DOCSLIB.ORG

Assoc. Prof. HÜSEYİN EVREN ÇUBUKÇU

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Assoc. Prof. HÜSEYİN EVREN ÇUBUKÇU Assoc. Prof. HÜSEYİN EVREN ÇUBUKÇU EPmerasilo: necaulb [email protected] Education Information Doctorate, HUnaciveettrespiteé ÜDn''iavuevresirtgensie, FCelenr mBiolinmtl-eFreir Ernanstd., IJ,e Socloiejni Mceüsh Deen dLias lTiğeir, rTeu, rVkoelyc a2n0o0l2o g- i2e,0 F0r8ance 2004 - 2008 UPonsdtegrrgardaudautaet, eH, aHcaectetettpeep Üe nÜinveivresritseitsei,s Fi, eMnü Bhielinmdleisrlii kE Fnastk.,ü Jleteosloi, jJie Molüohjie Mndüihsleiğnid, iTsulirğki,e Tyu 1r9ke9y9 1- 929040 2- 1999 FEnogrliesihg, nC1 L Aadnvagnucaedges Dissertations FDeonc tBoirliamtele, Nrie Emnrsutitt üsstrüa, tJoevoololkjia Mnıünhıne npdeitsrloiğloi j(iDk re)v, r2im00i:8 çarpışma bölgesinde peralkali magmatizma, Hacettepe Üniversitesi, MPoüshtgernaddisulaiğtie (, YBlo)d (rTuemzl iv)o, 2lk0a0n2izmasının petrolojik incelenmesi, Hacettepe Üniversitesi, Fen Bilimleri Enstitüsü, Jeoloji RGeeosloegaircaclh E nAgrineeaesring, Mineralogy-petrography, Petrography and Petrology, Engineering and Technology Ascsaisdtaenmt Pirco Tfeistsloers, H/a cTeattsekpes Üniversitesi, Mühendislik Fakültesi, Jeoloji Mühendisliği Bölümü, 2018 - Continues RAessiesatarcnht PArsosfisetsasnotr, ,H Haacceettteeppee Ü Ünniviveerrssititeessi,i ,M Müühheennddisislilkik F Faakküültlteessi,i ,J Jeeoololojij iM Müühheennddisislilğiği iB Böölülümmüü, ,2 2000122 - - 2 2001128 Advising Theses İÇnUcBelUeKmÇeUs iH, P. oEs. t, gKraapdaudaotek,y Va. EVRoKlkUaTn(ikS tPurdoevnetn),s 2i'0n1d8e Yer Alan Eğrem Tepe Hidrovolkanik Çökellerinin Petrolojik pÇeUtBroUlKoÇjiUk iHn.c Eel. e, mKuesvia, tPeorsntegrr aGdöulcaütek, (EI.sApKaKrtAaŞ)( vSotulkdaennitz)m, 2a0sı1n5a ait hidrovolkanik çökellerdeki magmatik ksenolitlerin Articles Published in Journals That Entered SCI, SSCI and AHCI Indexes I. Shoshonitic volcanism of the Bodrum caldera (SW Turkey): Hybridization of enriched mantle- dÇUerBiUvKeÇdU a Hn.d E c. ,r AuYsDtaAl Rm Ee.,l tUsLUSOY İ., Gourgaud A. II. ZJOirUcRoNnA gLe OoFc hArSoIAnNo lEoAgRyT aHn SdC IOE-NHCfE iSs, ovtool.p2e1s9 , o2f0 C21a p(pJoaudroncail aInd iegxneidm ibn rSiCteI)s: New insights into continental cArKuINst aLl., aArYcDhAitRe Ect.,u Srceh muinttd Ae.r Kn.e , aÇtUhB tUhKeÇ CUe Hn. tEr.a , lG Aenrdaetso lAia.n Volcanic Province, Turkey III. GOeoNcDhWemANicAa Rl ESvEaAluRaCtHio, vno ol.9f 1S, upipta.1b6i6li-t1y8 7o,f 2 C0e2n1t (rJaolu Arnnaalt Ionldiaenxe (dT iun rSkCeI)y) Volcanic Rocks for Rock Fiber PERroSOdYu cOt.i, oAnYDAR E., ÇUBUKÇU H. E. IV. AN AmTiUcRrAoL-c RoEmSpOuUtReCdE Sto RmEoSEgAraRpChHi, c2 0a2ss0e (sJsomurennatl Ionfd reoxeodt icna SnCaIl) preparation with conventional and dESifEfNerTeÜnRtK r Go.t, aArKyK fAilŞe Es. ,i Cnu pbruikmcua rEy., Nteaegtahs aEn., dU yyaonuikn Og. , pÇeErHmRaEnLeİ nZ.t Ct.eeth V. AINpTpElRicNaAtiToInO NoAf Lz iJrOcUoRnN tAyLp OoFlo PgAyE mDIeAtThRoIdC tDoE NfeTlIsSiTc RrYo, cvkosl. 