Asst. Prof. İNAN ULUSOY

Total Page:16

File Type:pdf, Size:1020Kb

Asst. Prof. İNAN ULUSOY Asst. Prof. İNAN ULUSOY OPfefricseo Pnhaol nIen:f +or9m0 3a1t2io 2n97 7700 Extension: 136 EFmaxa iPl:h oinnaen:@ +h9a0ce 3tt1e2p e2.9ed9u 2.t0r34 Education Information DPoosctt oDroacteto, rHaatcee, tLtuepned sÜ Unnivievresristieesti ,( MLuünhde nUdniisvliekr sFiatyk)ü, lFteasciu, Jletyo lOofj iS Mciüenhceen,d Diselpiğai rBtmöleünmt üO f/ GMeionleorgayl,o Sjiw Peedtreong 2r0af0i 8A -b 2d0,09 DTuorcktoerya 2te0,0 U2n -i v2e0r0si9té Blaise Pascal: Clermont-Ferrand Iı, Sciences De La Terre, Laboratoire Magmas Et Volcans, France P2o0s0t4g r-a 2d0u0a8te, Hacettepe Üniversitesi, Mühendislik Fakültesi, Jeoloji Mühendisliği Bölümü / Mineraloji Petrografi Abd, UTunrdkeeryg r1a9d9u9a t-e 2, 0H0a2cettepe Üniversitesi, Mühendislik Fakültesi, Jeoloji Mühendisliği Bölümü, Turkey 1994 - 1999 Foreign Languages EFnregnlicsh,, BC1 AIndtvearmnceeddiate Research Areas SGeeiosmteochlongicya, lE Eanrtghinqeuearkien gS,e Gisemoogrloagpyh, iAc pInpfloierdm Gaetiopnh Syyssictesm, Esl,e Rctermo oMtea gsneentsiicn agn, Idm Ealgeect Prircoacl eMsseitnhgo, dGse, oGpehoylosgiciacal lEngineering, gEenogliongeye,r sinogil,s G),e Mneinrearl aGleooglyo-gpye,t rGoegoraarpchye,o Ploegtryo, gSrtraupchtyu raanld G Peeotlrooglyo, gSyu, r3fDic-iaMl oGdeeolliongy, E (nggeionmeeorripnhg oalnodg yT, eqcuhantoerlongayry ALeccatudrerm PihcD T, Hitalceestt e/p Te aÜsnkivsersitesi, Mühendislik Fakültesi, Jeoloji Mühendisliği Bölümü, 2010 - Continues CMoinuerasleogsy-Petrography, Undergraduate, 2016 - 2017 Advising Theses PUoLsUtSgOraYd İu.,a Dteo, ğCu.D AİnKaEdRo(lSut uvdoelknatn),l a2r0ın1ı4n termal kızılötesi uydu görüntüleri ile uzun süreli termal aktivitesinin gözlenmesi, AIr. ticSlheoss Phuonbiltiisch veodlc ainn iJsomu orfn tahles BTohdartu Emn ctaelrdeedra S (CSIW, S TSuCrIk eayn)d: HAyHbrCiId iIznadtieoxne osf enriched mantle- dÇUerBiUvKeÇdU a Hn.d E c. ,r AuYsDtaAl Rm Ee.,l tUsLUSOY İ., Gourgaud A. II. VJOoUlRcaNnAiLc OuFn rAeSsIAt Np oEsAsRibTiHli tSiCeIsE NinC ErSe,s vpool.n2s1e9 , t2o0 r2e1c (eJnout rOnbarl uInkd esxeeisdm inic S CswI)arm on and around Hasandag sAtYrDaAtoRv Eo.l, cDaİnKoE R( Ce., nUtLrUaSl OAYn İa., tŞoElNia ,E T.urkey) III. VCOoMlcPaTnEicS eRrEuNpDtUioSn G eEyOeS-CwIEiNtnCeEs, sveodl.3 a5n3d, n roe.1c,o prpd.1e-d1 8b,y 2 0p2r1e h(iJsotuorrniacl hInudmexaends in SCI) QUULUASTOEYR Nİ.,A SRaYr ıSkCayIEaN MC.E A R. ,E SVcIhEmWitSt, Avo. Kl.2. ,1 Ş2E, Npp E.1., 8D7a-n1i9s8ik, 2M0.,1 G9Ü (MJoÜuŞr nEa.l Indexed in SCI) IV. Tuemrkpeoyr)a ul sriandgi aAtSivTeE Rhe iamt afgluexr yestimation and alteration mapping of Tendurek volcano (eastern JUOLUURSNOAYL İ .OF VOLCANOLOGY AND GEOTHERMAL RESEARCH, vol.327, pp.40-54, 2016 (Journal Indexed in SCI) V. STwimeed-elanpse electrical resistivity tomography of a water infiltration test on Johannishus