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A NEW MEDIUM TO HIGH ENTHALPY GEOTHERMAL FIELD IN AEGEAN REGION (AKYAR) MENDERES – SEFERİHİSAR – İZMİR, WESTERN ANATOLIA, TURKEY

Yıl 2013, Cilt: 147 Sayı: 147, 153 - 167, 01.12.2013

Öz

There are also geothermal areas of low and medium enthalpy besides the high-temperature geothermal fields in the Western Anatolia. These areas are important for thermal tourism and agricultural applications. According to the surface temperature at by the lowtemperature action for known fluid high temperature fluid can be provided. They are the purpose of the study. The study area between the towns of Mendere and Seferihisar. These districts are located south-southwest of Izmir. İnvestigate the potential of geothermal energy and fluid provide covers more than one professional discipline. Field studies, geological prospecting, geothermal energy potential areas detailed geological studies, hydrogeology, hydrogeochemistry, geophysical surveys and drilling completed. As a result of studies, conducted exploratory drilling to a depth of 1215.50 m around Akyar Tepe. Maximum temperature of 141,18 oC in the well. Fluid flow rate of 104 tons/hour water and water vapor is obtained with compressor machine. Hot water, sodium chloride water category. It consists of a mixture of hot water, surface water and sea water. In this field for many years, known as low-temperature. In this study, medium - high enthalpy geothermal system as revealed

