Araştırma Makalesi
BibTex RIS Kaynak Göster

YEŞİLOVA (BURDUR) OFİYOLİTİNİN KUZEYBATISINDA YER ALAN ULTRAMAFİK-MAFİK KAYAÇLARIN VE İZOLE DAYKLARIN PETROLOJİSİ VE JEOKİMYASI

Yıl 2022, , 1 - 18, 13.12.2022
https://doi.org/10.17780/ksujes.1146888

Öz

Toros kuşağında Likya napları içerisinde yer alan Yeşilova (Burdur) Ofiyoliti ultramafik tektonitler, ultramafik-mafik kümülatlar, izotropik gabrolar, plajiyogranitler ve bazaltlardan oluşmaktadır. Bu çalışma, Yeşilova Ofiyolitinin, Salda, Düden ve Doğanbaba (KB Yeşilova, Burdur) mevkilerinde yüzeyleyen, ultramafik-mafik kayaçları (ana kayaçlar) ve bu kayaçları kesen izole dayklar ile ilgilidir. Bu araştırmada, kayaçların petrografik, jeokimyasal ve petrolojik özellikleri belirlenmeye çalışılmıştır. Yapılan petrografik incelemeler sonucunda ana kayaçlar serpantinit ve gabro, izole dayklar ise diyabaz bileşimine sahiptir. Ana kayaçlarda ve izole dayklarda serpantinleşme, uralitleşme, kloritleşme, sossoritleşme, epidotlaşma ve serisitleşme gibi alterasyon türleri gözlenmiştir. Ana kayaçlarda elek/ağ dokusu, izole dayklarda ise ofitik/subofitik ve intersertal dokular gözlemlenmiştir. Ti/Y - Nb/ Y diyagramına göre Yeşilova örnekleri toleyitik ve alkalen özelliktedir. Örümcek diyagramlarda, ana kayaçlar ve izole dayklarda LIL (ör: Rb, Ba, K, Sr, Eu) elementlerinde zenginleşme ve HFS elementlerinde (ör: Ta, Nb) ise tüketilme gözlenmektedir. Kondrit-normalize REE diyagramlarına göre ana kayaçlarda ve izole dayklarda LRE elementlerinde tüketilme ve HRE elementlerinde ise yataya yakın bir dağılıma sahip olup; N-MORB trendine benzerlik göstermektedir. Jeokimyasal değerlendirmeler sonucunda ise inceleme konusu olan kayaçlar için dalma-batma zonundaki (SSZ) yay ile ilişkili bir magmadan türediği söylenebilir.

Destekleyen Kurum

Akdeniz Üniversitesi Bilimsel Araştırmalar Koordinasyon Birimi

Proje Numarası

FYL-2019-4877

Teşekkür

Bu çalışma Akdeniz Üniversitesi Bilimsel Araştırma Projeleri Koordinatörlüğü tarafından FYL-2019-4877 nolu proje ile desteklenmiştir.

