B XI, 2, 124-129.

  • Yalçınlar, I-,1954, Les gisements de Mammiferes et d`autres Vertebres cossiles de la Turquie. -Cong- geol. int- Alger 1952, C-R. 19. Sess-, Sect. 13, 15: 139-147, 1 Abb.

  • Geochemistry of the Neogene Volcanics Around Ankara
    Ayla Tankut
    View as PDF

    Abstract: The Neogene volcanics occur in four main areas around Ankara- Petrochemical characteristics of therocks revealed that i) the intermediate-acidic rocks show calcalkaline affinity whereas ii) the mafic rocks showalkaline affinity.The calk-alkaline group contains hornblende, biotite, pyroxene and andesine as phenoeryst phases- Major elementchemistry of some of the rocks is similar to that of the Andean type continental margin volcanics. However ,thehigh incompatible trace element contents (Rb, Nb, Zr, Y) are not comparable with those of the Andean type.The mafic rocks contain phenoeryst of clinopyroxene with  without olivine, and lack the orthorombic pyroxene.The intermediate members of this group also contain hornblende and plagioclase as phenocrysts. Olivine is dominantlypresent in the normative composition of the rocks together with either nepheline hypersthene. The mafic volcanics have been classified, in terms of the mojor and immobile trace element (Ti, Zr, Y, Nb) abundances in two groups as alkaline basalts and shoshonites- The Zr and Y contents of both group of rocks suggest a within-platetectonic setting, for the mafic volcanics around Ankara

  • biotite

  • pyroxene

  • clinopyroxene

  • Ankara

  • Ach, J.A-, 1982, The Geochemistry of the Ankara Volcanics. Central Turkey, (Abstract): EOS, Transactions, American Geophysical Union, 63-45, 148

  • Best. M.G. ve Brimhall, W.H.. 1974, Late Cenozoic alkalic basaltic magmas in the western Colorado Plateaus and the Basin and Range Transition Zone, U.S.A.,and their bearing on mantle dynamics: Geol. Soc America Bull-, 85, 1677-1690.

  • Borsi, S. F-, Innocenti, F- ve Mazuoli, 1972, Geochronology and Petrology of recent volcanics in the Eastern Aegean Sea. Bull- Volcanol-, 36, 473-496.

  • Chaput, E-, 1931, Ankara mıntıkasının 1/135-000 mikyasında jeoloji haritasına dair izahat: 1st- öarülf. GeolEnst-, 7, istanbu

  • Chayes, F., 1966, Alkaline and Subalkaline basalts: AmJour. Sci-, 264, 128-145.

  • Çalgın, R., Ercan, T., Pehlivanoğlu, H-, Şengün, M-, 1973, Ankara çevresi jeolojisi: MTA- Enst., rapor no 6487 (yayımlanmamış) •

  • Ercan, T-, Dinçel A., ve Günay, E-, 1979, Uşak volkanitlerinin petrolojisi ve plaka tektoniği açısından, Ege bölgesindeki yeri: Türkiye Jeol- Kur. Bült, 22, 185-198

  • Erol, O-, 1961, Ankara bölgesinin tektonik gelişmesi: Türkiye Jeol- Kur. Bült, 7-2, 57-58.

  • Ewart, A-, Baxter, K. ve Ross, J. A-, 1980, The petrology and petrogenesis of The Tertiary anorogenic mafic lavas of southern and central Queensland, Australiapossible implications for crustal thickening: Contrib. Mineral- Petrol-, 75, 129-152

  • Irvine, T-N. ve Baragar, W-R-A-, 1971, A guide to chemical classification of the common volcanic rocks. CanJ. Earth Sci. 8, 523-548

  • Jakes, P- ve White, AJ-R-, 1972, Major and trace element abundances in volcanic rocks of orogenic areas: Geol. Soc. of America Bull-, 83, 29-40.

  • Kolios, N-, Innocenti, F. Manetti, P., Peccerillo, A., Guiliani. O-, 1980, The Pliocene volcanism of the Voras Mts (Central Macedonia, Greece), Bull- Volcanol-, 43-3, 553-568

  • Lahn, E-, 1945, Anadoluda Neojen ve 4`cü zaman nizması Coğrafya Dergisi, 3, 7-8

  • Leake, B-E-, Hendry, G-L-, Kemp, A-, Plant, A-G-. Harvey, P.K-, Wilson, J.R-, Coats, J-S-, Aucott, J.W., Lunel, T-, 1970, The Chemical Analysis of Rock Powders by Automatic X-Ray Fluorescence: Chemical Geology, 5, 7-86.

