TMMOB
Geology and problems of dating of Neogene basins in Gedig and southern Emet
Gediz-Emet
Neogene Basins
Problems of Dating
Discordant
Palentology
Radiometry
AKKUŞ, M, F., (3M2) : Kütahya - Gediz arasında ki sahanın Jeolojisi M.T.A, Dergisi s, 58f 21-30
ARPAT, E- BÎNGÖüU E, (1969) : Ege bölgesi graben sisteminin gelişimi üzerine düşünceler M.T.A* Dergisi s: 73, 1-9
AKDENİZ, N. -KONAK, N: (1979) : Simav - EmetDursunbey - Demirci yörelerinin jeolojisi M.T.A, Derleme Rap, No :
BİNGÖL, E. (1974) : Muratdağı merkezi kesiminin je^ okgisi magmatik metamorfik kayaçların pet= roloji ve jeokronolojisi - ANKARA
BmaöU E. ARPAT, E. (1969): 23 Mart 1969 De« mirci-Sındırgı, 28 Mart 1980 Alaşehir Depremleri M,T, A, Derleme Rap, No: 4172
ERGİN, K, (1972): Gediz Depremi,
ERCAN, T, . DÎNÇEL, A, - GÜNAY, E. - TÜRKECAN, A, (1977): Uşak Yöresinin jeolojisi ve volkanitlerin Petrolojisi M.T.A, Derleme Rap.
CAWLJK, J. (1956): Borate deposits of Emet Neoge^ ne basin M;TäA, Derleme Rap, No: 2470
GÜN, H, (1971): Kula-B§me bölgesinde mevcut Radyoaktif seviyenin etüdüne ait Rapor M.T.A, Derleme No: Sİ59*
GÜN» H, (1975): Gediz İlçesi (Kütahya İli) Neojen havrası ve güneyinin jeolojisi Master teM, îst, Üniv, Fen Fak, Jeoloji Enst, va M.T.A, Derleme Rapor No:
GÜN, H, - BİNGÖL, Eä - AKDENÎ2, N. ~ GÜNAY, E, (1976): Géologie du Bassin tertiaire des Re« gions Nord-Est du massif d© Menderes. Bull, Soc, GéoL France t, XVXn, no: 2, p. 451-458
HELVACI, q-FIRMAN, R.J.-(1977): Emet Borat Yataklarmm jeolojik Konumu ve Mineralojisi« Jeoloji Mühendislifi Dergisi, Sap: 2, p. 17-28.
SBLLIIY, R,Ö, (1973): Eski Çökelme ortamları, Prof. Dr, I.E. Altınlı tercümesi 1st, Üniv; TatMM Jeoloji Kürsüsü
ABSTRACT:. In the basins of Emet and Gediz, Tertiary and Quaternary sediments and volcanic rocks are widespread. The rocks of the Neogene age unconformably overlie the basement rocks which are upper Cretaceous or Pre-Ctetaceous in age, The Miocene and the Pliocene Sediments are of terrestrial origin, being accurately datey by radiometriö, palinologic and paléontologie methods. They were deposited in the intermontane basins representing different faciès. An angular unconformity has been found between the rock units of Miocene and Pliocene age especialy in the southern part of the investigated area. The volcanic activity continued during the Moeene and the Pliocene periods* Plio-Quaternary and Quaternary sediments are represented by coarse grained fluviatUe deposits,
Fosailiferous plaser occurrences and reïictê of ultrabasic rocks of Precambrian age near
Taşbaşî; Çukurca-HakkarL
Hakkari-Çukurca-Taşbaşı
Fosailiferous Plaser Occurrences
Ultrabasic Rocks
Minerals
Microscopic Studies
Aksu, R, ve dif erleri, 107» UludereJHakkari^Çükurea dolayı Paleozoik istifmin temel jeoloji Özellikleri.- 33, Türkiye jeoloji bilimsel ve teknik kurultayında bildiri olarak sunuldu. Ankara
Andren T, ve Doughty F, T, C. 1971, TJpgading iron» sanda at New Zealand Steel.-Minlng Magazine, London, March, pp. 200-203,
Bascom, Wn 1960, Beaches.- Scientific American, August, Offprint 845, Freeman and Comp,, San Francisco.