Kaynakça

  • Bağcı, U., Parlak, O., & Höck, V. (2010). Tectonic significance of the geochemistry and petrology of the Tekirova (Antalya) ophiolite, Southern Turkey. In Proc. 10th International Multidisciplinary Scientific GeoConference (SGEM), Varna, Bulgaria (pp. 157-164).
  • Bağcı, U., & Parlak, O. (2009). Petrology of the Tekirova (Antalya) ophiolite (Southern Turkey): evidence for diverse magma generations and their tectonic implications during Neotethyan-subduction. International Journal of Earth Sciences, 98, 387-405. https://doi.org/10.1007/s00531-007-0242-7
  • Beyarslan, M., & Bingöl, A.F. (2000). Petrology of a supra-subduction zone ophiolite (Elazığ, Turkey). Canadian Journal Earth Sciences, 37, 1411-1424. https://doi.org/10.31202/ecjse.993333
  • Boynton, W.V. (1984). Geochemistry of the Rare Earth Elements: Meteorite Studies. In Henderson, P. (Ed.), Rare Earth Element Geochemistry. Elsevier, Amsterdam (pp. 63-114)
  • Çelik, Ö.F. (2008). Detailed geochemistry and K-Ar geochronology of the metamorphic sole rocks and their mafic dykes from the Mersin Ophiolite, Southern Turkey. Turkish Journal of Earth Sciences, 17, 685-708.
  • Çelik, Ö.F., & Chiaradia, M. (2008). Geochemical and petrological aspects of dyke intrusions in the Lycian Ophiolites (SW Turkey): a case study for the dyke emplacement along the Tauride Belt Ophiolites. International Journal of Earth Sciences, 97, 1151-1164. https://doi.org/10.1007/s00531-007-0204-0
  • Çelik, Ö.F. (2007). Metamorphic sole rocks and their mafic dykes in the Eastern Tauride Belt ophiolites (Southern Turkey): implications for OIB type magma generation following slab break-off. Geological Magazine, 144, 849-866. https://doi.org/10.1007/s00531-007-0204-0
  • Çelik, Ö.F., & Delaloye, M. (2003). Origin of metamorphic soles and their post-kinematic mafic dyke swarms in the Antalya and Lycian ophiolites, SW Turkey. Geological Journal, 38, 235-256. https://doi.org/10.1002/gj.954
  • Çetrez, B. (2022). Yeşilova (Burdur) ofiyolitinde yer alan izole daykların jeokimyası ve petrojenezi. Yüksek Lisans Tezi. Akdeniz Üniversitesi Fen Bilimleri Enstitüsü Jeoloji Mühendisliği Anabilim Dalı, Antalya 98s.
  • Dilek, Y., & Flower, M.F.J. (2003). Arc-trench rollback and forearc accretion: 2. A model template for ophiolites in Albania, Cyprus, and Oman. In Dilek, Y. & Robinson, P.T., (Eds.), Ophiolites in Earth History. Geological Society London Special Publication 218, 43-68. https://doi.org/10.1144/GSL.SP.2003.218.01.04
  • Dilek, Y., Thy, P., & Hacker, B.R. (1999). Structure and petrology of Tauride Ophiolites and mafic dyke intrusions (Turkey): implications for the Neotethyan Ocean. Geological Society of America Bulletin, 111, 1192-1216. https://doi.org/10.1130/0016-7606(1999)111<1192:SAPOTO>2.3.CO;2
  • Ersoy, S. (1990). Batı Toros (Likya) Naplarının Yapısal Ögelerinin ve Evriminin Analizi. Jeoloji Mühendisliği, 37, 5-16.
  • Güneş, A., İlbeyli, N., Rasimgil, S., & Demirbilek, M. (2021). Petrological and geochemical characteristics of the diabase and metasomatised dikes from the Tekirova ophiolite (SW Anatolia, Turkey): Tectonomagmatic evolution of the southern Neotethys. Geochemistry, 81, 125767. https://doi.org/10.1016/j.chemer.2021.125767
  • Jenner, G.A., Dunning, G.R., Malpas, J., Brown, M., & Brace, T. (1991). Bay of Islands and Little Port complexes, revisited: age, geochemical and isotopic evidence confirm suprasubduction-zone origin. Canadian Journal of Earth Sciences, 28(10), 35-52. https://doi.org/10.1139/e91-146
  • Juteau, T. (1980). Ophiolites of Turkey. Ofioliti 2, 199-235.
  • Irvine, T.N., & Baragar, W.R.A. (1971). A guide to the chemical classification of the common volcanic rocks. Canadian Journal of Earth Sciences, 8, 523-548. http://doi.org/10.1139/e71-055
  • Karaman, T. (1987). Yeşilova-Tefenni (Burdur) Batısında Kalan Alanın Jeolojisi ve Petrografisi, Yüksek Lisans Tezi, Selçuk Üniversitesi, Fen Bilimleri Enstitüsü, Konya.
  • Kavak, K.S., Parlak, O., & Temiz, H. (2017). Geochemical characteristics of ophiolitic rocks from the southern margin of the Sivas basin and their implications for the Inner Tauride Ocean, Central-Eastern Turkey. Geodinamica Acta, 29(1), 160-180. https://doi.org/10.1080/09853111.2017.1359773
  • Middlemost, E.A.K. (1994). Naming materials in the magma/igneous rock system. Earth-Science Reviews, 37, 215-224. https://doi.org/10.1016/0012-8252(94)90029-9
