Jeoloji Münendisliği Dergisi
Jeoloji Mühendisliği Dergisi

Jeoloji Mühendisliği Dergisi

1984 OCAK
COVER
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COPYRİHT PAGE
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CONTENTS
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TO OUR READERS
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Geology of the Göksün « Af şin « Elbistan Region
Niyazi Tarhan
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ABBTBACT: In the »tûdy aıea two aUoobthonoui unit» are identiffed, One »erf these unit*; Çardak «nitemplaned before Cainpamien» conal»te of Göksün MetaopWolites, Kabaktepe I etani(*ri>hics ^d Acidic Ininisi.«Miü respectivöly, iğde Unit ©mplaeed in the region during the Lower and Middle Eocene consists ofGaf ilhan MetamorpMos and! Andırın Group yqcks,Along the Göksün vafcy, an ophîöüte assemblage developed In the Upper Portlandian-Lovvor Berriasian,erojm out. They pre^rve their primary sequential features In üpite «>£ an totonse tectonic deformation,This sequence, comprising gabbro, sheeted dyke complex, vol< imo-sedimentiiry rocks and deep seapelagic seÄnents from bottom to top, had been called and defined m Ookwim Metaophlolite,The Kabaktepe MetamorpMcs, which are probably «of Devonian age, constitute a metomofphics nappeenver on tte Göksün M*Uaophio1ïte, Bath of mme two units are cut by the Senontan (Conİasİan-SantoııİLin)a©Mlc intrusions,TOe Ereene f ornmtton of Campanlan = Maastrlcttan age and the Upper PaJeocene.IiDWër Eocene Fındıkformation, which te gradational to tiie former, overMe the Çardak Unit wltii an angular unconformity.In the studied a^ea. the Middle Eocene Ballıkısık, Miocene Salyan fomiations and flue - and coarsegrained Fecent deposits unoiwfnformably overEe allochthonous units and older formations

  • Göksun-Afşin-Elbistan

  • Allochthonous

  • Ophiolite Community

  • Metaophiolite


  • AKKOCA, A,B. ve BAHÇECİ, A., 1972, Beritdafı ve yöresindeki demir prospeksiyonunun jeolojik raporu: Maden Tetkik ve Arama Enst. Derleme Rap, No. 5001, Ankara (yayınlanmamıştır).

  • ATASEVEE, İ, 1978 a, K. Maraş - Elbistan Çakçakder© ve Arpacık T, demir zuhurları jeoloji raporu: Maden Tetkik ve Arama Enst, Derleme Rap, Noa 6804, Ankara (yayınlanmamış).

  • ATASEVER, î.f İ978 b, K. Maraş . Elbistan - Çardak - Mendikli _ Haveılar demir zuhurları raporu: Maden Tetkik ve Arama Enst. Derleme Rap. No. 6633, Ankara/(yayınlanmamış).

  • BAYKAL, F., 1961, Malatya - Darende Gürün :bölge- sindeki yeşil sahrelerle sediment kayaçlar arasındaki ilişki: Maden Tetkik ve Arama Enst, Derleme Bap. No, 3806, Ankara (yayınîaıımamı§)

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  • ERDOĞAN, T., 1975, Geology of Gölbaşı région, TPAO unpublished report 229, Ankara (yayinianmami§)

  • FOURQUtN, G,, WHÎTEOHURCH», H, ve JUTEAU, T,, 1983, Toros ofiyolitlerinde okyanus içi olaylar ve Pomtid etkin kenarındaki mafmatik işlev: benzerlikleri ve önemi: Yeryuvarı ve insan, cilt: 8, sayı: l, Ankara,

  • GÖKAİ4P, E,, 1972, Elbistan « Cela içmeleri jeoloji - hidroloji etüdü raporu: Maden Tetkik ve Arama Enst. Derleme Bap, No, 5827, Ankara (yaymlaııınamı§),

  • GÖNCÜOĞLU, M,C,f ve TURHAN, N.f 1983, Bitlis metamorfitlerinde yeni ya§ bulguları: Maden Tetkik ve Arama Enst, Dergi No, 95/96, Ankara,

  • HATAY, N,, 1966f K, Mams. . Göksün - Elbistan bök gesi diasporit prospeksiyonu raporu: Maden Tetkik ve Arama Enst, Derleme Rap, No, 8S52, Ankara ( y ayınlanmami| ),

