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SEYFE FAY ZONUNA AİT KİL MİNERALLERİNİN YAŞI, PETROGRAFİSİ VE KİNEMATİĞİ: ORTA ANADOLU, TÜRKİYE

Year 2018, Volume: 7 Issue: 3, 1066 - 1071, 28.12.2018

Mehmet Furkan Şener Mehmet Şener Muhammed Zeynel Öztürk1

Abstract

Çalışma alanı Orta Anadolu Kristalen
Karmaşığı (OAKK) içerisinde Seyfe Fay Zonu (SFZ) ve uzantısı olan Boğazlıyan
Fayı üzerinde yer almaktadır. SFZ, Orta Anadolu’daki en önemli bölgesel ölçekli
fay sistemlerinden birini temsil etmekte ve Neo-Tetis'in kapanması sırasında
ortaya çıkan çarpışma olaylarının kayıtlarını bulundurmaktadır. SFZ, BKB-DGD
doğrultulu sağ yanal doğrultu atımlı faylardan oluşmaktadır. Tüm kaya ve kil
XRD ile eser element verileri illitlerin derin tektonik aktivite esnasında
yüzeye ulaşan hidrotermal sulardan çökeldiğini göstermektedir. Bu akışkanlar,
sığ kırılgan deformasyon bölgeleri boyunca yüzeye doğru göç etmiştir. Farklı
kataklastik zonlardaki (1266, 1276 ve 1488 m) illitlerden yapılan Rb-Sr
jeokronolojisi aktivitenin yaşını 21,4 ± 0,57 My olarak göstermiştir. Buna göre
SFZ, Erken Miyosen’e kadar uzanır ve bu da hem göreceli yaşlarla hem de OAKK
içerisindeki yapılan önceki çalışmalarda önerilen yaş verileri ile tutarlıdır. Muhtemel
bir bindirme zonuna ait olan 1266 m ve 1276 m örnekleri Burdigaliyen dönemi
olarak kabul edilen Paleotetisin kapanmasının ve Neotetisin başlangıcının OAKK
içerisinde yaklaşık 21 my önce gerçekleştiğini ortaya koymaktadır.