Kaynakça

  • Başarir, E., Konuk, Y.T. 1982. Gümüldür yöresinin kristalin temeli ve allokton birimleri. Türkiye Jeoloji Kurumu Bülteni 24, 1–6.
  • Bozkurt, E., Park, R.G. 1994. Southern Menderes Massif: an incipient metamorphic core complex in western Anatolia, Turkey. Journal of Geological Society 151, 213-216.
  • Borsi, S., Ferrara, G., Innocenti, F., Mazzuoli, R. 1972. Geochronology and Petrology of Recent Volcanics in the Eastern Aegean sea (West Anatolia and Leovos Island). Bulletin of Volcanology 36, 473–496.
  • Bulut, M., Büyükboyaci, Ü., Dünya H. 2013. Akyar- Ilikpinar (Seferihisar-Menderes-İzmir) ruhsat sahalarinin jeotermal etüt (Jeoloji-Jeofizik) ve Akyar İSA-2011/10 jeotermal arama sondaji kuyu bitirme raporu. Maden Tetkik Arama Genel Müdürlüğü,109, (unpublished) Ankara.
  • Dora, O., Kun, N., Candan, O. 1990. Metamorphic history and geotectonic evolution of the Menderes massif. International Earth Sciences Congress on Aegean Regions, İzmir-Turkey, Proceedings, 102–115.
  • Emre Ö., Özalp S., Doğan A., Özaksoy V., Yildirim C., Göktaş F. 2005. İzmir yakin çevresinin diri faylari ve deprem potansiyelleri. Maden Tetkik Arama Genel Müdürlüğü Rapor No: 10754, 80, (unpublished) Ankara.
  • Erdoğan, B. 1990. İzmir-Ankara Zonu’nun, İzmir ile Seferihisar Arasindaki Bölgede Stratigrafik Özellikleri ve Tektonik Evrimi. Türkiye Petrol Jeologları Dergisi Bülteni 2/1, 1–20.
  • Eşder, T. 1988. Gümüldür-Cumaovasi (İzmir) alaninin jeolojisi ve jeotermal enerji olanaklarinin araştirilmasi. PhD Thesis, İstanbul Üniversitesi. Fen Bilimleri Enstitüsü, Jeoloji Mühendisliği Bölümü Anabilim Dali, 401 p. (unpublished).
  • Eşder, T, Şimşek, Ş. 1975. İzmir (Seferihisar) alani, Çubukludağ grabeni ile dolaylarinin jeolojisi ve jeotermal olanaklari. Maden Tetkik ve Arama Enstitüsü Raporu, 190, (unpublished), İzmir.
  • Fournier, R. O. 1977. Chemical geothermometers and mixing models for geothermal system. Geohthermics, 5, 41-50.
  • Fournier, R. O. 1979. A revised equation for the Na/K geothermometer. Geothermal Res. Council Trans., 3, 221-224.
  • Fournier, R. O., Truesdell, A.H. 1973. An Empirical Na-K-Ca Geothermometer for Natural Waters. Geochimica et Cosmochimica Acta, 37, 1255- 1275.
  • Fournier, R. O., Potter, R. W. 1979. Magnesium correction to the Na-K-Ca chemical geothermometer. Geochimica et Cosmochimica Acta, 43, 1543- 1550.
  • Genç, S.C., Altunkaynak, Ş., Karacik, Z., Yilmaz, Y. 2001. The Çubukludağ graben, Karaburun peninsula: it’s tectonic significance in the Neogene geological evolution of the western Anatolia. Geodinamica Acta 14, 45–55.
  • Giggenbach, W. F. 1988. Geothermal solute equilibria. Derivation of Na-K-Mg-Ca geoindicators. Geochimica et Cosmochimica Acta, 52, 2749- 2765.
  • Güngör, T. 1998. Stratigraphy and Tectonic Evolution of the Menderes Massif in the Söke-Selçuk Region. Doktora Tezi, Dokuz Eylül University.
  • Güngör, T., Erdoğan, B. 2002. Tectonic significance of mafic volcanic rocks in a Mesozoic sequence of the Menderes Massif, West Turkey. International Journal of Earth Science 91, 386–397.
  • Hetzel, R., Ring, U., Akal, C., Troesch, M. 1995. Miocene NNE-directed extensional unroofing in the Menderes Massif, southwestern Turkey. Journal of Geological Society 152, 639–654.
  • Kaya, O. 1979. Ortadoğu Ege çöküntüsünün Neojen stratigrafisi ve tektoniği. Türkiye Jeoloji Kurumu Bülteni 7/22, 35–58.
  • Kaya, O. 1981. Miocene reference section for the coastal parts of West Anatolia. Newsletters on Stratigraphy 10, 164–191 pp.
  • MTA, 2005. Türkiye Jeotermal Kaynaklari Envanteri, Ankara.
  • Okay, A.İ., Siyako, M. 1991. The New Position of the İzmir-Ankara Neo-Tethyan Suture Between İzmir and Balikesir. Proceedings of the Ozan Sungurlu Symposium, Ankara, 333–355.
  • Özer, S., Sözbilir, H. 2003. Presence and tectonic significance of Cretaceous rudist species in the so-called Permo-Carboniferous Göktepe Formation, central Menderes Massif, western Turkey. International Journal of Earth Sciences 92, 397–404.
  • Özgenç, İ. 1978. Cumaovasi (İzmir) asit volkanitlerde saptanan iki ekstrüzyon aşamasi arasindaki göreceli yaş ilişkisi. Türkiye Jeoloji Kurumu Bülteni, 21/1, 31–34.
  • Somay, M. 2006. Hydrogeology of Küçük Menderes River coastal wetland. Dokuz Eylül Üniversitesi Fen Bilimleri Enstitüsü Doktora Tezi, 222. (unpublished).
  • Şengör, A.M.C. 1979. The North Anatolian Transform Fault: its age, offset and tectonic significance. Journal of the Geological Society of London, 136, 269–282.
  • Şengör, A.M.C. 1980. Türkiye’nin neotektoniğinin esaslari, Türkiye Jeoloji Kurumu yayını, 40.
  • Şengör, A.M.C., Satir, M., Akkök, R. 1984. The timing of tectonic events in the Menderes Massif, western Turkey: implication for tectonic evolution and evidence for Pan-African basement in Turkey. Tectonics 3, 693–707.
  • Truesdell, A.H. 1976. Summary of section III geochemical techniques in exploration. Proceedings of second United Nations Symposium on the development and use of geothermal resources. 1975, San Francisco, 1, 53-89 pp.
  • Uzel, B., Sözbilir, H. 2008. A First record of strike-slip basin in western Anatolia and its tectonic implication: The Cumaovasi basin as an example. Turkish Journal of Earth Sciences 17, 559–591.
  • Yilmaz, Y., Genç, S.C., Gürer, O.F., Bozcu M., Yilmaz K., Karacik Z., Altunkaynak Ş., Elmas A. 2000. When did the western Anatolian grabens begin to develop Bozkurt E., Winchester J.A., Piper J.D.A. (Eds.), Tectonics and magmatism in Turkey and the surrounding area, Geological Society of London,