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  • Tarhan, N . (1984). Göksün - Afşin - Elbistan Dolayının Jeolojisi . Jeoloji Mühendisliği Dergisi , 8 (1) , 3-10 . Retrieved from https://dergipark.org.tr/tr/pub/jmd/issue/28444/301887

  • Tarhan, N . Göksün - Afşin - Elbistan Dolayının Jeolojisi. Jeoloji Mühendisliği Dergisi 8 (1984 ): 3-10

  • Relations between the meiamorphism and deformation in the southern margin of the Bitlis Massif (Lice-Kulp district, Diyarbakır Province^ SE Turkey)
    Salim Genç
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    ABSTRACT: The I Joe-Kulp area comprises FYë-Permian basement and rormian niotamor|»hiTerttary se^mentary and ignamis rock^. The Permiaıı rast with an angular imeonflarmity em the Pre-Permian nietamorphics (basement rocks), The basement rocks have been metamorphosşcl at least twice am! as a whole the area haa undergone polyphase deformation« During the first episode of deformation, which Is older than the Permian, a distinct élevage structure In the basement rooks was developed and at the same Mme an amphlbollte fades metatnorphfsm occurred. Folds plunging evidently NW and NE respectively are observed in the basement metamorphlcs and Miocene (Tertiary) segmente. These folds were presumably formed as a result of two distinct deformation phases(D^ ani &3 ) and thus during Post=»flocene periods auiilorni and synform In the ba«emeat rooks, and an tie I ine and synoMne structures 1m the Miocene sediments were developed. Later a second episode of metamorphÉMn (greenschlst faeies niotamorpliism) and faulting) to»k plam and beeauëe of ttilfe low grade nietamorphism the basement rocks were extensively

  • Bitlis Massif

  • Metamorphism

  • Lice-Kulp(Diyarbakır)

  • Deformation


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  • Helvacı, C . (1984). Bitlis Masifi Avnik (Bingöl) Yöresindeki Zengin Demir Yataklarının Oluşumu . Jeoloji Mühendisliği Dergisi , 8 (1) , 11-15 . Retrieved from https://dergipark.org.tr/tr/pub/jmd/issue/28444/303042

  • Helvacı, C . Bitlis Masifi Avnik (Bingöl) Yöresindeki Zengin Demir Yataklarının Oluşumu. Jeoloji Mühendisliği Dergisi 8 (1984 ): 11-15

  • Organic geochemistry of tırcmmn
    Hüseyin Yilmaz
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  • Uranium

  • Organic Geochemistry

  • Hümic Acid


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  • Yılmaz, H . (1984). Uranyumun Organik jeokimyası . Jeoloji Mühendisliği Dergisi , 8 (1) , 16-22 . Retrieved from https://dergipark.org.tr/tr/pub/jmd/issue/28444/301900

  • Yılmaz, H . Uranyumun Organik jeokimyası. Jeoloji Mühendisliği Dergisi 8 (1984 ): 16-22

  • The use of strontium isoiopic ratio contents of igneous rocks in the genetic interpretation : Examples from the volcanic rocks of Western Anatolia and Aegean island
    Tuncay Ercan Önder Öztunali
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    ABSTRACT: Studies in the recent years have estabüshecl that the strontium laotoplc ratio» (8îSr/S6İr)measured in igneous rocks have considerable contributed to the attempts aiming to light up the genetteproblems of these rocks. In this paper, these studies are summarized, their appUeations to the Cenozolcvolcanic rocks In the Aegean and in West Anatolia are stated, and the genetic problems and mapnaicevolutions of these voloanles are discussed. The Sr lsotopic ratio measurements earned out in the PlioQuaternarY island are volcanic» found in the Aegean sea have revealed that this arc wleaiiism hasa much greater 8?Sr/86Sr content than those of other island arcs in the world, and that this ratio alsoshows differences locally from one point to another. On the lother hand, the Sr isotope measurement»conducted in the Cenozoie volcanic rocks of West Anatolia Imply that voieamsm in this region k notmonogenic, and that there is a mantle-crust relationship.