  • Moores, E.M., Kellogg, H., Yıldırım, D. (2000). Tethyan ophiolites, mantle convection, and tectonic “historical contingency”: A resolution of the “ophiolite conundrum”. Geological Society of America, 349, 3-12. https://doi.org/10.1130/0-8137-2349-3.3
  • Parlak, O. (2016). The Tauride ophiolites of Anatolia (Turkey): a review. Journal of Earth Science, 27 (6), 901-934. https://doi.org/10.1007/s12583-016-0679-3
  • Parlak, O., Yılmaz, H., & Boztuğ, D. (2006). Origin and tectonic significance of the metamorphic sole and isolated dykes of the Divriği Ophiolite (Sivas, Turkey): evidence for slab break-off prior to ophiolite emplacement. Turkish Journal of Earth Sciences, 15, 25-45.
  • Parlak, O., Höck, V., Kozlu, H., & Delaloye, M. (2004). Oceanic crust generation in an island arc tectonic setting, SE Anatolian Orogenic Belt (Turkey). Geological Magazine, 141, 583-603. https://doi.org/10.1017/S0016756804009458
  • Parlak, O., Höck, V., & Delaloye, M. (2002). The supra-subduction Pozantı-Karsantı ophiolite, southern Turkey: evidence for high pressure crystal fractionation of ultramafic cumulates. Lithos, 65, 205-224. https://doi.org/10.1016/S0024-4937(02)00166-4
  • Parlak, O. (2000). Geochemistry and significance of mafic dyke swarms in the Pozantı- Karsantı ophiolite (Southern Turkey). Turkish Journal of Earth Sciences, 9, 29-38.
  • Parlak, O., & Delaloye, M. (1996). Geochemistry and timing of post-metamorphic dike emplacement in the Mersin ophiolite (southern Turkey): new age constraints from 40Ar/39Ar geochronology. Terra Nova, 8, 585-592. https://doi.org/10.1111/j.1365-3121.1996.tb00788.x
  • Parlak, O., Delaloye, M., & Bingöl, E. (1995). Origin of sub-ophiolitic metamorphic rocks beneath the Mersin ophiolite, southern Turkey. Ofioliti, 20, 97-110.
  • Pearce, J.A. (2014). Immobile element fingerprinting of ophiolites. Elements, 10 (2), 101-108. https://doi.org/10.2113/gselements.10.2.101
  • Pearce, J.A., Lippard, S.J., & Roberts, S. (1984). Characteristics and Tectonic Significance of Supra-subduction Zone Ophiolites. In Kokelaar, B.P., & Howells, M.F. (Eds.), Marginal Basin Geology. Geological Society of London Special Publication, 16, 77-89. https://doi.org/10.1144/GSL.SP.1984.016.01.06
  • Pearce, J.A. (1982). Trace Element Characteristics of Lavas from Destructive Plate Boundaries. In Thorpe, J.S. (Ed.), Andesites (pp.525-548). New York: John Wiley.
  • Robertson, A.H.F., Parlak, O., & Metin, Y. (2013). Late Palaeozoic-Cenozoic tectonic development of carbonate platform, margin and oceanic units in the Eastern Taurides, Turkey. In Robertson, A.H.F., Parlak, O., & Ünlügenç, U.C. (Eds.), Geological Development of Anatolia and the Easternmost Mediterranean Region. Geological Society London Special Publication, 372, (pp. 167-218)
  • Robertson, A.H.F. (2004). Development of concepts concerning the genesis and emplacement of Tethyan ophiolites in the eastern Mediterranean and Oman regions. Earth-Science Reviews, 66, 331-387. https://doi.org/ 10.1016/j.earscirev.2004.01.005
  • Robertson, A.H.F. (2002). Overview of the genesis and emplacement of Mesozoic ophiolites in the Eastern Mediterranean Tethyan region. Lithos, 65, 1-67. https://doi.org/10.1016/S0024-4937(02)00160-3
  • Shervais, J.W., (2022). The petrogenesis of modern and ophiolitic lavas reconsidered: Ti-V and Nb-Th. Geoscience Frontiers, 13(2), 101319. https://doi.org/10.1016/j.gsf.2021.101319
  • Shervais, J.W., Reagan, M.K., Godard, M., Prytulak, J., Ryan, J.G., Pearce, J.A., Almeev, R.A., Li, H., Haugen, E., Chapman, T., Kurz, W., Nelson, W.R., Heaton, D., Kirchenbaur, M., Shimizu, K., Sakuyama, T., Vetter, S.K., Li, Y., & Whattam, S. (2021). Magmatic Response to Subduction Initiation, Part II: Boninites and related rocks of the Izu-Bonin Arc from IODP Expedition 352. Geochemistry, Geophysics, Geosystems, 22, e2020GC009093. https://doi.org/10.1029/2020GC009093
  • Sun, S., & McDonough, W.F. (1989). Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. In Saunders, A.D., & Norry, M.J. (Eds.), Magmatism in the Ocean Basins. Geological Society London Special Publication, 42, (pp. 313-345).
  • Şengör, A.M.C., & Yılmaz, Y. (1981). Tethyan evolution of Turkey: a plate tectonic approach. Tectonophysics, 75, 181-241.
  • Whitechurch, H., Juteau, T., & Montigny, R. (1984). Role of the Eastern Mediterranean ophiolites (Turkey, Syria, Cyprus) in the history of the Neo-Tethys. In Dixon, J.E., & Robertson, A.H.F. (Eds.), The Geological Evolution of the Eastern Mediterranean. Geological Society London Special Publication, 17, (pp. 301-319)