3(0C,a npop.2a, dpopc.2ia0,2 C-2e0n8t,r 2a0l 2A0n (aJotoulrinaa, lT Iundrkexeeyd) :i na SCI) zAiKrIcNo nL .,c ArYyDstAaRll iEz.a, Sticohnm ittet mA.p Ke. r, aÇtUuBrUeK pÇeUr sHp. eEc.tive VI. ATU 2R5K ImSHy rJ OcUhRrNonAoL sOtFra EtAigRrTaHp hSCyI EoNf CigEnSi, mvobl.r2i8te, ns oi.n3 , spopu.3t5h1 P-3e8r6u,: 2 i0m1p9l i(cJoautironnasl Ifnodre xthede ivno SlCcIa)nic history of tThheo uCreent tJr., aJilc hAan Bd.e, sPaquette J., ÇUBUKÇU H. E. VII. VJOeUrRtiNcAalL vOaFr iTaHtiEo GnE iOnL tOhGeI CdAeLu SteOrCiIcE ToYx,i dvoalt.1io7n3 , onfo t.5it, apnpo.7m34a-g7n5e6t, i2te0s1 6in ( Jaonu ringanli Imndberxiteed dine pSCoIs)it: Kizilkaya IÇgUnBiUmKbÇrUit He . (EC.appadocia, Turkey) VIII. AJopuprnliacla otifo Vno locaf nDoelocgisyi oannd T Greeoet hAelrgmoarli tRhemse aforcrh c, lvaosl.s3i0fi8c,a ptpio.1n0 -a1n8d, 2 i0d1e5n t(iJfoiucarntiaol nIn odfe xneadt uinr aSCl Im)inerals using SAEKMKA-EŞ DES., AKIN L., ÇUBUKÇU H. E. , ARTUNER H. IX. TCOhMe PmUaTjEoRrS a &n dG EtrOaScCeIE eNlCeEmSe, nvot lg.8l0a,s psp c.3o8m-4p8o, s2i0ti1o5n (sJ ooufr tnhael Ipndroexdeudc itniv SeC IM)editerranean volcanic sources: Tomollsin fsorn cEo. Lr.r ,e Slmatiitnhg V d. Cis. t, aAll bterpth Pr. aG .l a, Ayyedrasr i nE. ,a Cnivde tatrao Lu., nCdio Eniu Rr.o, Çpuebukçu E., Gertisser R., Isaia R., Menzies M. QAu. ,a etet ranl.ary Science Reviews, vol.118, pp.48-66, 2015 (Journal Indexed in SCI) X. CAeYnDtArRa lE A., nÇUatBoUlKiaÇnU PHl.a Ete. ,a ŞuE,N T Eu.r, kAeKyIN: iLn.cision and paleoaltimetry recorded from volcanic rocks XI. ATU RRhKiInSoHc JeOrUoRtNidA SLk OuFl lE CAoRoTkHe SdC-ItEoN-DCEeSa,t vho iln.2 2a, n9o.2.5 M, pap-.7O3ld9 -I7g4n6i,m 20b1r3it e(J oFulornwa lo Ifn dTeuxrekde iyn SCI) PALNOTSO OINNEE P, v., oOl.R7L, nIAoC.1 M1,. 2J.0 , 1A2T (ICJoI uGr.,n UaLl IUnSdOeYx eİ.d, ŞinE NS CEI.), ÇUBUKÇU H. E. , ALBAYRAK E., OYAL N., AYDAR E., SEN S. XII. VULoUlcSaOnYo İl.o, ÇgUicBaUl KeÇvUo lHu. tEio. ,n A aYnDdA Rc aEl.d, LeArBa AfZoUrmY Pin., gE ReSrOuYp tOio., nŞEs No fE .M, GtO. UNReGmArUuDt (AE.astern Turkey) XIII. AJO UcoRmNApLa rOaFt iVvOeL sCtAuNdOy LoOfG qYu AaNliDta GtiEvOeT aHnEdR MquAaLn RtEitSaEtAivReC mH,e vtohlo.2d4s5 ,f popr. 2t1h-e3 9a,s 2s0e1s2sm (Jeonutr noafl aInddheexseidv ein r SeCmI)nant aCfetherre lbi rSa. Bck. ,e Pto dlaetb-Ooznsdoyin Og., Sar C., ÇUBUKÇU H. E. , ÇEHRELİ Z. C. XIV. CEUoRrrOePlEaAtiNo nJO oUfR iNgAnLim ObFr OitReTsH iOnD tOhNe TcIeCnSt, rvaoll .3A4n, antoo.2li,a pnp .v1o8l8c-a1n9i2c, 2p0r1o2v i(nJocuer unsail nIngd zeixrecdo nin aSnCdI) plagioclase aAgYeDsA aRn Ed., SzCirHcMonIT cTo Am. Kp.o , sÇiUtiBoUnKsÇU H. E. , AKIN L., ERSOY O., ŞEN E., Duncan R. A. , ATICI G. XV. MJOtU. RNNeAmLr OuFt VvoOlLcCaAnNoO (LEOaGsYt eArNnD T GuErOkTeHy)E:R TMeAmLp RoErSaElA pReCtHro, vlogl.2ic1a3l, epvpo.8l3u-t9i7o,n 2012 (Journal Indexed in SCI) JÇOUUBRUNKAÇLU OHF. EV.O , LUCLAUNSOYL Oİ.G, AYY ADNADR GEE., OETRHSEORYM OA., LŞ ERNE SEE., AGROCUHR, GvAoUl.2D0 A9,. , pGpU.3IL3L-6O0U, 2H0.12 (Journal Indexed in SCI) XVI. aSnentisciatnivcee rs edpriuogli-tDeN-cAa ribnotenr ancatniontusbes based disposable electrodes for direct detection of DNA and AErNdAeLmY SAT.,, Kvuorl.a1l3a7y, Fn.o, Ç.1U7B, UppK.Ç4U0 0H1. -E4.0 , 0C4o, n2g0u1r2 G (.,J oKuArRnAaDl IEnNdİeZx eHd., iCna SnCaIv)ar E. XVII. SUuYrAfNaIcKe Mp.o Ör.o , sNiatyg aosf E h., aÇnUdB-UmKiÇxUe dH,. sEy. r, Dinaggeli- Fm.,i ÇxEeHd RaEnLdİ Ze.n Cc.apsulated set endodontic sealers 2O0R1A0L (SJUouRrGnEaRl YIn OdRexAeLd M inE DSCICI)INE ORAL PATHOLOGY ORAL RADIOLOGY AND ENDODONTOLOGY, vol.109, no.6, XVIII. cSitrrcuucltautrioen of the Nemrut caldera (Eastern Anatolia, Turkey) and associated hydrothermal fluid JUOLUURSNOAYL İ .,O LFA VBOALZCUAYN PO.,L AOYGDYA ARN ED., EGRESOOTYH EOR., MCuAbLu