  • Magmatic Rock

  • Strontium İsoiopic

  • Volcanic Rocks

  • Aegean island

  • Western Anatolia


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  • Ercan, T , Öztunalı, Ö . (1984). Magmatik Kayaçların Stronsiyum İzotop Oranı içeriklerinin Kökensel Yorumlamada Kullanılışı : Batı Anadolu Ve Ege Adalarındaki Volkanik Kayaçlardan Örnekler . Jeoloji Mühendisliği Dergisi , 8 (1) , 23-32 . Retrieved from https://dergipark.org.tr/tr/pub/jmd/issue/28444/301934

  • Ercan, T , Öztunalı, Ö . Magmatik Kayaçların Stronsiyum İzotop Oranı içeriklerinin Kökensel Yorumlamada Kullanılışı : Batı Anadolu Ve Ege Adalarındaki Volkanik Kayaçlardan Örnekler. Jeoloji Mühendisliği Dergisi 8 (1984 ): 23-32

  • Genesis of the apatite-rich iron ore deposits, Avnik (Bingöl) region, Bitlis massif, Turkey
    Cahit Helvaci
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    ABSTRACT: In the Avmlk aıea, apattte-rlch iron mm are toterbedl^d wîtti basic to İ&lfAe calo-alkaMne metmolmnâm (ca, 4Ä OMa) showing some well-preserved parphyritiô* spheruUttc and voîoaıüelastie texture»,They ar« intrudM by the Avnik and YaylÉ* graMttAï (ca. SÄO Ma). The toon ores and associated metavolcoiiù`s and granitoids are utioonfornmbly overlain by ntieaschtets and Permian marbles, which were foldedand metamorphosed during the Alpine orogeny The won ore bodies are banded, massive or âï»m mtoated M form and me located along the gmdatfionalcontact zone between the gneisses and the better-pre »rved parts of the metavoleanic sequenee. The vmmUve lonsdkkil oi^ zones ar© teaninated, 1-» millimeters to a few eenttmeters, and the banded ore zones showmagnetite-apatite lamination». The dissemtoated iron ot€» are re^onally widespread in til© metovolcaniçs, butusually are coneent^teâ adjecent to the massive ore zones.Magnetite, apatite and acttnolite are the dominant minerals to all ty^ s of depteit; accessory phases tolude feldspar» quartz, mÊm, diopside, hornblende, eroiàte and sphene, OMorite, tale, epMote, aHanite, eaMte, hematite, Mmenite and mtile are low- T retrograde minerals. Surface and near surface, magnetite eoneentmttons are always wtte â The final stage of alteration con»tet§ of a general toasformatton in togTOthite. Fluo^pattte was partly altered to hydroxy-fluorapattte and hyroxyapattte. The apatite-rich iron ares were initially formedj in a volcanic environment and it i* concluded thatthe ores formed from Immiscible Mquids which se^mted from magmas that underwent strong fraettonation,BEE data on coexisting apatite ana magnetite and on the associated metevoicamtes support this conclusion. Where the apattte-rfeh iron ores were intrudedby the AvMk granitoid, they were remobiiîzeâ to from»toekwork type veiiis of large magnetite, apatite and aotiaiolite crystals,

  • Bitlis Massif

  • Avnik(Bingöl)

  • İron Deposits

  • Metamorphic

  • Magma


  • ALTINLJ, I.E., 1966» Oeoloşy of eastern and south eastern Anatolia, Part n: Turkey Mineral Research and Explor, Inst, Bull,, 6T, 1=22,

  • ARVAOTrmiS, N., ve RICKARD, Dé , 1981, REE - (geochemistry of an early Proterozoie volcanic ore district, Dammberg, central Sweden, a summary of results: Annual Report of the Ore Research group, Stockholm University,

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  • BRUNFELT» A,O4i ve RÖEX4ANDTS, Iif 1974» Determination of rare earttis and thorium in apatites by thermal and epithermal neutron - activation analysis; Talanta, 21, 513-521,

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  • ERDOĞAN, B.f 1982, Bitlis Masifinin Avnik (Bingöl) yöresinde jeolojisi ve yapısal özellikleri: Ege Ünlv,, Yerbilimleri Fak,, femir, yayınlanmamıg doçentlik tezi, 108 s,

  • ERDOĞAN, B.} HELVACI, C, ve DORA, O.Ö., 1981, Avnik. Bingöl yöresi apatitli demir yataklarının jeolojisi ve oluşumu: Kesin rapor, Yerbilimleri Fak., Ege Üniv,, î-smir, 121 s.