PETROLOGY AND GEOCHEMISTRY OF ULTRAMAFIC-MAFIC ROCKS AND ISOLATED DIKES IN THE NORTHWEST OF YEŞİLOVA (BURDUR) OPHIOLITE

Yıl 2022, , 1 - 18, 13.12.2022
https://doi.org/10.17780/ksujes.1146888

Öz

Proje Numarası

FYL-2019-4877

Kaynakça

  • Bağcı, U., Parlak, O., & Höck, V. (2010). Tectonic significance of the geochemistry and petrology of the Tekirova (Antalya) ophiolite, Southern Turkey. In Proc. 10th International Multidisciplinary Scientific GeoConference (SGEM), Varna, Bulgaria (pp. 157-164).
  • Bağcı, U., & Parlak, O. (2009). Petrology of the Tekirova (Antalya) ophiolite (Southern Turkey): evidence for diverse magma generations and their tectonic implications during Neotethyan-subduction. International Journal of Earth Sciences, 98, 387-405. https://doi.org/10.1007/s00531-007-0242-7
  • Beyarslan, M., & Bingöl, A.F. (2000). Petrology of a supra-subduction zone ophiolite (Elazığ, Turkey). Canadian Journal Earth Sciences, 37, 1411-1424. https://doi.org/10.31202/ecjse.993333
  • Boynton, W.V. (1984). Geochemistry of the Rare Earth Elements: Meteorite Studies. In Henderson, P. (Ed.), Rare Earth Element Geochemistry. Elsevier, Amsterdam (pp. 63-114)
  • Çelik, Ö.F. (2008). Detailed geochemistry and K-Ar geochronology of the metamorphic sole rocks and their mafic dykes from the Mersin Ophiolite, Southern Turkey. Turkish Journal of Earth Sciences, 17, 685-708.
  • Çelik, Ö.F., & Chiaradia, M. (2008). Geochemical and petrological aspects of dyke intrusions in the Lycian Ophiolites (SW Turkey): a case study for the dyke emplacement along the Tauride Belt Ophiolites. International Journal of Earth Sciences, 97, 1151-1164. https://doi.org/10.1007/s00531-007-0204-0
  • Çelik, Ö.F. (2007). Metamorphic sole rocks and their mafic dykes in the Eastern Tauride Belt ophiolites (Southern Turkey): implications for OIB type magma generation following slab break-off. Geological Magazine, 144, 849-866. https://doi.org/10.1007/s00531-007-0204-0
  • Çelik, Ö.F., & Delaloye, M. (2003). Origin of metamorphic soles and their post-kinematic mafic dyke swarms in the Antalya and Lycian ophiolites, SW Turkey. Geological Journal, 38, 235-256. https://doi.org/10.1002/gj.954
  • Çetrez, B. (2022). Yeşilova (Burdur) ofiyolitinde yer alan izole daykların jeokimyası ve petrojenezi. Yüksek Lisans Tezi. Akdeniz Üniversitesi Fen Bilimleri Enstitüsü Jeoloji Mühendisliği Anabilim Dalı, Antalya 98s.
  • Dilek, Y., & Flower, M.F.J. (2003). Arc-trench rollback and forearc accretion: 2. A model template for ophiolites in Albania, Cyprus, and Oman. In Dilek, Y. & Robinson, P.T., (Eds.), Ophiolites in Earth History. Geological Society London Special Publication 218, 43-68. https://doi.org/10.1144/GSL.SP.2003.218.01.04
  • Dilek, Y., Thy, P., & Hacker, B.R. (1999). Structure and petrology of Tauride Ophiolites and mafic dyke intrusions (Turkey): implications for the Neotethyan Ocean. Geological Society of America Bulletin, 111, 1192-1216. https://doi.org/10.1130/0016-7606(1999)111<1192:SAPOTO>2.3.CO;2
  • Ersoy, S. (1990). Batı Toros (Likya) Naplarının Yapısal Ögelerinin ve Evriminin Analizi. Jeoloji Mühendisliği, 37, 5-16.
  • Güneş, A., İlbeyli, N., Rasimgil, S., & Demirbilek, M. (2021). Petrological and geochemical characteristics of the diabase and metasomatised dikes from the Tekirova ophiolite (SW Anatolia, Turkey): Tectonomagmatic evolution of the southern Neotethys. Geochemistry, 81, 125767. https://doi.org/10.1016/j.chemer.2021.125767
  • Jenner, G.A., Dunning, G.R., Malpas, J., Brown, M., & Brace, T. (1991). Bay of Islands and Little Port complexes, revisited: age, geochemical and isotopic evidence confirm suprasubduction-zone origin. Canadian Journal of Earth Sciences, 28(10), 35-52. https://doi.org/10.1139/e91-146
  • Juteau, T. (1980). Ophiolites of Turkey. Ofioliti 2, 199-235.
  • Irvine, T.N., & Baragar, W.R.A. (1971). A guide to the chemical classification of the common volcanic rocks. Canadian Journal of Earth Sciences, 8, 523-548. http://doi.org/10.1139/e71-055
  • Karaman, T. (1987). Yeşilova-Tefenni (Burdur) Batısında Kalan Alanın Jeolojisi ve Petrografisi, Yüksek Lisans Tezi, Selçuk Üniversitesi, Fen Bilimleri Enstitüsü, Konya.
  • Kavak, K.S., Parlak, O., & Temiz, H. (2017). Geochemical characteristics of ophiolitic rocks from the southern margin of the Sivas basin and their implications for the Inner Tauride Ocean, Central-Eastern Turkey. Geodinamica Acta, 29(1), 160-180. https://doi.org/10.1080/09853111.2017.1359773
  • Middlemost, E.A.K. (1994). Naming materials in the magma/igneous rock system. Earth-Science Reviews, 37, 215-224. https://doi.org/10.1016/0012-8252(94)90029-9