A NEW MEDIUM TO HIGH ENTHALPY GEOTHERMAL FIELD IN AEGEAN REGION (AKYAR) MENDERES – SEFERİHİSAR – İZMİR, WESTERN ANATOLIA, TURKEY

Yıl 2013, Cilt: 147 Sayı: 147, 153 - 167, 01.12.2013

Öz

There are also geothermal areas of low and medium enthalpy besides the high-temperature geothermal fields in the Western Anatolia. These areas are important for thermal tourism and agricultural applications. According to the surface temperature at by the lowtemperature action for known fluid high temperature fluid can be provided. They are the purpose of the study. The study area between the towns of Mendere and Seferihisar. These districts are located south-southwest of Izmir. İnvestigate the potential of geothermal energy and fluid provide covers more than one professional discipline. Field studies, geological prospecting, geothermal energy potential areas detailed geological studies, hydrogeology, hydrogeochemistry, geophysical surveys and drilling completed. As a result of studies, conducted exploratory drilling to a depth of 1215.50 m around Akyar Tepe. Maximum temperature of 141,18 oC in the well. Fluid flow rate of 104 tons/hour water and water vapor is obtained with compressor machine. Hot water, sodium chloride water category. It consists of a mixture of hot water, surface water and sea water. In this field for many years, known as low-temperature. In this study, medium - high enthalpy geothermal system as revealed

