Research Article
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Year 2021, , 537 - 550, 30.12.2021
https://doi.org/10.54287/gujsa.1032149

Abstract

References

  • Anıl, M. (l990). Pozantı-Karsantı, Mersin ve Kızıldağ (Hatay) Ofiyolitlerindeki Bazı Kromit Yataklarının Morfolojik Yapısal ve Jenetik Özellikleri ile Akdeniz Bölgesindeki Benzer Kromit Yataklarının Karşılaştırılması. Doğa, l4, 645-675, Ankara.
  • Blumenthal, M. (1946), Kilikya Toros’larının Çok Dikkate Değer Bir Parçası: Karanfildağ. MTA Mecmuası, 2. 257-286.
  • Boudier, F., & Nicolas, A. (1985) Harzburgite and lherzolite subtypes in ophiolitic and oceanic environments. Earth and Planet. Science Letters, 76(1-2), 84-92. doi:10.1016/0012-821X(85)90150-5
  • Brown, M. (1980). Textural and geochemical evidence for the origin of some chromite deposits in the Oman ophiolite. In: A. Panayiotou (Eds.) Ophiolites, Proceed. Intern. Ophiolite Symp. Cyprus, 714-721. Geol. Surv. Dep., Nicosia.
  • Cassard, D., Nicolas, A., Rabinovitch, M., Moutte, J., Leblanc, M., & Prinzhofer, A., (1981). Structural classification of chromite pods in southern New Caledonia. Economic Geology, 76(4), 805- 831. doi:10.2113/gsecongeo.76.4.805
  • Choi, S. H., Shervais, J. W., & Mukasa, S. B. (2008). Supra-subduction and abyssal mantle peridotites of the Coast range ophiolite, California. Contributions to Mineralogy and Petrology, 156, 551–576. doi:10.1007/s00410-008-0300-6
  • Colás, V., González-Jiménez, J. M., Griffin, W. L., Fanlo, I., Gervilla, F., O’Reilly, S. Y., Pearson, N. J., Kerestedjian, T., & Proenza, J. A. (2014). Fingerprints of Metamorphism in Chromite: New Insights from Minor and Trace Elements. Chemical Geology, 389, 137–152. doi:10.1016/j.chemgeo.2014.10.001
  • Çakır, Ü. (1978). Petrologie Du Masisf De Pozantı-Karsantı (Taurus Cilicien, Turquie): Etude La Partie Centralla. These De Doctorat d’Ing. Univ. Satrasbourg. p. 251. (unpublished).
  • Dare, S. A. S., Pearce, J. A., McDonald, I., & Styles, M. T. (2009). Tectonic Discriminationof Peridotites Using fO2-Cr# and Ga-Ti-FeIII Systematics in Chrome-Spinel. Chemical Geology, 261(3-4), 199–216. doi:10.1016/j.chemgeo.2008.08.002
  • Dickey, J. S. (1976). A Hypothesis of Origin For Podiform Chromite Deposits. Chromium: its Physicochemical Behavior and Petrologic Significance, 1061-1074. doi:10.1016/B978-0-08-019954-2.50026-3
  • Dilek, Y., & Robinson, P. T. (Eds.) (2003). Ophiolites in Earth History. Geological Society, London, Special Publications, 218. doi:10.1029/2004EO440009
  • Dilek, Y., & Morishita, T. (2009). Melt migration and upper mantle evolution during incipient arc construction: Jurassic Eastern Mirdita ophiolite, Albania. Island Arc, 18(4), 551–554. doi:10.1111/j.1440-1738.2009.00692.x
  • Duke, J. M., (1983). Ore Deposit Models 7. Magmatic Segregation Deposits of Chromite. Geoscience Canada, 10(1), 15–24.
  • Gervilla, F., Padro'n-Navarta, J. A., Kerestedjian, T., Sergeeva, I., González-Jiménez, J. M., & Fanlo, I. (2012). Formation of ferrian chromite in podiform chromitites from the Golyamo Kamenyane serpentinite, Eastern Rhodopes, SE Bulgaria: a two stage process. Contributions to Mineralogy and Petrology, 164, 643-657. doi:10.1007/s00410-012-0763-3
  • Greenbaum. D. (1977). The chromitiferous rocks of the Troodos ophiolite complex, Cyprus. Economic Geology, 72(7): 1175-1194. doi:10.2113/gsecongeo.72.7.1175
  • Huang, Y., & Deng, H. (2020) Geochemical Characteristics of Zoned Chromites in Peridotites from the Proterozoic Miaowan Ophiolitic Complex, Yangtze Craton: Implications for Element Mobility and Tectonic Setting. Journal of Earth Science, 31(2), 223–236. doi:10.1007/s12583-019-1278-x
  • Leblanc, M. (1980). Chromite growth, dissolution and deformation from a morphological view point: SEM investigations. Mineralium Deposita, 15(2), 201-210. doi:10.1007/BF00206514