Keywords

Seyfe Fay Zonu Boğazlıyan Fayı Jeokronoloji Rb-Sr Orta Anadolu

References

  • 1] ANGELİER, J.E, DUMONT, J.E, KARAMANDERESİ, H., POİSSON, A.M., ŞİMŞEK, Ş., UYSAL, Ş., “Analyses of fault mechanisms and expansion of southwestern Anatolia since the late Miocene”, Tectonophysics 75(3-4), TI-T9, 1981.
  • [2] KOÇYİĞİT, A., TÜRKMENOĞLU, A., BEYHAN, A., KAYMAKÇI, N., AKYOL, E., “Post-collisional tectonics of Eskişehir-Ankara-Çankırı segments of izmir-Ankara-Erzincan Suture Zone (IAESZ): Ankara orogenic phase”, Bull. Turk. Assoc. Pet. Geol. 6, 69-86, 1995.
  • [3] WESTAWAY, R., “Block rotations in Western Turkey I. Observational evidence”, The Journal of Geophysical Research, 95, 19857-19884, 1990.
  • [4] TAYMAZ. T., JACKSON, J., MCKENZİE. D.. “Active tectonics of the north and central Aegean Sea”, Geophysical Journal International, 106, 433-490, 1991.
  • [5] PRİCE, S.. SCOTT, B., “Fault-block rotations at the edge of a zone of continental extension, Southwest Turkey”, Journal of Structural Geology. 16, 381-392, 1994.
  • [6] GÖRÜR, N., ŞENGÖR, A.M.C., SAKINÇ, M., TÜYSÜZ, O., AKKÖK, R., YIĞITBAŞ, E., OKTAY, F.Y., BARKA, A., SANCA, N., ECEVITOĞLU, B., DEMIRBAŞ, E., ERSOY, Ş., ALGAN, O., GÜNEYSU, C., AYKOL, A., “Rift formation in the G6kova region, southwest Anatolia: implications for the opening of the Aegean Sea”, Geological Magazine, 132, 637-650, 1995.
  • [7] DIRIK, K., GÖNCÜOĞLU, M.C., “Neotectonic characteristics of Central Anatolia”, International Geology Review, 38, 807-817, 1996.
  • [8] ŞENGÖR, A.M.C., GÖRÜR, N., ŞAROĞLU, F., “Strike-slip deformation basin formation and sedimentation: Strike-slip faulting and related basin formation in zones of tectonic escape: Turkey as a case study”, In: Biddle, K.T, Christie-Blick, N. (Eds.) Strike-slip faulting and basin formation. Society of Economic Paleontologists and Mineralogist, Special Publication, 37, 227-264, 1985.
  • [9] FACCENNA, C., BELLIER, O., MARTINOD, J., PIROMALLO, C., REGARD, V., “Slab detachment beneath eastern Anatolia: a possible cause for the formation of the North Anatolian fault”, Earth and Planetary Science Letters, 242, 85–97, 2006.
  • [10] ŞENGÖR, A.M.C., YILMAZ, Y., “Tethyan evolution of Turkey: a plate tectonic approach”, Tectonopbysics, 75, 181 241, 1981.
  • [11] POISSON, A., GUEZOU, J.C., ÖZTÜRK, A., İNAN, S., TEMİZ, H., GÜRSOY, H., KAVAK, K.S., ÖZDEN, S., “Tectonic setting and evolution of the Sivas Basin, Central Anatolia, Turkey”, International Geology Review, 38, 838-853, 1996.
  • [12] YALINIZ, M.K., FLOYD, P.A., GÖNCÜOGLU, M.C., “Supra-subduction zone ophiolites of Central Anatolia: geochemical evidence from the Sarıkaraman Ophiolite, Aksaray, Turkey”, Mineralogical Magazine, 60, 697-710, 1996.
  • [13] ÇAPAN, U.Z., FLOYD, P.A., “Geochemical and petrographic features of metabasalts within units of the Ankara Mélange”, Ophioliti 10, 3-18, 1985.
  • [14] ISIK, V., UYSAL, I.T., CAGLAYAN, A., SEYITOGLU, G., “The evolution of intra-plate fault systems in central Turkey: Structural evidence and Ar-Ar and Rb-Sr age constraints for the Savcili Fault Zone”, Tectonics, 33 (10), 1875-1899, 2014.
  • [15] YALINIZ, M.K., FLOYD, P.A., GÖNCÜOĞLU, M.C., “Geochemistry of volcanic rocks from the Çiçekdağ Ophiolite, Central Anatolia, and their inferred tectonic setting within the northern branch of the Neotethyan Ocean”, In: Bozkurt E, Winchester J.A, Piper J.D.A, editors, Tectonics and Magmatism in Turkey and the Surrounding Area. Journal of the Geological Society London Special Publication 173: 203–218, 2000.
  • [16] KADIOĞLU, Y.K., DILEK, Y., GÜLEÇ, N., FOLAND, K.A., “Tectonomagmatic evolution of bimodal plutons in the Central Anatolian Crystalline Complex, Turkey”, Journal of Geology, 111, 671–690, 2003.
  • [17] İLBEYLI, N., PEARCE, J.A., THIRLWALL, M.F., MITCHELL, J.G., “Petrogenesis of collision-related plutonics in central Anatolia, Turkey”, Lithos 72, 163–182, 2004.
  • [18] KÖKSAL, S., ROMER, R.L., GÖNCÜO⁄LU, M.C., TOKSOY-KÖKSAL, F., “Timing of post-collisional H-type to A-type granitic magmatism: U-Pb titanite ages from Alpine central Anatolian granitoids (Turkey)”, International Journal of Earth Sciences, 93, 974–989, 2004.
  • [19] BOZTUĞ, D., JONCKHEERE, R.C, HEIZLER, M., RATSCHBACHER, L., HARLAVAN, Y., TICHOMIROVA, M., “Timing of post-obduction granitoids from intrusion through cooling to exhumation in central Anatolia, Turkey”, Tectonophysics, 473, 223-233, 2009.
  • [20] GÖRÜR, N., TÜYSÜZ, O. & ŞENGÖR, A.M.C. 1998. Tectonic evolution of the Central Anatolian Basins. International Geology Review 40, 831–850.
  • [21] ÇEMEN, İ., GÖNCÜOĞLU, M.C., DIRIK, K., “Structural evolution of the Tuzgölü basin in Central Anatolia, Turkey”, Journal of Geology, 107 (6), 693-706, 1999.
  • [22] JAFFEY, N., ROBERTSON, A.H.F., “Non-marine sedimentation associated with Oligocene-Recent exhumation and uplift of the Central Taurus Mountains, S Turkey”, Sedimentary Geology, 173: 53–89, 2005.
  • [23] KOÇYIĞIT, A., “Orta Anadolu’nun genel neotektonik özellikleri ve depremselliği”, Türkiye Petrol Jeologları Derneği, Özel Sayı, 5, 1- 26, 2003.