Kaynakça

  • Başarir, E., Konuk, Y.T. 1982. Gümüldür yöresinin kristalin temeli ve allokton birimleri. Türkiye Jeoloji Kurumu Bülteni 24, 1–6.
  • Bozkurt, E., Park, R.G. 1994. Southern Menderes Massif: an incipient metamorphic core complex in western Anatolia, Turkey. Journal of Geological Society 151, 213-216.
  • Borsi, S., Ferrara, G., Innocenti, F., Mazzuoli, R. 1972. Geochronology and Petrology of Recent Volcanics in the Eastern Aegean sea (West Anatolia and Leovos Island). Bulletin of Volcanology 36, 473–496.
  • Bulut, M., Büyükboyaci, Ü., Dünya H. 2013. Akyar- Ilikpinar (Seferihisar-Menderes-İzmir) ruhsat sahalarinin jeotermal etüt (Jeoloji-Jeofizik) ve Akyar İSA-2011/10 jeotermal arama sondaji kuyu bitirme raporu. Maden Tetkik Arama Genel Müdürlüğü,109, (unpublished) Ankara.
  • Dora, O., Kun, N., Candan, O. 1990. Metamorphic history and geotectonic evolution of the Menderes massif. International Earth Sciences Congress on Aegean Regions, İzmir-Turkey, Proceedings, 102–115.
  • Emre Ö., Özalp S., Doğan A., Özaksoy V., Yildirim C., Göktaş F. 2005. İzmir yakin çevresinin diri faylari ve deprem potansiyelleri. Maden Tetkik Arama Genel Müdürlüğü Rapor No: 10754, 80, (unpublished) Ankara.
  • Erdoğan, B. 1990. İzmir-Ankara Zonu’nun, İzmir ile Seferihisar Arasindaki Bölgede Stratigrafik Özellikleri ve Tektonik Evrimi. Türkiye Petrol Jeologları Dergisi Bülteni 2/1, 1–20.
  • Eşder, T. 1988. Gümüldür-Cumaovasi (İzmir) alaninin jeolojisi ve jeotermal enerji olanaklarinin araştirilmasi. PhD Thesis, İstanbul Üniversitesi. Fen Bilimleri Enstitüsü, Jeoloji Mühendisliği Bölümü Anabilim Dali, 401 p. (unpublished).
  • Eşder, T, Şimşek, Ş. 1975. İzmir (Seferihisar) alani, Çubukludağ grabeni ile dolaylarinin jeolojisi ve jeotermal olanaklari. Maden Tetkik ve Arama Enstitüsü Raporu, 190, (unpublished), İzmir.
  • Fournier, R. O. 1977. Chemical geothermometers and mixing models for geothermal system. Geohthermics, 5, 41-50.
  • Fournier, R. O. 1979. A revised equation for the Na/K geothermometer. Geothermal Res. Council Trans., 3, 221-224.
  • Fournier, R. O., Truesdell, A.H. 1973. An Empirical Na-K-Ca Geothermometer for Natural Waters. Geochimica et Cosmochimica Acta, 37, 1255- 1275.
  • Fournier, R. O., Potter, R. W. 1979. Magnesium correction to the Na-K-Ca chemical geothermometer. Geochimica et Cosmochimica Acta, 43, 1543- 1550.
  • Genç, S.C., Altunkaynak, Ş., Karacik, Z., Yilmaz, Y. 2001. The Çubukludağ graben, Karaburun peninsula: it’s tectonic significance in the Neogene geological evolution of the western Anatolia. Geodinamica Acta 14, 45–55.
  • Giggenbach, W. F. 1988. Geothermal solute equilibria. Derivation of Na-K-Mg-Ca geoindicators. Geochimica et Cosmochimica Acta, 52, 2749- 2765.
  • Güngör, T. 1998. Stratigraphy and Tectonic Evolution of the Menderes Massif in the Söke-Selçuk Region. Doktora Tezi, Dokuz Eylül University.
  • Güngör, T., Erdoğan, B. 2002. Tectonic significance of mafic volcanic rocks in a Mesozoic sequence of the Menderes Massif, West Turkey. International Journal of Earth Science 91, 386–397.
  • Hetzel, R., Ring, U., Akal, C., Troesch, M. 1995. Miocene NNE-directed extensional unroofing in the Menderes Massif, southwestern Turkey. Journal of Geological Society 152, 639–654.
  • Kaya, O. 1979. Ortadoğu Ege çöküntüsünün Neojen stratigrafisi ve tektoniği. Türkiye Jeoloji Kurumu Bülteni 7/22, 35–58.
  • Kaya, O. 1981. Miocene reference section for the coastal parts of West Anatolia. Newsletters on Stratigraphy 10, 164–191 pp.
  • MTA, 2005. Türkiye Jeotermal Kaynaklari Envanteri, Ankara.
  • Okay, A.İ., Siyako, M. 1991. The New Position of the İzmir-Ankara Neo-Tethyan Suture Between İzmir and Balikesir. Proceedings of the Ozan Sungurlu Symposium, Ankara, 333–355.
  • Özer, S., Sözbilir, H. 2003. Presence and tectonic significance of Cretaceous rudist species in the so-called Permo-Carboniferous Göktepe Formation, central Menderes Massif, western Turkey. International Journal of Earth Sciences 92, 397–404.
  • Özgenç, İ. 1978. Cumaovasi (İzmir) asit volkanitlerde saptanan iki ekstrüzyon aşamasi arasindaki göreceli yaş ilişkisi. Türkiye Jeoloji Kurumu Bülteni, 21/1, 31–34.
  • Somay, M. 2006. Hydrogeology of Küçük Menderes River coastal wetland. Dokuz Eylül Üniversitesi Fen Bilimleri Enstitüsü Doktora Tezi, 222. (unpublished).
  • Şengör, A.M.C. 1979. The North Anatolian Transform Fault: its age, offset and tectonic significance. Journal of the Geological Society of London, 136, 269–282.
  • Şengör, A.M.C. 1980. Türkiye’nin neotektoniğinin esaslari, Türkiye Jeoloji Kurumu yayını, 40.
  • Şengör, A.M.C., Satir, M., Akkök, R. 1984. The timing of tectonic events in the Menderes Massif, western Turkey: implication for tectonic evolution and evidence for Pan-African basement in Turkey. Tectonics 3, 693–707.
  • Truesdell, A.H. 1976. Summary of section III geochemical techniques in exploration. Proceedings of second United Nations Symposium on the development and use of geothermal resources. 1975, San Francisco, 1, 53-89 pp.
  • Uzel, B., Sözbilir, H. 2008. A First record of strike-slip basin in western Anatolia and its tectonic implication: The Cumaovasi basin as an example. Turkish Journal of Earth Sciences 17, 559–591.
  • Yilmaz, Y., Genç, S.C., Gürer, O.F., Bozcu M., Yilmaz K., Karacik Z., Altunkaynak Ş., Elmas A. 2000. When did the western Anatolian grabens begin to develop Bozkurt E., Winchester J.A., Piper J.D.A. (Eds.), Tectonics and magmatism in Turkey and the surrounding area, Geological Society of London,
Toplam 31 adet kaynakça vardır.