RkcEuS EEA.RCH, vol.174, no.4, pp.269-283, 2008 (Journal Indexed in XIX. WSCDI)S versus silicon drift detector EDS: A case report for the comparison of quantitative chemical aÇnUaBlUyKsÇeUs oHf. En. a, tEuRrSaOl Ys iOli.,c AaYteD AmRi nEe., rCaalksir U. XX. TMeICxRtuOrNe, vdoisl.c3r9i,m noin.2a, tpiopn.8 8o-f9 4v,o 2lc0a0n8i (cJ oausrhneasl Ifnrdoemx eddi finfe SrCeIn)t fragmentation mechanisms: A case study, MERoSuOnYt ON., eCmHrINuGt As tGr.a, tAoYvDoAlcRa En.,o G, OeUaRstGeArUnD T Au.r, kCeuybukcu H. E. , Ulusoy I. XXI. VCOoMlcPaUnTicE RaSn d& dGeEfOoSrCmIEaNtiCoEnS , hvioslt.3o2r,y n o.f7 t, hpep .9B3o6d-9ru46m, 2r0e0s6u r(gJoeunrtn caal Ilnddeerxae sdy isnt SeCmI) (southwestern Turkey) JUOluUsRoNyA IL., COuFb VuOkcLuC AE.N, AOYLDOAGRY AE.N, LDA GBEAOZTUHYE PR.,M GAOLU RGESAEUADR AC.H, V, vINolC.1E3N6T, pPp..71-96, 2004 (Journal Indexed in SCI) AIr. ticJluelsio Ppoulbisl i(sIhuelidop ionl iOs)t hAenrth Jrooupronloagliscal Research: Preliminary Results JBoÜuYrÜnaKlK oAf RAAnKkAarYaA S Atu. dMie. ,s A, vlpoal.g6u, nt oA..2, Ç, pUpB.1U1K1Ç-U1 2H6. ,E 2. 0, 1C8av (aOlltih Fe.r Refereed National Journals) Books & Book Chapters I. NULeUmSrOuYt İC., aÇlUdBeUrKa ÇaUn Hd . EEa. ,s Mteorunr aAlinsa Dto., lAiaYnD AVRo Elc.anoes: Fire in the Highlands Nina: tLuarned, Cschaapme,s p apn.5d8 L9a-n5d9f9o, r2m0s1 9of Turkey, Kuzucuoğlu Catherine, Çiner Attila, Kazancı Nizamettin, Editor, Springer II. NULeUmSrOuYt İc., aÇlUdBeUraK ÇaUn dH .E Ea. s, tMeorunr Aalnisa Dto., lAiaYnD AvRo lEc.anoes: Fire in the highlands. 2in0: 1L9andscapes and Landforms of Turkey, Kuzucuoglu, C., Kazancı, N., Ciner,, Editor, Springer, Cham, pp.589-599, III. JÇeUoBlUoKjiÇkU N Hu.m E.unelerde uCT Kullanılarak Bileşen Analizi Gerçekleştirilmesi in: Ulusal uCT Yaz Okulu Ders Notları, Eyyuphan Yakıncı, Serkan Polat, Editor, 72 Tasarım, Malatya, pp.15-28, 2016 Refereed Congress / Symposium Publications in Proceedings I. VInotlecrasntistimal (GIslapsasr tBae-aTruirnkge Py)yroxenitic and Monzonitic Lithics: Possible magmatic origin of Gölcük XAXKIK IAnŞte Ern., aÇtUioBnUaKl ÇCUon Hg.r Ee.s ,s A oKf ItNh eK CAaRrApKatÜhLiaAnH B La.lkan Geological Association (CBGA), Salzburg, Austria, 10 - 13 II. MSeipctreomsbceorp 2ic0 1M8o, pnpit.1o2r3ing of Laboratory Based Physical Disintegration Ratio of Fibrous Zeolite CArKyKsAtŞa lEs. , fÇrUoBmU KCÇaUp pHa. dEo. ,c EiaRnK UATlt Ve.r, eAdK IINg nKiAmRbArKitÜeLsA (HT Lu.r, YkUeyR)DAKUL Y., ULUSOY İ., ŞEN E. III. SCeitlief-sP oont eVnotlicaaln, oSeusr 1fa0c, Ne aTpeomli,p Itearlya,t 2u r- e0,7 C SOe2p tmemebaesru r2e0m18e, nptps. 1a1n1d7 related structural discontinuities on MDİoKuEnRt C H., aUsLaUnS,O TYu İr., kAeKyKAŞ E., ŞEN E., ÇUBUKÇU H. E. , GÜMÜŞ E., BAŞAR O., AYDIN E., ERKUT V., KAYGISIZ N. IV. PCiOtiResO oSnIT VYo lIcNaVnoEeSsT 1IG0,A NTaIpOoNli , O2F - 0K7I NSeIKpt eCmObAeLrS 2 (0S1O8M, pAp .5B2A1SINTURKEY) USING X-RAY MICRO-CT 7K1A.R TAüYrİkĞiyİTe JAe.o İl. o, jÇi UKBuUruKlÇtaUy ıH, A. En.k ,a OrSaK, TAuYr kRe. yG, . 2, 3A K- K27A ŞA Ep.ril 2018 V. LAoKwIN TKeAmRApKerÜaLtAuHr eL .A, ÇltUeBrUaKtiÇoUn Ho.f E
Load more

Recommended publications
  • Acigöl Rhyolite Field, Central Anatolia (Part 1): High-Resolution Dating of Eruption Episodes and Zircon Growth Rates