  • Lian, D., Yang, J., Dilek, Y., Wu, W., Zhang, Z., Xiong, F., Liu, F., & Zhou. W. (2017). Deep mantle origin and ultra-reducing conditions in podiform chromitite: Diamond, moissanite, and other unusual minerals in podiform chromitites from the Pozanti-Karsanti ophiolite, southern Turkey. American Mineralogist, 102(5), 1101–1113. doi:10.2138/am-2017-5850
  • Niu, Y., Langmuir, C. H., & Kinzler, R. J. (1997). The origin of abyssal peridotites: a new perspective. Earth and Planetary Science Letters 152, 251–265. doi:10.1016/S0012-821X(97)00119-2
  • Parlak, O., Höck, V., & Delaloye. M. (2002). The Supra-Subduction Zone Pozantı-Karsantı-Ophiolite Southern Turkey: Evidence For High-Pressure Crystal Fractionation of Ultramafic Cumulates. Lithos, 65(1-2), 205-224. doi:10.1016/s0024-4937(02)00166-4
  • Pearce, J. A., Lippard, S. J., & Roberts, S. (1984). Characteristics and tectonic significance of supra-subduction zone ophiolites. Geological Society, London, Special Publications, 16, 77–94. doi:10.1144/GSL.SP.1984.016.01.06
  • Polat, A., & Casey, J. F. (1995). A Stuructural Record of The Emplacement of the Pozantı-Karsantı Ophiolite onto the Menderes-Taurus Block in The Late Cretaceus, Eastren Taurides, Turkey. Journal of Structural Geology, 17(12), 1673-1688. doi:10.1016/0191-8141(95)00061-h
  • Prichard, H. M., Barnes, S. J., Godel, B., Reddy, S. M., Vukmanovic, Z., Halfpenny, A., Neary, C. R., & Fisher, P. C. (2015). The structure of and origin of nodular chromite from the Troodos ophiolite, Cyprus, revealed using high-resolution X-ray computed tomography and electron backscatter diffraction. Lithos, 218-219, 87-98. doi:10.1016/j.lithos.2015.01.013
  • Roberts, S. (1988). Ophiolitic chromitite formation: a marginal basin phenomenon. Economic Geology, 83(5), 1034-1036. doi:10.2113/gsecongeo.83.5.1034
  • Takazawa, E., Frey, F. A., Shimizu, N., & Obata, M. (2000). Whole rock compositional variations in an upper mantle peridotite (Horoman, Hokkaido, Japan): are they consistent with a partial melting process? Geochemica et Cosmochimica Acta, 64(4), 695–716. doi:10.1016/S0016-7037(99)00346-4
  • Tekeli, O. (1981). Toros’larda Aladağ Ofiyolitli Melanjının Özellikleri. Türkiye Jeoloji Bülteni, 24, 57-64.
  • Tekeli, O., Aksay, A., Ürgün, B. M. & Işık, A. (1984). Geology of the Aladağ Mountains. Geology Of The Taurus Belt: Procedings Int. Sym., 26-29. September., 143-149. Ankara. Turkey.
  • Thayer, T. P. (1964). Principal Features and origin of podiform chromite deposits and some observations on the Guleman-Soridag District, Turkey. Economic Geology, 59(8), 1497-1524. doi:10.2113/gsecongeo.59.8.1497
  • Thayer, T. P. (1969). Peridodite-gabbro complexes as keys to petrology of mid-ocean ridges. Geological Society of American Bulletin, 80(8), 1511-1522. doi:10.1130/0016-7606(1969)80[1515:PCAKTP]2.0.CO;2
  • Uysal, I., Ersoy, E. Y., Karsli, O., Dilek, Y., Sadiklar, M. B., Ottley, C. J., Tiepolo, M., & Meisel, T. (2012). Coexistence of abyssal and ultra-depleted SSZ type mantle peridotites in a Neo-Tethyan Ophiolite in SW Turkey: Constraints from mineral composition, whole-rock geochemistry (major–trace–REE–PGE), and Re–Os isotope systematics. Lithos, 132–133, 50–69. doi:10.1016/j.lithos.2011.11.009
  • Yetiş, C. (1978). Geology of the Çamardı (Niğde) Region and the Characterics of the Ecemiş Fault Zone Between Maden Bogazı and Kamışlı. İstanbul Ünv. Fen Fak. Mecm. Seri E. 43, 41-61. (unpublished).
  • Yu, H., Zhang, H-F., Zou, H-B. & Yang, Y-H. (2019). Minor and trace element variations in chromite from the Songshugou dunites, North Qinling Orogen: Evidence for amphibolite-facies metamorphism. Lithos, 328-329, 146-158. doi:10.1016/j.lithos.2019.01.009