Ayrıntılar

Birincil Dil İngilizce
Konular Mühendislik
Bölüm Makaleler
Yazarlar

Metin Bulut Bu kişi benim

Yayımlanma Tarihi 1 Aralık 2013
Yayımlandığı Sayı Yıl 2013 Cilt: 147 Sayı: 147

Kaynak Göster

APA Bulut, M. (2013). A NEW MEDIUM TO HIGH ENTHALPY GEOTHERMAL FIELD IN AEGEAN REGION (AKYAR) MENDERES – SEFERİHİSAR – İZMİR, WESTERN ANATOLIA, TURKEY. Bulletin of the Mineral Research and Exploration, 147(147), 153-167.
AMA Bulut M. A NEW MEDIUM TO HIGH ENTHALPY GEOTHERMAL FIELD IN AEGEAN REGION (AKYAR) MENDERES – SEFERİHİSAR – İZMİR, WESTERN ANATOLIA, TURKEY. Bull.Min.Res.Exp. Aralık 2013;147(147):153-167.
Chicago Bulut, Metin. “A NEW MEDIUM TO HIGH ENTHALPY GEOTHERMAL FIELD IN AEGEAN REGION (AKYAR) MENDERES – SEFERİHİSAR – İZMİR, WESTERN ANATOLIA, TURKEY”. Bulletin of the Mineral Research and Exploration 147, sy. 147 (Aralık 2013): 153-67.
EndNote Bulut M (01 Aralık 2013) A NEW MEDIUM TO HIGH ENTHALPY GEOTHERMAL FIELD IN AEGEAN REGION (AKYAR) MENDERES – SEFERİHİSAR – İZMİR, WESTERN ANATOLIA, TURKEY. Bulletin of the Mineral Research and Exploration 147 147 153–167.
IEEE M. Bulut, “A NEW MEDIUM TO HIGH ENTHALPY GEOTHERMAL FIELD IN AEGEAN REGION (AKYAR) MENDERES – SEFERİHİSAR – İZMİR, WESTERN ANATOLIA, TURKEY”, Bull.Min.Res.Exp., c. 147, sy. 147, ss. 153–167, 2013.
ISNAD Bulut, Metin. “A NEW MEDIUM TO HIGH ENTHALPY GEOTHERMAL FIELD IN AEGEAN REGION (AKYAR) MENDERES – SEFERİHİSAR – İZMİR, WESTERN ANATOLIA, TURKEY”. Bulletin of the Mineral Research and Exploration 147/147 (Aralık 2013), 153-167.
JAMA Bulut M. A NEW MEDIUM TO HIGH ENTHALPY GEOTHERMAL FIELD IN AEGEAN REGION (AKYAR) MENDERES – SEFERİHİSAR – İZMİR, WESTERN ANATOLIA, TURKEY. Bull.Min.Res.Exp. 2013;147:153–167.
MLA Bulut, Metin. “A NEW MEDIUM TO HIGH ENTHALPY GEOTHERMAL FIELD IN AEGEAN REGION (AKYAR) MENDERES – SEFERİHİSAR – İZMİR, WESTERN ANATOLIA, TURKEY”. Bulletin of the Mineral Research and Exploration, c. 147, sy. 147, 2013, ss. 153-67.
Vancouver Bulut M. A NEW MEDIUM TO HIGH ENTHALPY GEOTHERMAL FIELD IN AEGEAN REGION (AKYAR) MENDERES – SEFERİHİSAR – İZMİR, WESTERN ANATOLIA, TURKEY. Bull.Min.Res.Exp. 2013;147(147):153-67.

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