    Acigöl rhyolite field, Central Anatolia (part 1): high-resolution dating of eruption episodes and zircon growth rates Axel K. Schmitt, Martin Danišík, Noreen J. Evans, Wolfgang Siebel, Elena Kiemele, Faruk Aydin & Janet C. Harvey Contributions to Mineralogy and Petrology ISSN 0010-7999 Volume 162 Number 6 Contrib Mineral Petrol (2011) 162:1215-1231 DOI 10.1007/s00410-011-0648-x 1 23 Your article is protected by copyright and all rights are held exclusively by Springer- Verlag. This e-offprint is for personal use only and shall not be self-archived in electronic repositories. If you wish to self-archive your work, please use the accepted author’s version for posting to your own website or your institution’s repository. You may further deposit the accepted author’s version on a funder’s repository at a funder’s request, provided it is not made publicly available until 12 months after publication. 1 23 Author's personal copy Contrib Mineral Petrol (2011) 162:1215–1231 DOI 10.1007/s00410-011-0648-x ORIGINAL PAPER Acigo¨l rhyolite field, Central Anatolia (part 1): high-resolution dating of eruption episodes and zircon growth rates Axel K. Schmitt • Martin Danisˇ´ık • Noreen J. Evans • Wolfgang Siebel • Elena Kiemele • Faruk Aydin • Janet C. Harvey Received: 22 January 2011 / Accepted: 3 May 2011 / Published online: 24 May 2011 Ó Springer-Verlag 2011 Abstract Protracted pre-eruptive zircon residence is fre- crystallized in two brief pulses corresponding to eruptions quently detected in continental rhyolites and can conflict in the eastern and western part of the field during Middle with thermal models, indicating briefer magma cooling and Late Pleistocene times, respectively.
    [Show full text]
  • Monuments, Materiality, and Meaning in the Classical Archaeology of Anatolia
    MONUMENTS, MATERIALITY, AND MEANING IN THE CLASSICAL ARCHAEOLOGY OF ANATOLIA by Daniel David Shoup A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Classical Art and Archaeology) in The University of Michigan 2008 Doctoral Committee: Professor Elaine K. Gazda, Co-Chair Professor John F. Cherry, Co-Chair, Brown University Professor Fatma Müge Göçek Professor Christopher John Ratté Professor Norman Yoffee Acknowledgments Athena may have sprung from Zeus’ brow alone, but dissertations never have a solitary birth: especially this one, which is largely made up of the voices of others. I have been fortunate to have the support of many friends, colleagues, and mentors, whose ideas and suggestions have fundamentally shaped this work. I would also like to thank the dozens of people who agreed to be interviewed, whose ideas and voices animate this text and the sites where they work. I offer this dissertation in hope that it contributes, in some small way, to a bright future for archaeology in Turkey. My committee members have been unstinting in their support of what has proved to be an unconventional project. John Cherry’s able teaching and broad perspective on archaeology formed the matrix in which the ideas for this dissertation grew; Elaine Gazda’s support, guidance, and advocacy of the project was indispensible to its completion. Norman Yoffee provided ideas and support from the first draft of a very different prospectus – including very necessary encouragement to go out on a limb. Chris Ratté has been a generous host at the site of Aphrodisias and helpful commentator during the writing process.