Esker, HUlYuDsoRyO GI.,E DOaLhOliGnY T J.O, BUERRNGAMLA, vNo lB.2.3, no.3, pp.551-566, 2015 (Journal Indexed in SCI) VI. TIduernkteiyfying the Volcanic Eruption Depicted in a Neolithic Painting at Catalhoyuk, Central Anatolia, PSCLHOSM OITNTE A, v. oKl.. 9, D, nAoN.1IS, 2IK0 1M4., (AJoYuDrAnRa lE I.n, ŞdEeNxe Ed. ,i nU LSUCSI)OY İ., LOVERA O. M. VII. MULuUltSiO-dYi İr.,e LcAtiBoAnZaUl Yd ePr., iAvYaDtiAoRn Eo.f self-potential/elevation gradient (Ce) maps - swirl procedure VIII. AN ERAhRi nSoUcReFrAoCtEid G SEkOuPlHl YCSoICoSk, evdo-l.t1o1-,D neoa.3t,h p ipn.2 a7 59-.228 2M, a2-0O1l3d (IJgonuirmnabl rIintdee Fxelodw in o SfC TI)urkey 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. IX. 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) X. SJOTUcRoNrrA:L A OnF IVDOLL CcoAdNeO LfoOrG Yim AaNgDe GbEaOsTeHdE nRoMrAmLa RliEzSaEtiAoRnC Hof, vloalp.2s4e5 r, aptpe.2 a1n-3d9 ,i l2lu01m2i n(Jaotuiorna el fInfedcetxse do nin SCI) nUiLgUhStOtiYm İe., LTAIBRA iZmUaYg Pe.r, yAYDAR E. XI. MCOtM. NPeUmTErRuSt &vo GlEcaOnSCoI E(NEaCsEtSe, rvno l.T4u3r, pkpe.y6)3:- 7T2e,m 20p1o2r a(lJ opuertnraol lIongdiecxaeld e ivno SlCuIt)ion 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) XII. UPaNlEeSoCgOeo: gCraaspeh oicf atlh Re ePcloanins torfu cXtaionnth aonsd a nMda nLaegtoeomne n(Tt uCrhkaellye)nges of an Archaeological Site Listed by JFOoUuRaNchAeL E O., FE cEoAcRhTaHrd S EC.I, EKNuCzEu,c vuolg.2lu1 ,C p.,p C.2a3rc4a-u2d3 6N, .2, E0K10M (EJKoÇuİr nMa.,l UInludseoxye dI. ,i nC iSnCeIr) A., Cavalier L., des Courtils J. XIII. 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 XIV. TSCeIx)ture discrimination of volcanic ashes from different fragmentation mechanisms: A case study, MERoSuOnYt ON., eCmHrINuGt As tGr.a, tAoYvDoAlcRa En.,o G, OeUaRstGeArUnD T Au.r, kCeuybukcu H. E. , Ulusoy I. XV. 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) XVI. pMoosrspibhloel oimgipcacl ta anraelyassi so fo fu atcutrivee e Mruoputniotn Nemrut stratovolcano, eastern Turkey: evidences and JAOYUDRANRA EL. ,O GFO VUORLGCAAUNDO AL.O, UGlYu sAoNyD I. ,G DEIOGTOHNENREMTA FL., RLAESBEAAZRUCYH P, .v, Soel.n1 2E3.,, Bpapy.3h0a1n- 3H1., 2K, u2r0t0ta3s (TJ.o, uTrOnLaLl UInOdGeLxUe dA .in SCI) AIr. ticHleasfi fP buirb lİiHsAh eilde ibnir O Atçhıke rM Jaoduernn Oaclasğının 3B Çok-bakılı Stereo Modellemesi, (3D Multi-view Stereo MULoUdSeOlYli nİ.g, Ş oEfN a En., TOUpNeCnE MR iAn.e, S PÖiNt MUEsZin Hg. ,a B Layighhantw He.ight UAV) II. 3TüDr kMiyuel tJie-ovlioejwi B Sütlteernei,o v oMl.o60d,e pllpi.n2g2 5o-f2 4a5n, 2O0p1e7n ( MReinfeer ePeidt JUosuirnnga las oLfi gOhthtwere Iingshttit uUtAioVns) TUULRUKSOIYYE İ .J,E ŞOELNO EJI. , BTUULNTCEENRI -AG.E, SOÖLNOMGIECZA HL .B, BUALYLHETAINN HO.F TURKEY, vol.60, no.2, pp.223-241, 2017 (Journal Indexed III. Pina ElaSeCoI)geographical reconstruction and management challenges of an archaeological site listed by UFONUEASCCHOE : E t.h, EeC cOaCsHeA oRfD t hE.e, KLUeZtUoCoUnO sĞhLrUin Ce., iCnA RthCeA UXDan Nt.h, Eoksm Pelmaienk ç(iT Mu.r, kUeLyU)SOY İ., Çinener A., DES COURTİLS J. IV. DQuaağeıtsıtlimonıeşs A Gneaohgtrarplhaimcaael, ıv Öolz.3d1ir, neon.