AGE, PETROGRAPHY AND KINEMATICS OF CLAY MİNERALS OF SEYFE FAULT ZONE: CENTRAL ANATOLIA, TURKEY

Year 2018, Volume: 7 Issue: 3, 1066 - 1071, 28.12.2018

Mehmet Furkan Şener Mehmet Şener Muhammed Zeynel Öztürk1

Abstract

The study area is located on the Seyfe Fault Zone (SFZ) and Boğazlıyan
Fault which is thought to be extension of Seyfe Fault Zone in Central Anatolian
Crystalline Complex (CACC). The SFZ represents one of the most important
regional-scale fault systems in Central Anatolia and has records the collision
events that occurred during the closure of Neo-Tethys. The SFZ consists of
WNW-ESE oriented dextral strike-slip faults. Whole rock and clay XRD and trace
element data show that clay minerals collapse from hydrothermal water reaching
the surface during deep tectonic activity. These fluids are migrated upward
along shallow fragile deformation zones. The age of Rb-Sr geochronology of
three different cataclastic zones as 1266, 1276 and 1488
m, showed the age of activity as 21.4 ± 0.57 Ma. According to this, the SFZ
extends to the early Miocene and is consistent with both the relative age and
the age data suggested in previous studies conducted within the CACC. Samples of 1266 m and 1276 m belonging to a possible
thrust zone reveal that the closure of Palaeotethys and the beginning of
Neotethys, which is accepted as Burdigalian period, occurred around 21 Ma ago
in the Central Anatolian Crystalline Complex.