Bülow, Kè . von, 1951, Schwer mineralseifen an der Meeklenburgschen Ostseeküste,-Archiv für Lagerstaettenforsehung, Heft 81, Akademie Verlag G, m, b, H,, Bariin
Çafatay, A. ve Arda O., 1977, Mineralojik rapor no 97-945g.-Numune arşiv no 105390. M.T.A, Enstitüsü Mİn.-Petrog, servisi arşivlerinde, Ankara yayınlanmamış,
Çafatay, A. ve Üregel N., 1978, Metin Çelikorsô ait numunelerin mikroskopik incelenmesi M.T.A, Enstitüsü mineraloji ve petrografi arşivinde, Ankara, yayınlanmamış
Davidson, O* F,f 1956, The economic geology of thorium,-Mining Magazine, voL 94, No, 4, pp. 197-208, London,
Friedrich, G., 1974, Schwermineral sandvrkommen im Küstenbereieh Àugtraliens.-Erzmetallj Band 27, s. 350-353, Stuttgart.
Gallagher, M, J,, 19f 4, Rutile and zircon in Northumbrian beach sands. Institution of Mining and Metallurgy, Transactions/Section B (Applied earth science), London, August, pp. B 97-B 98
Gardner, D. Mt 1955, Beach-sand heavy-mineral deposits of eastern AustraHa.-Australia Bureau Mineral Resources Geology and Geophysics,- Bull. 28,
Gillson, J, I*., 1950, Deposits of heavy minerals on the Brazilian coast.-Mining Engineering (AIME), Transactions, vol. 187, New York, pp, 685*693,
Gillson, J, I., 1959, Sand deposits of titanium minerals,- Transactions of the American Institute of Mining, Metallurgical, and Petroleum Engineers (Allara ), vol. 214 pp, 421-429, New York,
Ingh, J, C. Jr., 1966, The movement of beach sand-Developments in Sedimentology» 5, Elsevier, Amsterdam
Johnson, D, W,, 191», Shore processes and shoreline development. John Wiley and Sons,
Ketin, % 1979, Hakkart-Çukurea arasının büyük Zap suyu boyunca jeolojik kesiti,- S3, Türkiye jeo« loji Bilimsel ve teknik kurultayında bildiri olarak sunuldu, Ankara,
Köksoy, M,, 1975, Doğu Karadeniz plaser manyetit yatakları. Türkiye madencilik bilimsel ve teknik kongresi.- Maden mühendisleri odası yayınları, s. 435-451, Ankara
Kuenen, H,, 1950, Marine Geology.-New York
Lütting, G,, 1974, Seifenlagerstaetten an der nieder« saechsishen Küste.-Glückauf, 110,, Essen, s. 169-171,
Mason, M, A,, 1950, Geology in shore=control problems»- Oıapter 15, pp. 176-290 in: P, D, Trafik, Applied Sedimentation, John Wiley and Sons, New York etc,
Pfeiffer, H,, 1972, Sçhwermineralsëifen, Küstendynamik uni Sedimenthaushalt sandiger Flachküsten Mecklenburgs. Jahrbuch für Geologie, herausgegeben vom Zentralen Geologischen Institut der D.D.R. Band 4, Berlin.
Ramdohr, P., 1975, Die Efzmineralien und ihre Verwachsungen. 4, Aufl. Akademie-Verlag, Berlin.
Singh, R., 1973, Depositional Sedimentary Environments,- Springer Verlog, BerlinJffeidelbergNew York,
Ward, J., 1965, Heavy-mineral beach sands of Australia. Eighth Commonwealth Mining and Metallurgical Congres®, vol 1. pp. 53-54, Melbourne
Williams, CK, 1965, Economic Geology of New Zealand, 1. Baskı.