    [Show full text]
  • Yer-18-1-1-0806-2:Mizanpaj 1
    Turkish Journal of Earth Sciences (Turkish J. Earth Sci.), Vol. 18, 2009, pp. 1–27. Copyright ©TÜBİTAK doi:10.3906/yer-0806-2 First published online 07 July 2008 Geochemical Characteristics of Mafic and Intermediate Volcanic Rocks from the Hasandağ and Erciyes Volcanoes (Central Anatolia, Turkey) AYKUT GÜÇTEKİN & NEZİHİ KÖPRÜBAŞI Department of Geological Engineering, Kocaeli University, TR–41040 İzmit, Turkey (E-mail: nezihi@ kocaeli.edu.tr) Received 23 June 2007; revised typescript received 24 November 2007; accepted 07 December 2007 Abstract: Hasandağ and Erciyes stratovolcanoes, which are the two important stratovolcanoes in Central Anatolia, erupted volcanic products with both calc-alkaline and alkaline compositions, although the calc-alkaline activity is more widespread. There are three stages of geochemical evolution in the history of the Hasandağ stratovolcanic complex: (1) Keçikalesi tholeiitic volcanism, (2) Hasandağ calc-alkaline volcanism, and (3) Hasandağ alkaline volcanism. The geochemical evolution of Erciyes volcanic complex also exhibits three distinct evolutionary stages: (1) Koçdağ alkaline volcanism, (2) Koçdağ calc-alkaline volcanism and (3) Erciyes calc- alkaline volcanism. The volcanic rocks from both suites show enrichments in LREE relative to HREE. The rocks as a whole show enrichments in large ion lithophile elements (LILE) relative to high field strength elements (HFSE) in N-MORB normalized multi- element diagrams, although the thoeliitic and alkaline rocks have less pronounced effects of HFSE/LILE fractionation comparing to the calc-alkaline rocks. Theoretical fractionation models obtained using the whole-rock trace element data indicate two distinct fractionation trends for the Hasandağ volcanism: amphibole and plagioclase fractionation for the tholeiitic and calc-alkaline rocks and plagioclase, pyroxene and amphibole fractionation for the alkaline rocks.
    [Show full text]
  • MOUNTAINEERING in TURKEY DAGCILIK Turkey's Mountaineering Map
    Mountaineering, Turkey-Adiyamanli.org wysiwyg://38/http://www.adiyamanli.org/mountaineering_turkey.h MOUNTAINEERING IN TURKEY DAGCILIK Turkey's Mountaineering Map A glance at a topographical map of Turkey immediately reveals that this is a country of mountains. Rising in all four directions, mountains encircle the peninsula of Anatolia. A part of the Alpine-Himalayan mountain range, Turkey has mountainous regions of different geological formations. The North Anatolian range skirts the Mediterranean shore. Turkey's magnificent mountains and forests are mostly undeveloped, existing as wonderful natural preserves for an extraordinary variety of wildlife, flora and fauna. Two of Turkey's most famous peaks are volcanoes, both inactive, Mt. Erciyes in Kayseri in Central Anatolia (3917 m) and Mt. Agri (Mt. Ararat 5137 m) in the East. Other well-known mountain ranges are the Rize-Ka‡kar (3932 m) in the Eastern Black Sea region, Nigde-Aladag (3756 m) in the Central Taurus range, and the Cilo and Sat Mountains (4136 m) near Hakkari in the Eastern Taurus. The mountainous nature of the country has influenced its cultural evolution. For centuries, nomads and semi-nomadic peoples have migrated annually to the fresh pastures of the higher elevations in the summer. These alpine meadows, called yayla, still represent a firm tie to traditional culture. For climbers and those interested in mountain geography, Turkey offers a wealth of exploration. Glaciers, volcanoes, and peculiar geological formations such as kars prove irresistible to researchers and students of geology. The challenging terrain offers great opportunities for aficionados of outdoor sports who find interesting experiences on the mountains of Eastern, Central and Southern Turkey.