Keywords

Seyfe Fault Zone Boğazlıyan Fault Geochronology Rb-Sr Central Anatolia

References

  • 1] ANGELİER, J.E, DUMONT, J.E, KARAMANDERESİ, H., POİSSON, A.M., ŞİMŞEK, Ş., UYSAL, Ş., “Analyses of fault mechanisms and expansion of southwestern Anatolia since the late Miocene”, Tectonophysics 75(3-4), TI-T9, 1981.
  • [2] KOÇYİĞİT, A., TÜRKMENOĞLU, A., BEYHAN, A., KAYMAKÇI, N., AKYOL, E., “Post-collisional tectonics of Eskişehir-Ankara-Çankırı segments of izmir-Ankara-Erzincan Suture Zone (IAESZ): Ankara orogenic phase”, Bull. Turk. Assoc. Pet. Geol. 6, 69-86, 1995.
  • [3] WESTAWAY, R., “Block rotations in Western Turkey I. Observational evidence”, The Journal of Geophysical Research, 95, 19857-19884, 1990.
  • [4] TAYMAZ. T., JACKSON, J., MCKENZİE. D.. “Active tectonics of the north and central Aegean Sea”, Geophysical Journal International, 106, 433-490, 1991.
  • [5] PRİCE, S.. SCOTT, B., “Fault-block rotations at the edge of a zone of continental extension, Southwest Turkey”, Journal of Structural Geology. 16, 381-392, 1994.
  • [6] GÖRÜR, N., ŞENGÖR, A.M.C., SAKINÇ, M., TÜYSÜZ, O., AKKÖK, R., YIĞITBAŞ, E., OKTAY, F.Y., BARKA, A., SANCA, N., ECEVITOĞLU, B., DEMIRBAŞ, E., ERSOY, Ş., ALGAN, O., GÜNEYSU, C., AYKOL, A., “Rift formation in the G6kova region, southwest Anatolia: implications for the opening of the Aegean Sea”, Geological Magazine, 132, 637-650, 1995.
  • [7] DIRIK, K., GÖNCÜOĞLU, M.C., “Neotectonic characteristics of Central Anatolia”, International Geology Review, 38, 807-817, 1996.
  • [8] ŞENGÖR, A.M.C., GÖRÜR, N., ŞAROĞLU, F., “Strike-slip deformation basin formation and sedimentation: Strike-slip faulting and related basin formation in zones of tectonic escape: Turkey as a case study”, In: Biddle, K.T, Christie-Blick, N. (Eds.) Strike-slip faulting and basin formation. Society of Economic Paleontologists and Mineralogist, Special Publication, 37, 227-264, 1985.
  • [9] FACCENNA, C., BELLIER, O., MARTINOD, J., PIROMALLO, C., REGARD, V., “Slab detachment beneath eastern Anatolia: a possible cause for the formation of the North Anatolian fault”, Earth and Planetary Science Letters, 242, 85–97, 2006.
  • [10] ŞENGÖR, A.M.C., YILMAZ, Y., “Tethyan evolution of Turkey: a plate tectonic approach”, Tectonopbysics, 75, 181 241, 1981.
  • [11] POISSON, A., GUEZOU, J.C., ÖZTÜRK, A., İNAN, S., TEMİZ, H., GÜRSOY, H., KAVAK, K.S., ÖZDEN, S., “Tectonic setting and evolution of the Sivas Basin, Central Anatolia, Turkey”, International Geology Review, 38, 838-853, 1996.
  • [12] YALINIZ, M.K., FLOYD, P.A., GÖNCÜOGLU, M.C., “Supra-subduction zone ophiolites of Central Anatolia: geochemical evidence from the Sarıkaraman Ophiolite, Aksaray, Turkey”, Mineralogical Magazine, 60, 697-710, 1996.
  • [13] ÇAPAN, U.Z., FLOYD, P.A., “Geochemical and petrographic features of metabasalts within units of the Ankara Mélange”, Ophioliti 10, 3-18, 1985.
  • [14] ISIK, V., UYSAL, I.T., CAGLAYAN, A., SEYITOGLU, G., “The evolution of intra-plate fault systems in central Turkey: Structural evidence and Ar-Ar and Rb-Sr age constraints for the Savcili Fault Zone”, Tectonics, 33 (10), 1875-1899, 2014.
  • [15] YALINIZ, M.K., FLOYD, P.A., GÖNCÜOĞLU, M.C., “Geochemistry of volcanic rocks from the Çiçekdağ Ophiolite, Central Anatolia, and their inferred tectonic setting within the northern branch of the Neotethyan Ocean”, In: Bozkurt E, Winchester J.A, Piper J.D.A, editors, Tectonics and Magmatism in Turkey and the Surrounding Area. Journal of the Geological Society London Special Publication 173: 203–218, 2000.
  • [16] KADIOĞLU, Y.K., DILEK, Y., GÜLEÇ, N., FOLAND, K.A., “Tectonomagmatic evolution of bimodal plutons in the Central Anatolian Crystalline Complex, Turkey”, Journal of Geology, 111, 671–690, 2003.
  • [17] İLBEYLI, N., PEARCE, J.A., THIRLWALL, M.F., MITCHELL, J.G., “Petrogenesis of collision-related plutonics in central Anatolia, Turkey”, Lithos 72, 163–182, 2004.
  • [18] KÖKSAL, S., ROMER, R.L., GÖNCÜO⁄LU, M.C., TOKSOY-KÖKSAL, F., “Timing of post-collisional H-type to A-type granitic magmatism: U-Pb titanite ages from Alpine central Anatolian granitoids (Turkey)”, International Journal of Earth Sciences, 93, 974–989, 2004.
  • [19] BOZTUĞ, D., JONCKHEERE, R.C, HEIZLER, M., RATSCHBACHER, L., HARLAVAN, Y., TICHOMIROVA, M., “Timing of post-obduction granitoids from intrusion through cooling to exhumation in central Anatolia, Turkey”, Tectonophysics, 473, 223-233, 2009.
  • [20] GÖRÜR, N., TÜYSÜZ, O. & ŞENGÖR, A.M.C. 1998. Tectonic evolution of the Central Anatolian Basins. International Geology Review 40, 831–850.
  • [21] ÇEMEN, İ., GÖNCÜOĞLU, M.C., DIRIK, K., “Structural evolution of the Tuzgölü basin in Central Anatolia, Turkey”, Journal of Geology, 107 (6), 693-706, 1999.
  • [22] JAFFEY, N., ROBERTSON, A.H.F., “Non-marine sedimentation associated with Oligocene-Recent exhumation and uplift of the Central Taurus Mountains, S Turkey”, Sedimentary Geology, 173: 53–89, 2005.
  • [23] KOÇYIĞIT, A., “Orta Anadolu’nun genel neotektonik özellikleri ve depremselliği”, Türkiye Petrol Jeologları Derneği, Özel Sayı, 5, 1- 26, 2003.
There are 23 citations in total.

