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Kızıldere Killerinin (ARSUZ-HATAY) Ana Kaya Karakteristikleri

Year 2018, Volume: 39 Issue: 2, 524 - 530, 29.06.2018
https://doi.org/10.17776/csj.429709

Abstract

İskenderun körfezi, Adana
Havzasının devamı niteliğindedir ve oluşum mekanizması bakımından hidrokarbon
aramaları için uygun yerdir. Petrol oluşum mekanizmasında ana kaya, rezervuar
ve örtü kaya litolojik özelliklerini gösterebilecek kayaların bulunması gerekmektedir.
İskenderun havzasında rezervuar ve örtü kaya litolojisinde formasyonlar
mevcuttur.

Ana kaya olan Kızıldere formasyonu
gri renkli kumtaşı kiltaşı ardışımlarından meydana gelmektedir. Kumtaşları
katmanları 10-50 cm kalınlığındadır ve kiltaşı katmanlarının kalınlıkları ise
2-30 cm arasında değişmektedir. Kumtaşı ve kiltaşı ardışımının üstünde yer yer
tabakalı jibs seviyeleri gözlemlenmektedir ve katman kalınlıkları 5-15 cm
arasındadır.

Kızıldere Formasyonu killerinin
hidrokarbon üretimi TOK(Toplam Organik Karbon) miktarının hesaplanmasıyla bulunmuştur
ve bu değer ortalama %0.56 olarak belirlenmiştir. Ayrıca bölgede TOC
değerlerinin bölgenin Kuzey ve Kuzey doğusunda yüksektir ve güneye gidildikçe
azalma görülmüştür.







Misis yükselimine bağlı olarak
tektonik çatlakların bol görüldüğü bölgece kiltaşı kumtaşı ardışımlı
formasyonda kumtaşlarının rezervuar kaya, üzerine gelen Haymaseki formasyonu
olarak bilinen evaporitik birimler ise örtü kaya niteliğindedir. 

References

  • [1]. Durand B., Espitalie, J., Et Nicaise, G., Etude De La Matiere Organique İnsoluble Des Argiles Du Toarcien De Bassin De Paris. Etude par les procedes optiques analyse elemantaire, etude microscopie et diffraction electronniques: Rev. Ist. Fr. Petr., 27 (1972) 865-884.
  • [2]. Dessort, D., Gelin, F., Duclerc, D., Le-Van-Loi, R., Enhanced assessment of the distribution of organic matter in unconventional plays and tarmat in reservoirs using a new laser pyrolysis method on core. In: SPE 161626, presented at the Abue Dhabi International Petroleum Exhibition and Conference in Abu Dhabi, UAE, 211–14 November 2012.
  • [3]. Washburn, K.E., Rapid geochemical and mineralogical characterization of shale by laser-induced breakdown spectroscopy. Org. Geochem., 83–84 (2015) 114 – 117.
  • [4]. Charsky, A., Herron, S., Accurate, direct total organic carbon (TOC) log from a new advanced geochemical spectroscopy tool: comparisons with conventional approaches for TOC estimation. In: AAPG Paper 1547013, presented at the AAPG Annual Conference and Exhibition, Pittsburgh, Pennsylvania, 20–22 May 2013.
  • [5]. Baumgardner, R.W., and H.S., Hamlin, Core-based Geochemical study of Mudrocks in Basinal Lithofacies in the Wolfberry Play, Midland Basin, Texas, Part II: Search and Discovery Article no. 10572, 2014.
  • [6]. Hunt J. M., Petroleum Geochemistry and Geology, W.H. Freeman and Company, New York, 743, 1995.
  • [7]. Loverson A. İ., 1967. Geologie of Petroleum: W. H. Free, Comp, SanFransisco.
  • [8]. Ronov, AJB., Organic carbon in sedimentary rocks: Geochemistry, 5 (1958) 496-509.
  • [9]. Aksu, R., Demirkol, C., Quantitative basin modeling and hydrocarbon potential of İskenderun Basin. TAPG Bulletin, 13-1 (2001) 65–117.
  • [10]. Kozlu, H., İskenderun Baseni jeolojisi ve petrol olanakları :TPAO Rapor no.1921, 1982.
  • [11]. Kozlu, H., Doğu Akdeniz Bölgesinde yer alan Neojen basenlerinin (İskenderun Misis-Andırın) tektono-stratigrafi birimleri ve bunların tektonik gelişimi. Ç.Ü. Fen Bilimleri Enstitüsü Jeoloji Mühendisligi Anabilim Dalı, Doktora Tezi, 1997; 188s.
  • [12]. Schmidt, G., Stratigrafic nomenclature for the Adana region petroleum distirict VII.Petroleum Administration Pub. Bull., 1961.
  • [13]. Kozlu, H., Stratigraphy and structural evolution around Misis–Andırın (SE Turkey). 7th Turkish Petroleum Congress, Ankara, Geology Announcements, pp (1987) 104–116.
  • [14]. Donat, D., Sinanlı-Samandağ ve Arsuz-İskenderun (Hatay) Yöresi Miyo-Pliyosen Geçişinde Yer Alan Çökellerin Mikropaleontolojik İncelemesi ve Ortamsal Yorumu, Ç.Ü. Fen Bilimleri Enstitüsü Jeoloji Mühendisligi Anabilim Dalı, Yüksek Lisans Tezi, 2009; 133s.
  • [15]. Kozlu, H., Tectono-stratigraphic units of the Neogene basins (İskenderun, Misis– Andırın) and their tectonic evolution in the eastern Mediterranean region. Çukurova Univ. Natural Science Institute, Adana–Turkey, unpublished Ph.D. Thesis, 1997; 189 p.
  • [16]. Tekin, E., Varol, B., & Ayyıldız, T. Sedimentology and paleoenvironmental evolution of Messinian evaporites in the Iskenderun–Hatay basin complex, Southern Turkey. Sedimentary Geology, 229-4 (2010) 282-298.
  • [17]. Ruble et al., Tim Ruble, Richard J. Heck, A. Drozd William Practical Geochemical Methods to Assess Unconventional Reservoirs Weatherford International Ltd., 2015.