    [Show full text]
  • Etude Volcano-Structurale Du Volcan Nemrut (Anatolie De L'est, Turquie)
    Etude volcano-structurale du volcan Nemrut (Anatolie de l'Est, Turquie) et risques naturels associ´es Inan Ulusoy To cite this version: Inan Ulusoy. Etude volcano-structurale du volcan Nemrut (Anatolie de l'Est, Turquie) et risques naturels associ´es. Volcanologie. Universit´eBlaise Pascal - Clermont-Ferrand II, 2008. Fran¸cais. <NNT : 2008CLF21855>. <tel-00730602> HAL Id: tel-00730602 https://tel.archives-ouvertes.fr/tel-00730602 Submitted on 10 Sep 2012 HAL is a multi-disciplinary open access L'archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destin´eeau d´ep^otet `ala diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publi´esou non, lished or not. The documents may come from ´emanant des ´etablissements d'enseignement et de teaching and research institutions in France or recherche fran¸caisou ´etrangers,des laboratoires abroad, or from public or private research centers. publics ou priv´es. Numéro d’Ordre: D.U. 1855 UNIVERSITE BLAISE PASCAL – CLERMONT FERRAND II U.F.R. Sciences et Technologies ECOLE DOCTORALE DES SCIENCES FONDAMENTALES N° 577 THESE présentée pour obtenir le grade de DOCTEUR D’UNIVERSITE Spécialité : Volcanologie Par ULUSOY İnan Master Etude volcano-structurale du volcan Nemrut (Anatolie de l’Est, Turquie) et risques naturels associés Soutenue publiquement le 18 Septembre 2008, devant la commission d’examen Président : LENAT Jean-François Université Blaise Pascal - Clermont-Ferrand Examinateur : YÜRÜR Tekin Université
    [Show full text]
  • Ruins from the Extractive Era Nemestudio and the Curatorial Team Extractivist Era, Ruin, Waste
    PAVILION OF TURKEY LA BIENNALE DI VENEZIA EXHIBITION ARCHITECTURE INTERNATIONAL 17TH ↳ RUINS FROM Episodes 9 THE EXTRACTIVE ERA NEMESTUDIO AND THE CURATORIAL TEAM PAVILIONOFTURKEY21 ● IKSV ● ORG WWW ● ● WWW 17TH INTERNATIONAL ARCHITECTURE EXHIBITION ARCHITECTURE INTERNATIONAL 17TH Episodes4 Words by: Keywords: PAVILION OF TURKEY LA BIENNALE DI VENEZIA RUINS FROM THE EXTRACTIVE ERA NEMESTUDIO AND THE CURATORIAL TEAM EXTRACTIVIST ERA, RUIN, WASTE ●3 ●5 ●6 ●4 ●8 ●2 ●7 ●1 2 Image: Image: NEMESTUDIO, Four Dioramas, 2021. Diorama of Logistics. Courtesy of NEMESTUDIO. ●1 Ancient marble quarry as ruin ●2 Open-air museum ●3 Mount Ararat spoil tip 1 ●4 Mount Süphan spoil tip ●5 Mount Erciyes spoil tip ●6 Cooling tower replicas from the ancient nuclear power plants ●7 Replica fragment of the ancient Ilısu Dam 2 ●8 Ancient statue from Mount Nemrut 3 1 Mount Ararat is a passive double-peaked stratovolcano and Turkey’s easternmost and largest mountain located at the border between Turkey, Armenia, and Iran. It is considered a sacred mountain by all the three nations and their cultures. 2 Ilısu Dam is a recently activated dam on the Tigris River in southeastern Turkey. Upon its completion, 199 settlements and more than 300 mounds were flooded along with Hasankeyf, a 15,000-year-old village hosting different ethnicities and ancient artifacts. The tomb of Zeynel Bey and 800-year-old Artuklu Hamam are amongst the artifacts that have been relocated due to the flood. Unfortunately, the effects of the flood are unpredictable and still felt by many today; some of the locals are settled in tents and containers lacking infrastructures in the midst of the COVID-19 pandemic.
    [Show full text]
  • The Late PPNB “World” Systems in Northern Mesopotamia and South Levant
    Anejos a CuPAUAM 3, 2018, pp. 45-68 http://dx.doi.org/10.15366/ane3.rubio2018.004 The Late PPNB “World” Systems in Northern Mesopotamia and South Levant: agglomeration, control of long distance exchange and the transition of early religious centers to central villages El Sistema “Mundial” del PPNB Final en el Norte de Mesopotamia y el Sur del Levante: Aglomeraciones, control del intercambio a larga distancia y transición de los primeros centros religiosos a poblados centrales Jesús Gil Fuensanta1 Alfredo Mederos Martín2 Abstract During the Aceramic Neolithic (PPN) period of the Near East, many economic and societal changes took place. During the PPNA is when we recognize a process of agglomeration of hundreds people in big sites such as Jericho. The archaeo- logical record proves more than likely contacts between the contemporary societies of the Levant and some Eastern and Central Anatolian sites. The extent of those far contacts is hard to estimate, but we assume that such contacts and the trade network, which we can study mainly through the obsidian trade, using terrestrial and maritime routes, with the interaction of big villages though a few intermediary steps, already full operating at that time, must have helped to transform the local hierarchies, economic interdependences and rituals, and for instance it could accelerated the end of Göbekli Tepe around mid PPNB. And therefore during the Late PPNB consolidated the central villages, key nodes in the trade networks, and these, in different ecological regions, reached between 10 and 15 ha, v. gr. in Basta, Beisamoun or ‘Ain Ghazal. And in such a way, those built interdependent Ancient “World” Systems.