Details

Primary Language Turkish
Subjects Engineering
Journal Section Others
Authors

Mehmet Furkan Şener 0000-0002-7362-2738

Mehmet Şener This is me 0000-0001-9284-673X

Muhammed Zeynel Öztürk1 0000-0002-9834-7680

Publication Date December 28, 2018
Submission Date November 14, 2018
Acceptance Date December 21, 2018
Published in Issue Year 2018 Volume: 7 Issue: 3

Cite

APA Şener, M. F., Şener, M., & Öztürk1, M. Z. (2018). SEYFE FAY ZONUNA AİT KİL MİNERALLERİNİN YAŞI, PETROGRAFİSİ VE KİNEMATİĞİ: ORTA ANADOLU, TÜRKİYE. Niğde Ömer Halisdemir Üniversitesi Mühendislik Bilimleri Dergisi, 7(3), 1066-1071.
AMA Şener MF, Şener M, Öztürk1 MZ. SEYFE FAY ZONUNA AİT KİL MİNERALLERİNİN YAŞI, PETROGRAFİSİ VE KİNEMATİĞİ: ORTA ANADOLU, TÜRKİYE. NOHU J. Eng. Sci. December 2018;7(3):1066-1071.
Chicago Şener, Mehmet Furkan, Mehmet Şener, and Muhammed Zeynel Öztürk1. “SEYFE FAY ZONUNA AİT KİL MİNERALLERİNİN YAŞI, PETROGRAFİSİ VE KİNEMATİĞİ: ORTA ANADOLU, TÜRKİYE”. Niğde Ömer Halisdemir Üniversitesi Mühendislik Bilimleri Dergisi 7, no. 3 (December 2018): 1066-71.
EndNote Şener MF, Şener M, Öztürk1 MZ (December 1, 2018) SEYFE FAY ZONUNA AİT KİL MİNERALLERİNİN YAŞI, PETROGRAFİSİ VE KİNEMATİĞİ: ORTA ANADOLU, TÜRKİYE. Niğde Ömer Halisdemir Üniversitesi Mühendislik Bilimleri Dergisi 7 3 1066–1071.
IEEE M. F. Şener, M. Şener, and M. Z. Öztürk1, “SEYFE FAY ZONUNA AİT KİL MİNERALLERİNİN YAŞI, PETROGRAFİSİ VE KİNEMATİĞİ: ORTA ANADOLU, TÜRKİYE”, NOHU J. Eng. Sci., vol. 7, no. 3, pp. 1066–1071, 2018.
ISNAD Şener, Mehmet Furkan et al. “SEYFE FAY ZONUNA AİT KİL MİNERALLERİNİN YAŞI, PETROGRAFİSİ VE KİNEMATİĞİ: ORTA ANADOLU, TÜRKİYE”. Niğde Ömer Halisdemir Üniversitesi Mühendislik Bilimleri Dergisi 7/3 (December 2018), 1066-1071.
JAMA Şener MF, Şener M, Öztürk1 MZ. SEYFE FAY ZONUNA AİT KİL MİNERALLERİNİN YAŞI, PETROGRAFİSİ VE KİNEMATİĞİ: ORTA ANADOLU, TÜRKİYE. NOHU J. Eng. Sci. 2018;7:1066–1071.
MLA Şener, Mehmet Furkan et al. “SEYFE FAY ZONUNA AİT KİL MİNERALLERİNİN YAŞI, PETROGRAFİSİ VE KİNEMATİĞİ: ORTA ANADOLU, TÜRKİYE”. Niğde Ömer Halisdemir Üniversitesi Mühendislik Bilimleri Dergisi, vol. 7, no. 3, 2018, pp. 1066-71.
Vancouver Şener MF, Şener M, Öztürk1 MZ. SEYFE FAY ZONUNA AİT KİL MİNERALLERİNİN YAŞI, PETROGRAFİSİ VE KİNEMATİĞİ: ORTA ANADOLU, TÜRKİYE. NOHU J. Eng. Sci. 2018;7(3):1066-71.
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