Chromitite Ore Types and Geochemical Investigation of Pozantı-Karsantı Ophiolite in Mazmılı Region (Turkey)

Year 2021, , 537 - 550, 30.12.2021
https://doi.org/10.54287/gujsa.1032149

Abstract

The Pozantı-Karsantı Ophiolite located in the middle Taurus has significant chromitite reserves in Turkey. The chromitite ore bodies belong to concordant and subconcordant form and are located within mantle harzburgite surrounded by bodies of dunite. Chromitite ore types are small or medium bodies of massive, disseminated, banded and nodular, also the result of a combination of at least two of these types of ores consist of mixed-type ore. Chromite ores bear traces of plastic deformation under the influence of lateral forces developing in the lateral direction. Plastic deformation is also observed at the micro scale. This study presents the concentrations of a complete suite of major (SiO2, Cr2O3, MgO, Al2O3, and FeO(t)) and trace elements (Ni, Ti, Co, V, Zn, S, Ca, Ga and Cl) in podiform chromitites of the Pozantı-Karsantı Ophiolite. According to the chromite ore whole-rock geochemical analysis, there was a positive relationship between the amount of Cr2O3 and Zn, V, Ti, and Co, while a negative relationship was found between Ni, S and Ca. This situation is opposite with the dunites in which the chromite ore is located.