    [Show full text]
  • Istanbul Technical University Graduate School of Science
    ISTANBUL TECHNICAL UNIVERSITY Æ GRADUATE SCHOOL OF SCIENCE ENGINEERING AND TECHNOLOGY THE GEOLOGY, PETROLOGY AND THERMOCHRONOLOGY OF ILICA- ŞAMLI (SOLARYA) VOLCANO-PLUTONIC COMPLEX AND ITS SIGNIFICANCE ON WESTERN ANATOLIAN GEODYNAMICS PhD THESIS Alp ÜNAL Department of Geological Engineering Geological Engineering Programme NOVEMBER 2019 ISTANBUL TECHNICAL UNIVERSITY Æ GRADUATE SCHOOL OF SCIENCE ENGINEERING AND TECHNOLOGY THE GEOLOGY, PETROLOGY AND THERMOCHRONOLOGY OF ILICA- ŞAMLI (SOLARYA) VOLCANO-PLUTONIC COMPLEX AND ITS SIGNIFICANCE ON WESTERN ANATOLIAN GEODYNAMICS PhD THESIS Alp ÜNAL (505132301) Department of Geological Engineering Geological Engineering Programme Thesis Advisor: Prof. Dr. Şafak ALTUNKAYNAK NOVEMBER 2019 ISTANBUL TEKNİK ÜNİVERSİTESİ Æ FEN BİLİMLERİ ENSTİTÜSÜ ILICA-ŞAMLI (SOLARYA) VOLKANO-PLÜTONİK KOMPLEKSİNİN JEOLOJİSİ, PETROLOJİSİ, TERMOKRONOLOJİSİ VE KB ANADOLU JEODİNAMİGİNDEKİ YERİ DOKTORA TEZİ Alp ÜNAL (505132301) Jeoloji Mühendisliği Anabilim Dalı Jeoloji Mühendisliği Programı Tez Danışmanı: Prof. Dr. Şafak ALTUNKAYNAK KASIM 2019 To my beloved family, vii viii FOREWORD First of all, i would like to thank my advisor, Prof. Dr. Şafak ALTUNKAYNAK; this thesis and all my acedemic background would not be possible without her limitless guidance, support and especially encouragement throughout my not only academic but also entire life. I know, from the bottom of my heart, that this simple “thank you” is not enough. I have been and always will be more than proud to be her student… My special thanks belong to my “family” Işıl Nur GÜRASLAN and Ömer KAMACI, who are not any different from sister and brother which I do not have in my non- academic life. Without their support and patience, this thesis would not be succesful. They will always stay as an important part of my life.
    [Show full text]
  • Revista De Turismo Y Patrimonio Cultural
    Volumen 10 • Número 5 • 2012 Revista de Turismo y Patrimonio Cultural www.pasosonline.org ISSN 1695 - 7121 PASOS. REVISTA DE TURISMO Y PATRIMONIO CULTURAL GUÍA DE ESTILO PARA AUTORES Revista indexada en: DOAJ; Latindex; ISOC; Redalyc; DICE; E-Revistas; CAB-Abstract PASOS. Revista de Turismo y Patrimonio Cultural es una Texto: El texto debe ser escrito a 1,5 de espaciado y publicación en web que se especializa en el análisis con una extensión de 5.000 a 9.000 palabras para académico y empresarial de los distintos procesos que artículos y de 3.000 a 5.000 tanto para opiniones y se desarrollan en el sistema turístico, con especial ensayos como para notas de investigación, incluyendo interés a los usos de la cultura, la naturaleza y el Título, Datos Biográficos de los autores, Resumen, territorio, la gente, los pueblos y sus espacios, el Introducción, los apartados que se estimen oportunos, patrimonio integral. Desde una perspectiva inter y Conclusión, Agradecimientos (si fuera pertinente) y transdisciplinar solicita y alienta escritos venidos desde Bibliografía. las ciencias y la práctica administrativo‐empresarial. Su Cuadros, Gráficos e Imágenes: los artículos pueden objetivo es cumplir con el papel de foro de exposición y incluir cualquier grafismo que se estime necesario. discusión de metodologías y teorías, además de la Deberán estar referidos en el textos y/o situados divulgación de estudios y experiencias. Pretende convenientemente y acompañados por un pie que los contribuir a otros esfuerzos encaminados a entender el identifique. Pueden utilizarse colores, pero ha de turismo y progresar en las diversas formas de tenerse en consideración la posibilidad de una prevención de efectos no deseados, pero también publicación en soporte papel en blanco y negro.