  • Moores, E.M., Kellogg, H., Yıldırım, D. (2000). Tethyan ophiolites, mantle convection, and tectonic “historical contingency”: A resolution of the “ophiolite conundrum”. Geological Society of America, 349, 3-12. https://doi.org/10.1130/0-8137-2349-3.3
  • Parlak, O. (2016). The Tauride ophiolites of Anatolia (Turkey): a review. Journal of Earth Science, 27 (6), 901-934. https://doi.org/10.1007/s12583-016-0679-3
  • Parlak, O., Yılmaz, H., & Boztuğ, D. (2006). Origin and tectonic significance of the metamorphic sole and isolated dykes of the Divriği Ophiolite (Sivas, Turkey): evidence for slab break-off prior to ophiolite emplacement. Turkish Journal of Earth Sciences, 15, 25-45.
  • Parlak, O., Höck, V., Kozlu, H., & Delaloye, M. (2004). Oceanic crust generation in an island arc tectonic setting, SE Anatolian Orogenic Belt (Turkey). Geological Magazine, 141, 583-603. https://doi.org/10.1017/S0016756804009458
  • Parlak, O., Höck, V., & Delaloye, M. (2002). The supra-subduction Pozantı-Karsantı ophiolite, southern Turkey: evidence for high pressure crystal fractionation of ultramafic cumulates. Lithos, 65, 205-224. https://doi.org/10.1016/S0024-4937(02)00166-4
  • Parlak, O. (2000). Geochemistry and significance of mafic dyke swarms in the Pozantı- Karsantı ophiolite (Southern Turkey). Turkish Journal of Earth Sciences, 9, 29-38.
  • Parlak, O., & Delaloye, M. (1996). Geochemistry and timing of post-metamorphic dike emplacement in the Mersin ophiolite (southern Turkey): new age constraints from 40Ar/39Ar geochronology. Terra Nova, 8, 585-592. https://doi.org/10.1111/j.1365-3121.1996.tb00788.x
  • Parlak, O., Delaloye, M., & Bingöl, E. (1995). Origin of sub-ophiolitic metamorphic rocks beneath the Mersin ophiolite, southern Turkey. Ofioliti, 20, 97-110.
  • Pearce, J.A. (2014). Immobile element fingerprinting of ophiolites. Elements, 10 (2), 101-108. https://doi.org/10.2113/gselements.10.2.101
  • Pearce, J.A., Lippard, S.J., & Roberts, S. (1984). Characteristics and Tectonic Significance of Supra-subduction Zone Ophiolites. In Kokelaar, B.P., & Howells, M.F. (Eds.), Marginal Basin Geology. Geological Society of London Special Publication, 16, 77-89. https://doi.org/10.1144/GSL.SP.1984.016.01.06
  • Pearce, J.A. (1982). Trace Element Characteristics of Lavas from Destructive Plate Boundaries. In Thorpe, J.S. (Ed.), Andesites (pp.525-548). New York: John Wiley.
  • Robertson, A.H.F., Parlak, O., & Metin, Y. (2013). Late Palaeozoic-Cenozoic tectonic development of carbonate platform, margin and oceanic units in the Eastern Taurides, Turkey. In Robertson, A.H.F., Parlak, O., & Ünlügenç, U.C. (Eds.), Geological Development of Anatolia and the Easternmost Mediterranean Region. Geological Society London Special Publication, 372, (pp. 167-218)
  • Robertson, A.H.F. (2004). Development of concepts concerning the genesis and emplacement of Tethyan ophiolites in the eastern Mediterranean and Oman regions. Earth-Science Reviews, 66, 331-387. https://doi.org/ 10.1016/j.earscirev.2004.01.005
  • Robertson, A.H.F. (2002). Overview of the genesis and emplacement of Mesozoic ophiolites in the Eastern Mediterranean Tethyan region. Lithos, 65, 1-67. https://doi.org/10.1016/S0024-4937(02)00160-3
  • Shervais, J.W., (2022). The petrogenesis of modern and ophiolitic lavas reconsidered: Ti-V and Nb-Th. Geoscience Frontiers, 13(2), 101319. https://doi.org/10.1016/j.gsf.2021.101319
  • Shervais, J.W., Reagan, M.K., Godard, M., Prytulak, J., Ryan, J.G., Pearce, J.A., Almeev, R.A., Li, H., Haugen, E., Chapman, T., Kurz, W., Nelson, W.R., Heaton, D., Kirchenbaur, M., Shimizu, K., Sakuyama, T., Vetter, S.K., Li, Y., & Whattam, S. (2021). Magmatic Response to Subduction Initiation, Part II: Boninites and related rocks of the Izu-Bonin Arc from IODP Expedition 352. Geochemistry, Geophysics, Geosystems, 22, e2020GC009093. https://doi.org/10.1029/2020GC009093
  • Sun, S., & McDonough, W.F. (1989). Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. In Saunders, A.D., & Norry, M.J. (Eds.), Magmatism in the Ocean Basins. Geological Society London Special Publication, 42, (pp. 313-345).
  • Şengör, A.M.C., & Yılmaz, Y. (1981). Tethyan evolution of Turkey: a plate tectonic approach. Tectonophysics, 75, 181-241.
  • Whitechurch, H., Juteau, T., & Montigny, R. (1984). Role of the Eastern Mediterranean ophiolites (Turkey, Syria, Cyprus) in the history of the Neo-Tethys. In Dixon, J.E., & Robertson, A.H.F. (Eds.), The Geological Evolution of the Eastern Mediterranean. Geological Society London Special Publication, 17, (pp. 301-319)
Toplam 38 adet kaynakça vardır.