ABSTRACT: Syngenetically fomıed Çukurca-Ta^bafi fossiüferous plaser deposit occura in Cambriaıı quartzites, Microscopic investigations on samples taken from the deposit revealed various heavy minerals (haematite with rutüe, haematite, rutile, chromite, ilmenite, magnetite, limonite, psüomelane, pyırhotite, ehaJcopyrite, zircon and tourmaline), quartz, feldspar (microline, orthoclase and plagioclase), rock fragments, sericite, chlorite and muscovite. Chemical analyses of the samples shewed high concentrations of F^O3, mo2 and ZrOi, H future feasibility studio in the area give positive results the Çukurca-Ta§bap fossiMferous plaser deposit can be economical for Ti, Fe and Zr production. Additionally, the presence of chromite suggests that this mineral originated from ultrabasic rocks of Vre- Cambrian age.
Surveying of Gas Storage Underground Caverns by Laser and Btereophotographs
Underground cCvities
Laser
Stereophotographs
Gas Storage
ÖZMUMGU, Ö,, 1078 Yeraltı Boşluklarının Stereo Resimlerinin Çekilmesi (SD-Foto-Log), Petrol (Petrol Mühendisleri Odası Yayın Organı) sayı 11, gayfa 34-36
NÔLTBf E,, 1978 Lasermessungeıı und Stereofotogra« fie, Prakla-Seismos Report, 3/7S,
ABSTRACT: It is usual to encounter underground cavities in the geological formations invarious depths, This paper reporta the study of gas storage caverns by means of laser and stereophotographic surveying techniques
ABSTRACT: This article is an attempt to summarize the geologic environments for nickel deposits and parageneses with which nickel is associated; thus 14 types of nickel deposits are defined. On the other hand the nickel potential of Turkey is investigated concluding seven different types of nickel concentration can be expected. These are put in order of importance according to geologic and metallogenic data of Turkey. Nickel is mainly found in ultramafic rocks and their alteration products namely lateritic iron deposits. In addition acid plutonic rocks play a part in formation of nickel deposits Turkey is very likely to beara high nickel potential as large areas are covered by ultrabasic and acid plutonic rocks. Emphasis is also laid upon asphaltites covering an area of 20.000 square km. containing 3,2 kg. of Ni in one ton of asphaltite ash and other valuable minor products such as Mo and V and the recovery of such minor products.
Geologicahhydrogeologîcal investigation of Uşak Esme-Örencik hotspring
Eşme-Örencik(Uşak)
Hotspring
Geology
Hydrogeologîcal
Başkan, E,, (1971`j: Jeotermik Enerji Sondajlarında Elde Edilen Sıcak Suların Şifalı Su Olarak Deferlendirilmesi Türkiye i, Jeotermal Enerji Simpozyumu (Tebliğler) Ankara
Baykal, P,, (İ054) : Alafehir, Ugak Mıntıkasının Jeolosi hakkında Rapor MTA rapor No: 2296 Ankara
Castony, G,, (1969): Yeraltı suları hakkında pratik uygulamalar, Çevirenler: K. Karacadaf - A. geber, DSÎ Matbaası, Ankara
Çaflar, K,Ö,, 1950(): Türkiye Madensuları ve Kaplıcaları MTA Yay. Seri: B> No: İl Ankara,
Güzel, A,, (1978): Egme-Örencik Sondajı Bitirme Ön Raporu (Yayınlanmamış) Ankara.
Holler, H., (1953: B8/3, 88/4, 89/3 ve 105/1 ile 89/1 kısmen) Paftalarının Jeolojik Haritası Hakkında Rapor MTA Rapor No: 2385 Ankara
îça, M., (1978): E§me-,ÖrenGik Kaplıdsı Jeoloji - Hidrojeoloji Etüd Raporu, MTA Rapor No: 6034 Ankara.