References

  • Anıl, M. (l990). Pozantı-Karsantı, Mersin ve Kızıldağ (Hatay) Ofiyolitlerindeki Bazı Kromit Yataklarının Morfolojik Yapısal ve Jenetik Özellikleri ile Akdeniz Bölgesindeki Benzer Kromit Yataklarının Karşılaştırılması. Doğa, l4, 645-675, Ankara.
  • Blumenthal, M. (1946), Kilikya Toros’larının Çok Dikkate Değer Bir Parçası: Karanfildağ. MTA Mecmuası, 2. 257-286.
  • Boudier, F., & Nicolas, A. (1985) Harzburgite and lherzolite subtypes in ophiolitic and oceanic environments. Earth and Planet. Science Letters, 76(1-2), 84-92. doi:10.1016/0012-821X(85)90150-5
  • Brown, M. (1980). Textural and geochemical evidence for the origin of some chromite deposits in the Oman ophiolite. In: A. Panayiotou (Eds.) Ophiolites, Proceed. Intern. Ophiolite Symp. Cyprus, 714-721. Geol. Surv. Dep., Nicosia.
  • Cassard, D., Nicolas, A., Rabinovitch, M., Moutte, J., Leblanc, M., & Prinzhofer, A., (1981). Structural classification of chromite pods in southern New Caledonia. Economic Geology, 76(4), 805- 831. doi:10.2113/gsecongeo.76.4.805
  • Choi, S. H., Shervais, J. W., & Mukasa, S. B. (2008). Supra-subduction and abyssal mantle peridotites of the Coast range ophiolite, California. Contributions to Mineralogy and Petrology, 156, 551–576. doi:10.1007/s00410-008-0300-6
  • Colás, V., González-Jiménez, J. M., Griffin, W. L., Fanlo, I., Gervilla, F., O’Reilly, S. Y., Pearson, N. J., Kerestedjian, T., & Proenza, J. A. (2014). Fingerprints of Metamorphism in Chromite: New Insights from Minor and Trace Elements. Chemical Geology, 389, 137–152. doi:10.1016/j.chemgeo.2014.10.001
  • Çakır, Ü. (1978). Petrologie Du Masisf De Pozantı-Karsantı (Taurus Cilicien, Turquie): Etude La Partie Centralla. These De Doctorat d’Ing. Univ. Satrasbourg. p. 251. (unpublished).
  • Dare, S. A. S., Pearce, J. A., McDonald, I., & Styles, M. T. (2009). Tectonic Discriminationof Peridotites Using fO2-Cr# and Ga-Ti-FeIII Systematics in Chrome-Spinel. Chemical Geology, 261(3-4), 199–216. doi:10.1016/j.chemgeo.2008.08.002
  • Dickey, J. S. (1976). A Hypothesis of Origin For Podiform Chromite Deposits. Chromium: its Physicochemical Behavior and Petrologic Significance, 1061-1074. doi:10.1016/B978-0-08-019954-2.50026-3
  • Dilek, Y., & Robinson, P. T. (Eds.) (2003). Ophiolites in Earth History. Geological Society, London, Special Publications, 218. doi:10.1029/2004EO440009
  • Dilek, Y., & Morishita, T. (2009). Melt migration and upper mantle evolution during incipient arc construction: Jurassic Eastern Mirdita ophiolite, Albania. Island Arc, 18(4), 551–554. doi:10.1111/j.1440-1738.2009.00692.x
  • Duke, J. M., (1983). Ore Deposit Models 7. Magmatic Segregation Deposits of Chromite. Geoscience Canada, 10(1), 15–24.
  • Gervilla, F., Padro'n-Navarta, J. A., Kerestedjian, T., Sergeeva, I., González-Jiménez, J. M., & Fanlo, I. (2012). Formation of ferrian chromite in podiform chromitites from the Golyamo Kamenyane serpentinite, Eastern Rhodopes, SE Bulgaria: a two stage process. Contributions to Mineralogy and Petrology, 164, 643-657. doi:10.1007/s00410-012-0763-3
  • Greenbaum. D. (1977). The chromitiferous rocks of the Troodos ophiolite complex, Cyprus. Economic Geology, 72(7): 1175-1194. doi:10.2113/gsecongeo.72.7.1175
  • Huang, Y., & Deng, H. (2020) Geochemical Characteristics of Zoned Chromites in Peridotites from the Proterozoic Miaowan Ophiolitic Complex, Yangtze Craton: Implications for Element Mobility and Tectonic Setting. Journal of Earth Science, 31(2), 223–236. doi:10.1007/s12583-019-1278-x
  • Leblanc, M. (1980). Chromite growth, dissolution and deformation from a morphological view point: SEM investigations. Mineralium Deposita, 15(2), 201-210. doi:10.1007/BF00206514
  • Lian, D., Yang, J., Dilek, Y., Wu, W., Zhang, Z., Xiong, F., Liu, F., & Zhou. W. (2017). Deep mantle origin and ultra-reducing conditions in podiform chromitite: Diamond, moissanite, and other unusual minerals in podiform chromitites from the Pozanti-Karsanti ophiolite, southern Turkey. American Mineralogist, 102(5), 1101–1113. doi:10.2138/am-2017-5850