Ayrıntılar

Birincil Dil Türkçe
Konular Yer Bilimleri ve Jeoloji Mühendisliği (Diğer)
Bölüm Jeoloji Mühendisliği
Yazarlar

Burçin Çetrez 0000-0001-6494-6709

Nurdane İlbeyli 0000-0002-0557-8771

Alper Güneş 0000-0002-6711-266X

Mehmet Demirbilek 0000-0003-2749-5560

Yusuf Uras 0000-0001-5561-3275

Proje Numarası FYL-2019-4877
Yayımlanma Tarihi 13 Aralık 2022
Gönderilme Tarihi 22 Temmuz 2022
Yayımlandığı Sayı Yıl 2022

Kaynak Göster

APA Çetrez, B., İlbeyli, N., Güneş, A., Demirbilek, M., vd. (2022). YEŞİLOVA (BURDUR) OFİYOLİTİNİN KUZEYBATISINDA YER ALAN ULTRAMAFİK-MAFİK KAYAÇLARIN VE İZOLE DAYKLARIN PETROLOJİSİ VE JEOKİMYASI. Kahramanmaraş Sütçü İmam Üniversitesi Mühendislik Bilimleri Dergisi, 25(Özel Sayı), 1-18. https://doi.org/10.17780/ksujes.1146888