Kalafatçıoflu, A., (1961): Gediz_U§ak Arası Bölgenin Jeolojik Raporu, MTA Rapor No: 2818 Ankara
Turkman, M (1972) : Su Kimyasi Çali|maları Rehberi» DSÎ Yeraltısulan Dairesi Başkanlıfı Ankara,
The mıneralogical studies of schistose rocks (Gonäiies) occurring in the BitUş - Yukarı ölek
kÖyü-Süllap Bere area with a view about their origin
Yukarı Ölek Köyü(Bitlis)
Süllap Bere area
schistose(Gondites)
Mıneralogical Studies
Baedekers, (1968), Autoreiseführer» Türkei, - Verlag Stuttgart, Zweite Auflage,
Berner, R,A,, (1970), Sedimantary pyrite formation, American Journal Science, 268, pp. 1-23,
Olssarz, A,, (1965), Einführung in die allgemeine und systematische Lagerstaettenlëhre, Stuttgart,
Çafatay, A, ve Aydın, E (1977:, Bitlis masifinde rastlanan alabandin ve birlikte bulunan bazı maden minerallerinin mikroprob analizleri, Baskıda
Derby, O.A., (1901), On the mangenese ore deposits of the Queluz (Lafalette) district, Minas Gérais, BraMl-American Joura* Sei,, 162, pp, 18-32,
Dileköz, E. ve Çafatay, A., (1973), Bitlis.MerkezuYukarıölek- Süllap dere işaretle gelen numunelerin mineralojik tetkik raporu MTA, Lab, Dairesi, 6.1.1973, 1295/7525. (yayınlanmamış).
Fiebbiger, W,, (1975), Organische Substanze in praekambrisehen Itabiriten und deren Nebengesteninen, - Geolog, Rundschau, Band 84, Heft 2, S, 641*652, Stuttgart,
Herz, N, ve Bunarjes, S,, (1973), Amphibolites of the Laffidëtte* Minas Gerais and the Serro da Navio mangâAêse deposits, Brazil, Ecin, Geol. Vol. 68, pp. 1989 J966
Kılıç, M (1970), Kbltik-Humaç-Kalupat-Yapızmık köyü civan jeolojisi ve bakır mineralizasyonu, MTA ENS, Derleme Raporu, (yaymlanmâmış),
Kraeff, A, ve Çafatay, A,, (1972), Bitlis-Blmek bucafı-yukan ölek köyü i§aretiyle gelen numunelerin mineralojik tetkik raporu. MTA, Lab, Dairesi, 19.10,1972, 90S/7460» (yayınlaıımamıl).
Müller» O, ve Ftiehtbauer, H,f (1970), Sedimante ünd Sedimentgesteine, Teil l, Stuttgart
Niggii, P, ve Niggli, E (1952), Gesteine und Minerallagerstaetten, Zweite Band, Rosel,
Eamdohr, P., (1975), Die Erzmineralien und ihre Verwachsungen, Akademie-Verlag, Berlin
Ramdohr, P. vé Strunz, H., (1967), Kloekmann^ I^hrbuch der Mineralogie, Stuttgart.
Roy, S,, (1965), Comparative study of the metamorpho^ sad mangantse protorta oï toe world-the problem of the nomenclature of the gondites and kodurites, Eeoné Geol., Vol. 60» pp, 1238-12éo,
Roy, S, ve Purkait, P,K,, (1968-69), Minerâlöfy and gnesis of the metamorphosed mmnfanesê silicate rocks (gondite`) of Gowari Wadhona, Madhya, Pradesh, India, Beitraege zur minéralogie und petrolögıe. Vol, 20, pp, 86^114, Berlin-ReidelbergNewyork.
Stanton, R,L (1972), Preliminnary account of chemical relationship between suif i de lode and
ABSTRACT: The regionally metamorphosed rocks of the Bitlis area which are composed of quartz, spessartite, gericite, chlorite, diopside and actinolite age determined as an interesting type of schists or gondites. These rocks contain the following ore minerals: Alabandite, pyrrothite, graphite, sphalerite, pyrite, rutile, chalcopyrite» arsenopyrite, pararammelsberglte, marcasite, fahlen and niccolite besides a small amount of titanite ,apatite, zircon and topaz. All these minerals have been investigated mineralogically in detail and the paragenetic relationship between them have been worked out. The evidence obtained from these studies suggests, that these schists for gondites) have been formed by the regional metamorphism of fine-grained clastic sedimentary rocks falling between psammite and pelite group