  • FLEISCHER, M., 1983, Distribution of the ianthanidês and yttrium in apatites from iron ores and its bearing on the genesis of ores of the Kiruna type: E0ÖN, GEOL., 78, 1007-1010.

  • FRUTOS, J,J„ ve ÖYARZUN, J.M. 1975, Tectonic and geochemieal evidence concerning the genesis of El Laco magnetite lava flow deposits, Chi= le: EGON. GEOL,, 70, 988-990.

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  • Genç, S . (1984). Bitlis Masifi Güney Kenarında (Lice-Kulp Yöresi, Diyarbakır ili, GD Türkiye) Metamorfizma- Deformasyon İlişkileri . Jeoloji Mühendisliği Dergisi , 8 (1) , 33-52 . Retrieved from https://dergipark.org.tr/tr/pub/jmd/issue/28444/301890

  • Genç, S . Bitlis Masifi Güney Kenarında (Lice-Kulp Yöresi, Diyarbakır ili, GD Türkiye) Metamorfizma- Deformasyon İlişkileri. Jeoloji Mühendisliği Dergisi 8 (1984 ): 33-52

  • Geology of the Sinop basin and petroleum possibilities
    Abdullah Gedik Sadettin Korkmaz
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    ABSTRACT: In the Sinop bankı, a sedinıeaıtary sequence with a thickness öl more than ten thousandsmotors has been developed during the lias-Quaternary tiinie iiitervaJ,Metamorphlc rocks of Boyabat fonu the basement of the bairfit, I®m a^eû Akgël formation unctmfor^mably overlies the basement, Bürnük formation, composed of red iconfrlomerategj overlies Ategol formattonwith an unoonfiarmity, Dumig1 Borger and Malm» a shallow marine environment has been presented Inthe area and the Akkaya Umestone formation lia« been deposited with Its platform-type carbonates,consisting of thick layer» and occasionally ancwing reef characteristics with abundant organJsınSt LowerCretaceous aged Çağlayan formation overMes Akkaya Limestones with anı unconformity, and consists ofturbldltic sandy Hmeatonej üandstane MterbeMed black^^ialè and marts. Which implies the presence of amarine environment. Bareness of iomûn and the abunclamca of pyrites Indicate the presence of a reduction` inthe environmental canditftms. At the end of Lower Cretaceou^ the area has been teçtonïcalïy upliftedagalnı. From the beginning »of the Santonlan, aiubsidënce restarted, During Bantonian and Oampanianfred colored cherty, mlcrltlc limestones, indicatttag` the peeiitaftiJes of a dteep marine environment, have beendeposited, At the end of Oampanian, the area has clearly acquired the chraeteriistîes of a goesyneline.The Yeimfliomy formatJcn, v/hich has been developed over Kapanbofazı formattottj Is of the volcanic flysehfacie», eon&Ssting of turbïclltic sandston-nisarl Interbedded tuff and tuffite alternattons, Th% unit isovertain by the Cankurtaran formatton, which is of Maastricntian, and which coniÄist of the alternation oftıırMdiâtic sondstone» inarf and shale tiiat have been formed in the flyseh fades,Th© Akveren jßarmation has a caieiturbfditle charaeter, and it is overlain by ttie turbidlttc red coloredAtbap formatton. Of sédimentation that has Initiated in Santonian had continued until Lower Eocenewithout any intennission, The area preserves its geosyncllne character during this time Interval, The Yenikonak formation overlies these deposits with an unconformity. Them all these units are overlain by theSlnop and Sarikum formations with an angular unconformity. Additionally, the Hamsaros formation ofthe region oansists of basaltic agglomerates^ volcanic tuffs, dykes and basalt lavas,

  • Sinop Basin

  • Geology

  • Petroleum Possibilities

  • Metamorphites


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  • GEDİK, A, ve TÜRKAY, t, 1961, Ayancık batısmm 1/25,000 Ölçekli jeoloji haritası: Petrol İşleri Genel müdürlüfü arşivi,

  • GEDİK, Ao ÖZBUDAK, N., ÎZTAN, H,f KORKMAZ, S, be AĞRIDAĞ, D.S., 1981, Sinop havzaamm jeolojisi ve petrol olanakları ile ilgili ön sonuçlar: TJK 35, Bil, Tek, Kurul, Bil, Özet,