ç1 ,G pöpr.3ü7n-4tü9l, e2m01e2 S (iRsteefemrieed Journals of Other Institutions) YUeLrUbSilOimY lİe.,r Ai, RvToUl.3N3E, Rp pH.2., 0A5y-d2a1r8 E, 2.012 (Other Refereed National Journals) V. eRte Lcoéntôsotintu dtiaonns pl’aalnécoigeénonger Lapychiieq u(Te udreqsu diey)n :a mprieqmueiesr psa ryéssauglètartess durant l’Holocène autour de Xanthos NÉcoorcohisa,r vdo Él.2., 1F3o,u naoc.h4e, pÉp., .5K9u-z7u1c,u 2o0ğ0lu9 C(.R, Cefaerrceaeudd JNou., rEnKaMlsE oKfÇ Oİ tMhe.,r U ILnUstSitOuYti oİ.,n Çsİ)NER T. A. , Courtils J. D. 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, Refereed Congress / Symposium Publications in Proceedings I. AYnDalIoNg Eu.,e U aLnUdSO NYu İm., AeKrKicAaŞl Em.odelling of double-piston piecemeal calderas Cities on Volcanoes 10, Napoli, Italy, 2 - 07 September 2018, pp.830 II. CMriycsrtoaslcso fpriocm M Coanpitpoardinogc ioanf LAalbteorreadt oIrgyn iBmabsreidte Psh (yTsuicrakle Dy)isintegration Ratio of Fibrous Zeolite CAiKtiKesA Şo nE .V, ÇoUlcBaUnoKeÇsU 1 H0., EN. a, pEoRlKi, UItTa lVy,. ,2 A -K 0IN7 SKeApRteAmKÜbeLrA 2H0 L1.8, Y, pUpR.D11A1K7UL Y., ULUSOY İ., ŞEN E. III. MSeolfu-nPto Hteanstaianl,, TSurrkfaecye Temperature, CO2 measurements and related structural discontinuities on CDiİtKieEsR o Cn. ,V UoLlcUaSnOoYe sİ. ,1 A0K, NKAapŞo Eli.,, Ş2E -N 0 7E .,S ÇeUptBeUmKbÇeUr H20. E1.8 ,, GpÜpM.52Ü1Ş E., BAŞAR O., AYDIN E., ERKUT V., KAYGISIZ N. IV. aRgeev epaeloinpgle the age of a volcanic eruption in the Kula volcanic field (Turkey) eyewitnessed by Bronze- CUiLtiUeSs OoYn İV., oSlAcaRnIKoAesY A10 M, 2. A - . 0, 7S cShemptitetm Ab. eKr. ,2 Ş0E1N8 E., Danisik M., GÜMÜŞ E. V. LAoKwIN TKeAmRApKerÜaLtAuHr eL .A, ÇltUeBrUaKtiÇoUn Ho.f E Z. ,e AlvKeK AIgŞn Eim., YbUrRitDeA (KCUaLp Yp.a, EdRoKciUaT) VU.,n UdLeUrS EOxYp İ.e, rŞiEmNe En.tal Conditions VI. HEuyrdorpoetahne Grmeoaslc ifelnucides c Uirnciounla Gtieonne raanl Ads sstermubcltyu 2r0a1l 8d,i Vsciyoanntai,n Auuitsiterisa ,o 8n - M13o uAnprt ilH 2a0s1a8n, Turkey: preliminary rDeİKsuElRt sC.., ULUSOY İ., AKKAŞ E., ŞEN E., ÇUBUKÇU H. E. , GÜMÜŞ E., Başar O., Aydın E., Erkut V., Kaygısız N. VII. IEnu rsoitpue aanp Gpeliocsactiieonnce os fU Unliotrna Gsoenneicra Pl uAlssse mVbellyo 2c0it1y8 m, 8e -a 1s3u rAepmriel n20ts1 8to determine the degree of zeolitic aÇlUtBerUaKtÇioUn H o. Ef . i,g Ynuirmdbakruitle Y., Erkut V., AKKAŞ E., AKIN KARAKÜLAH L., ULUSOY İ., ŞEN E. VIII. TEuorpoopgeraanp Gheioc smcieondceelsl iUnngi oonf Gcaenldeerarla
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]
  • 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
    [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]