    [Show full text]
  • Geological and Geomorphological Evaluation of Melendiz Stream Basin1
    IOSR Journal Of Humanities And Social Science (IOSR-JHSS) Volume 25, Issue 2, Series. 8 (February. 2020) 19-29 e-ISSN: 2279-0837, p-ISSN: 2279-0845. www.iosrjournals.org Geological and Geomorphological Evaluation of Melendiz Stream Basin1, Halil Mesut BAYLAK2 Abstract: The research area is the Melendiz Stream Basin in Aksaray. Melendiz Stream Basin is located in the Lake Tuz Closed (Endorheic) Basin. The Ihlara Valley part of the basin is included in the Cappadocia tourism zone. Paleozoic, Mesozoic, Tertiary and Quaternary formations are observed in the study area and its immediate surroundings. Mount Hasan, Melendiz Mountain, Mount Keçiboyduran, Mount Göllü and Mount Kulaklı volcanoes have been influential on these formations. Major morphological elements that draw attention are mountainous and hilly areas, piedmont plains that we see in the east of the Çiftlik district and Ihlara Canyon Valley. The Fairy Chimneys, the horizontal forms of the formations (terrace sets), the covert appearance of the Mount Hasan ash, the thin but widespread outcrop of the travertines along the fault lines, constituted the present geomorphological structure of the erosion research area whose effects are observed. Göğüs Stream which is the largest tributary of Melendiz Stream forms the main stream of the basin. The Stream drains an area of approximately 565.2 km2 that we have identified with all of its tributaries. In Melendiz Stream, dendritic drenage is observed in the areas where the lateral tributaries reunite; braided drenage is observed along main stream
    [Show full text]
  • Türkiye'de Volkanizma Ve Volkanik Yerşekilleri
    TÜRKİYE'DE VOLKANİZMA VE VOLKANİK YERŞEKİLLERİ Özdoğan SÜR Magmanın yerkabuğuna doğru yükselmesi olayına volkanizma denir. Şayet, mağma yerkabuğu içinde kalırsa "derinlik volkaniz- ması", yeryüzüne ulaşır ise "yüzey volkanizması adı verilir. Volkanizmada esas rolü oynayan, erimiş silikatların gazlarla doygun bir karışımını oluşturan "mağma"'dır. Magmadan ayrılan gazların ve mağmanın yeryüzüne sıvı ya da katı halde ulaştığı baca veya fissür'e "volkan" denir. Dünyanın hareketli bir kuşağı üzerinde yeralan Türkiye, önce­ leri orojenik, daha sonra da epirojienik hareketlere maruz kalmıştır. Bunun bir sonucu olarak, çok kırıklı bir yapıya sahip olan Anado­ lu'da yarık erüpsiyonlan ve merkezi erüpsiyonlar tarih çağlarına ka­ dar devam etmişlerdir. Türkiye tektonik, deprem ve genç volkanik arazilerini gösteren haritalar karşılaştırıldığında, olaylar ve oluşum­ ları arasındaki ilgi açıkça görülmektedir (Haritalar 1, 2, 3). Mesozoik'in sonuna kadar volkanizma ile oluşan volkanik ara­ zi, zamanla aşınarak silinmiştir. III. Zaman'm ilk yansına (Paleo- jen'e) ait volkan topografyası çok aşınmıştır. III. Zaman'ın ikinci yansına (Neojen'e) ve IV. Zaman'a ait volkan reliefı ise Türkiye'de belirgindir. Faaliyet özelliklerine göre, ya Türkiye'nin en yüksek dağlannı meydana getirmişler, ya da geniş lâv platolan oluşturmuş­ lardır. Zamanla, bir kısım volkanik arazinin aşınmasından ise, Iç Anadolu'da olduğu gibi, Dünya'nın en ilginç topografyası meydana gelmiştir. Bunlara, volkanik infilâklar ile oluşan patlama kraterleri­ ni, maarlan ve diğerlerini de ilâve etmek mümkündür. Türkiye'de Neojen ve Kuatemer volkanizması ile meydana ge­ len volkanik arazinin dağılışı, Türkiye tektonik haritası ile karşılaş- 30 Türkiye'de Volkanizma ve Volkanik Yerşekilleri tınldığında, iki olay arasındaki yakın ilgi dikkat çekmektedir. Kı- nklann egemen olduğu Batı Anadolu, İç Anadolu, Doğu Anadolu ve Güneydoğu Anadolu Bölgeleri aynı zamanda Neojen ve Kuater- ner volkanizmalannın da yer aldığı, dolayısıyle volkanik reliefin bulunduğu yerlerdir.
    [Show full text]
  • USGS Open-File Report 2009-1133, V. 1.2, Table 3
    Table 3. (following pages). Spreadsheet of volcanoes of the world with eruption type assignments for each volcano. [Columns are as follows: A, Catalog of Active Volcanoes of the World (CAVW) volcano identification number; E, volcano name; F, country in which the volcano resides; H, volcano latitude; I, position north or south of the equator (N, north, S, south); K, volcano longitude; L, position east or west of the Greenwich Meridian (E, east, W, west); M, volcano elevation in meters above mean sea level; N, volcano type as defined in the Smithsonian database (Siebert and Simkin, 2002-9); P, eruption type for eruption source parameter assignment, as described in this document. An Excel spreadsheet of this table accompanies this document.] Volcanoes of the World with ESP, v 1.2.xls AE FHIKLMNP 1 NUMBER NAME LOCATION LATITUDE NS LONGITUDE EW ELEV TYPE ERUPTION TYPE 2 0100-01- West Eifel Volc Field Germany 50.17 N 6.85 E 600 Maars S0 3 0100-02- Chaîne des Puys France 45.775 N 2.97 E 1464 Cinder cones M0 4 0100-03- Olot Volc Field Spain 42.17 N 2.53 E 893 Pyroclastic cones M0 5 0100-04- Calatrava Volc Field Spain 38.87 N 4.02 W 1117 Pyroclastic cones M0 6 0101-001 Larderello Italy 43.25 N 10.87 E 500 Explosion craters S0 7 0101-003 Vulsini Italy 42.60 N 11.93 E 800 Caldera S0 8 0101-004 Alban Hills Italy 41.73 N 12.70 E 949 Caldera S0 9 0101-01= Campi Flegrei Italy 40.827 N 14.139 E 458 Caldera S0 10 0101-02= Vesuvius Italy 40.821 N 14.426 E 1281 Somma volcano S2 11 0101-03= Ischia Italy 40.73 N 13.897 E 789 Complex volcano S0 12 0101-041
    [Show full text]