  • Niu, Y., Langmuir, C. H., & Kinzler, R. J. (1997). The origin of abyssal peridotites: a new perspective. Earth and Planetary Science Letters 152, 251–265. doi:10.1016/S0012-821X(97)00119-2
  • Parlak, O., Höck, V., & Delaloye. M. (2002). The Supra-Subduction Zone Pozantı-Karsantı-Ophiolite Southern Turkey: Evidence For High-Pressure Crystal Fractionation of Ultramafic Cumulates. Lithos, 65(1-2), 205-224. doi:10.1016/s0024-4937(02)00166-4
  • Pearce, J. A., Lippard, S. J., & Roberts, S. (1984). Characteristics and tectonic significance of supra-subduction zone ophiolites. Geological Society, London, Special Publications, 16, 77–94. doi:10.1144/GSL.SP.1984.016.01.06
  • Polat, A., & Casey, J. F. (1995). A Stuructural Record of The Emplacement of the Pozantı-Karsantı Ophiolite onto the Menderes-Taurus Block in The Late Cretaceus, Eastren Taurides, Turkey. Journal of Structural Geology, 17(12), 1673-1688. doi:10.1016/0191-8141(95)00061-h
  • Prichard, H. M., Barnes, S. J., Godel, B., Reddy, S. M., Vukmanovic, Z., Halfpenny, A., Neary, C. R., & Fisher, P. C. (2015). The structure of and origin of nodular chromite from the Troodos ophiolite, Cyprus, revealed using high-resolution X-ray computed tomography and electron backscatter diffraction. Lithos, 218-219, 87-98. doi:10.1016/j.lithos.2015.01.013
  • Roberts, S. (1988). Ophiolitic chromitite formation: a marginal basin phenomenon. Economic Geology, 83(5), 1034-1036. doi:10.2113/gsecongeo.83.5.1034
  • Takazawa, E., Frey, F. A., Shimizu, N., & Obata, M. (2000). Whole rock compositional variations in an upper mantle peridotite (Horoman, Hokkaido, Japan): are they consistent with a partial melting process? Geochemica et Cosmochimica Acta, 64(4), 695–716. doi:10.1016/S0016-7037(99)00346-4
  • Tekeli, O. (1981). Toros’larda Aladağ Ofiyolitli Melanjının Özellikleri. Türkiye Jeoloji Bülteni, 24, 57-64.
  • Tekeli, O., Aksay, A., Ürgün, B. M. & Işık, A. (1984). Geology of the Aladağ Mountains. Geology Of The Taurus Belt: Procedings Int. Sym., 26-29. September., 143-149. Ankara. Turkey.
  • Thayer, T. P. (1964). Principal Features and origin of podiform chromite deposits and some observations on the Guleman-Soridag District, Turkey. Economic Geology, 59(8), 1497-1524. doi:10.2113/gsecongeo.59.8.1497
  • Thayer, T. P. (1969). Peridodite-gabbro complexes as keys to petrology of mid-ocean ridges. Geological Society of American Bulletin, 80(8), 1511-1522. doi:10.1130/0016-7606(1969)80[1515:PCAKTP]2.0.CO;2
  • Uysal, I., Ersoy, E. Y., Karsli, O., Dilek, Y., Sadiklar, M. B., Ottley, C. J., Tiepolo, M., & Meisel, T. (2012). Coexistence of abyssal and ultra-depleted SSZ type mantle peridotites in a Neo-Tethyan Ophiolite in SW Turkey: Constraints from mineral composition, whole-rock geochemistry (major–trace–REE–PGE), and Re–Os isotope systematics. Lithos, 132–133, 50–69. doi:10.1016/j.lithos.2011.11.009
  • Yetiş, C. (1978). Geology of the Çamardı (Niğde) Region and the Characterics of the Ecemiş Fault Zone Between Maden Bogazı and Kamışlı. İstanbul Ünv. Fen Fak. Mecm. Seri E. 43, 41-61. (unpublished).
  • Yu, H., Zhang, H-F., Zou, H-B. & Yang, Y-H. (2019). Minor and trace element variations in chromite from the Songshugou dunites, North Qinling Orogen: Evidence for amphibolite-facies metamorphism. Lithos, 328-329, 146-158. doi:10.1016/j.lithos.2019.01.009
There are 32 citations in total.

Details

Primary Language English
Journal Section Geological Engineering
Authors

Ali Tümüklü 0000-0003-1215-8748

Publication Date December 30, 2021
Submission Date December 3, 2021
Published in Issue Year 2021

Cite

APA Tümüklü, A. (2021). Chromitite Ore Types and Geochemical Investigation of Pozantı-Karsantı Ophiolite in Mazmılı Region (Turkey). Gazi University Journal of Science Part A: Engineering and Innovation, 8(4), 537-550. https://doi.org/10.54287/gujsa.1032149