  • GEDİK, A,, ERCAN, T, ve KORKMAZ, S,, 1983, Orta Karadeniz (Samsun-Sinop) havzasmm jeolojisi ve volkanik kayaçların petrolojisi: MTA Enstitüsü dergisi (Baskıda),

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  • WALKER, R,G„ 1978, Deep water sandstone facies and ancient submarine fans, Models for explo.* ration for stratigrafic traps: AAPG Bull. 62, 932-966,

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  • 5TILMAZ, O.f 1980, Daday . Devrekani masifi kuzeydoğu kesimi litostratigrafi birimleri ve tektoniği: 5, 6, 101^135,


  • Gedik, A , Korkmaz, S . (1984). Sinop Havzasının Jeolojisi ve Petrol Olanakları . Jeoloji Mühendisliği Dergisi , 8 (1) , 53-80 . Retrieved from https://dergipark.org.tr/tr/pub/jmd/issue/28444/303044

  • Gedik, A , Korkmaz, S . Sinop Havzasının Jeolojisi ve Petrol Olanakları. Jeoloji Mühendisliği Dergisi 8 (1984 ): 53-80

  • Mineralogy and petrography of the Serçeme creek (Ermrum) ultramaf Us
    Ali Bilgin
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    ABSTRACT: In thİA research the Serçeme creek and surrounding area in the NW of Erzurum have been Investigated. Producte of magmattsm comprises ultramafie rocks wMeh were intruded In the Upper Cretaceous and Tertiary boundary. They are compoaed of harzburgite and serpentïnite and Generally replaced by maJdmgcold fintnufon in to a tectonic Ipaumöary along which Lower Cretaceous Umaston© im thrusted on UpperCretaceous limestone, Serpenttnizatioii increases toward the nıargîns. miat situation pointe out that serpentinr/alion Is facilitated by tectonic agents. Serpentine minerals were studied by P.TÉA. method and It wasfound that those serpentinites contain mostly Mzardite. chry»ottle and chlinochrysotile but antig^rite.

  • Serçeme Creek (Erzurum)

  • Ultramafus

  • Mineralogy

  • Petrography


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  • Bilgin, A . Serçeme (Erzurum) Deresi Ultramafitlerinin Mineraloji Ve Petrografisi. Jeoloji Mühendisliği Dergisi 8 (1984 ): 81-88

  • J.a. Gilreath R.w. Stephens Necdet Şengündüz
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  • Delta Environment

  • Log

  • Clay

  • Dipmeter



  • Gilreath, J , Stephens, R . (1984). Delta Ortamında Log Değerlendirmesi . Jeoloji Mühendisliği Dergisi , 8 (1) , 89-92 . Retrieved from https://dergipark.org.tr/tr/pub/jmd/issue/28444/303046

  • Gilreath, J , Stephens, R . Delta Ortamında Log Değerlendirmesi. Jeoloji Mühendisliği Dergisi 8 (1984 ): 89-92

  • Geologist in the minerals industry
    G.r Davis Cihat Başocak Şener Teoman
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  • Minerals İndustry

  • Place of Geological Engineer

  • Applied Geology

  • Mineral Geology


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  • Davis, G . (1984). Madenlerle İlgili Endüstride jeoloji Mühendisinin Yeri . Jeoloji Mühendisliği Dergisi , 8 (1) , 93-102 . Retrieved from https://dergipark.org.tr/tr/pub/jmd/issue/28444/303047

  • Davis, G . Madenlerle İlgili Endüstride jeoloji Mühendisinin Yeri. Jeoloji Mühendisliği Dergisi 8 (1984 ): 93-102

  • importance of geology in this century and duties of Turkish geologist m the economy of Turkey
    Güner Göymen
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  • The İmportance of Geology in Our Time

  • Economy

  • Scientific Findings



  • Göymen, G . (1984). Jeolojinin Çağımızdaki Önemi Ve Türkiye`nin Ekonomik Hayatında Türk Mühendisine Düşen Görev . Jeoloji Mühendisliği Dergisi , 8 (1) , 103-104 . Retrieved from https://dergipark.org.tr/tr/pub/jmd/issue/28444/303048

  • Göymen, G . Jeolojinin Çağımızdaki Önemi Ve Türkiye`nin Ekonomik Hayatında Türk Mühendisine Düşen Görev. Jeoloji Mühendisliği Dergisi 8 (1984 ): 103-104

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