  • Leonhard, R-, 1902, Geologische Skizze der galatischen andesit gebietes nörlich von Angoras: E- Schweizertsche Verlagshandlung Stuttgart (E- O. Neagle)

  • MacDonald, G-A. ve Katsura, T-, 1964, Chemical composition of Hawaiian Lavas: J. Petrology, 5, 82-133.

  • Norrish, K. ve Hutton, J-T., 1969, An accurate X-ray spectrographic method for the analysis of a wide range of geologic samples: Geochim- et Cosmochim- Acta, 33, 431-453-

  • Pearce, J.A-, 1976, Statistical analysis of major element pattern in basalts: J. Petr., 17, 15-43

  • Pearce, JA. ve Norry, M-J-, 1979, Petrogenetic implications of Ti, Zr, Y and Nb variations in volcanic rocks. Contrib- Min. Petr-, 69, 33-47-

  • Peccerillo, A- ve Taylor, S-R-, 1976, Geochemistry of Eocene calc-alkaline volcanic rocks from Kastamonu area. Turkey: Contir. Miner. Petrol-, 68, 63-81

  • Savaşçın, MY-, 1982, Batı Anadolu Neojen magmatizmasının yapısal ve petrografik öğeleri: Batı Anadolunun genç tektoniği ve magmatizması paneli, T-J-K-, 1982, 22-38

  • Şengör, A.M-C. 1980, Türkiye`nin neotektoniğinin esasları: TJ.K. Konferans serileri, 52.

  • Vail, JR., Hornung, G. ve Cox, K.G., 1969, Karroo basalts of the Tuli Syncline, Rhodesia: Bull- Volcand. 33. 398

  • Wincshester, J-A- ve Floyd, P-A., 1977, Geochemical discrimination of different magma series and their differentiation products using immobile elements: ChemGeol-, 20, 325-343.

  • Wright, JB-, 1963, A note on possible differentiation trends in Tertiary to Recent lavas of Kenya: Geol. Mag-, 100, 164-180-

  • Yoder, H-S. Jr. ve Tilley, CE-, 1962, Origin of basalt magmas, An experimental study of natural and synthetic rock systems: Jour- Petrology. 3, 342-532.

  • Karayazı Fault
    Ali Koçyiğit
    View as PDF

    Abstract: A fault observed starting from the south of the Tutak town to the Santas village to the northwestextending in N65°W direction for 80-85 km has been detected and named as the Karayazı Fault- Some field evidencessuch as the juxtaposition of the older and younger rock units, the topographic expression, the drainage patternofwaters, aligned springs and the ruins of an ancient settlement observed along the fault zone have been attributedto the fact that the Karayazı Fault may be active.

  • Karayazı Fault

  • stream

  • Tutak

  • Arpat, E-, Şaroğlu, F. ve İz, H-B-, 1977, 1976 Çaldıran depremi: Yeryuvarı ve İnsan, 2, 1, 29-41.

  • Erentöz, C, 1954, Oltu 31/4, Kars 32/3 ve Hasankale 48/2 1/100000 ölçekli jeolojik paftalara ait Memuar: Maden Tetkik ve Arama Genel Müdürlüğü, Der- RapNo. 2159, 38 s

  • İlker, S-, 1966, Erzurum Bölgesinde Erzurum Î47-Cİ. İ47-c4, Î47-d2 ve Î47-d3 paftalarının detay petrol etüdü hakkında rapor: Maden Tetkik ve Arama Genel Müdürlüğü, Der. Rap- No- 4236.

  • Koçyiğit, A., 1983, Doğu Anadolu Bölgesi`nin depremselliği ve gerekli çalışmalar: Yeryuvarı ve İnsan, 8, 3, 25-29.

  • Koçyiğit, A-, 1984, Güneybatı Türkiye ve yakın dolayında levha içi yeni tektonik gelişim: Türkiye Jeol- KurBült, 27, 1, 1-15-

  • Le Pichon, X., Francheteau, J- ve Bonnin- j-, 1973, Plate tectonics: Developments in geotectonics. Elsevier, Amsterdam, 300 p

  • Me Kenzie, DP., 1972, Active tectonics of the Mediterranean region: Geophys- J-R- Astr- Soc, 30, 109-185

  • Morelli, C-, 1978, Eastern Mediterranean, geophysical results and implications: Tectonophysics 46, 333-346.

  • Rathur, A.Q., 1969, Pasinler-Horasan (Erzurum) sahasına ait genel jeolojik rapor: Maden Tetkik ve Arama Genel Müdürlüğü, Der. Rap-, No. 52, 66 s

  • Şaroğlu, F. ve Güner, Y-, 1979, Tutak Diri Fayı, Özellikleri ve Çaldıran Fayı ile ilişkisi: Yeryuvarı ve İnsan, 4, 1, 11-14.

  • ISSUE FULL FILE
    View as PDF