Source Rock Characterictic of The Kızıldere Clays (ARSUZ-HATAY)

Year 2018, Volume: 39 Issue: 2, 524 - 530, 29.06.2018
https://doi.org/10.17776/csj.429709

Abstract

Iskenderun Bay is the extension of the Adana Basin and
is a convenient place for hydrocarbon exploration in terms of its formation
mechanism. It is necessary to find rocks that can display lithological
properties of source, reservoir and cover rocks in the mechanism of oil
formation. There are formations in reservoir and cover rock lithology in
İskenderun basin.

Kızıldere formation, which is the main rock, has
gray-colored sandstone claystone sequences. Sandstones are 10-50 cm thick and
claystones 2-30 cm thick. Stratified gypsium levels are observed at the top of
the succession of sandstone and claystone and the thickness of the layers is
between 5 and 15 cm. The hydrocarbon production of Kızıldere Formation clay was
found by calculating the amount of TOC (Total Organic Carbon) and the average
value was 0.56%.  In addition, TOC values
in the region are higher in the north and north east of the region and decrease
in the south.





The sandstones in the region where the tectonic fractures
are abundant due to MisisAndırın systems are reservoir rocks, and the
evaporitic units known as Haymaseki formation are cover rocks.

References

  • [1]. Durand B., Espitalie, J., Et Nicaise, G., Etude De La Matiere Organique İnsoluble Des Argiles Du Toarcien De Bassin De Paris. Etude par les procedes optiques analyse elemantaire, etude microscopie et diffraction electronniques: Rev. Ist. Fr. Petr., 27 (1972) 865-884.
  • [2]. Dessort, D., Gelin, F., Duclerc, D., Le-Van-Loi, R., Enhanced assessment of the distribution of organic matter in unconventional plays and tarmat in reservoirs using a new laser pyrolysis method on core. In: SPE 161626, presented at the Abue Dhabi International Petroleum Exhibition and Conference in Abu Dhabi, UAE, 211–14 November 2012.
  • [3]. Washburn, K.E., Rapid geochemical and mineralogical characterization of shale by laser-induced breakdown spectroscopy. Org. Geochem., 83–84 (2015) 114 – 117.
  • [4]. Charsky, A., Herron, S., Accurate, direct total organic carbon (TOC) log from a new advanced geochemical spectroscopy tool: comparisons with conventional approaches for TOC estimation. In: AAPG Paper 1547013, presented at the AAPG Annual Conference and Exhibition, Pittsburgh, Pennsylvania, 20–22 May 2013.
  • [5]. Baumgardner, R.W., and H.S., Hamlin, Core-based Geochemical study of Mudrocks in Basinal Lithofacies in the Wolfberry Play, Midland Basin, Texas, Part II: Search and Discovery Article no. 10572, 2014.
  • [6]. Hunt J. M., Petroleum Geochemistry and Geology, W.H. Freeman and Company, New York, 743, 1995.
  • [7]. Loverson A. İ., 1967. Geologie of Petroleum: W. H. Free, Comp, SanFransisco.
  • [8]. Ronov, AJB., Organic carbon in sedimentary rocks: Geochemistry, 5 (1958) 496-509.
  • [9]. Aksu, R., Demirkol, C., Quantitative basin modeling and hydrocarbon potential of İskenderun Basin. TAPG Bulletin, 13-1 (2001) 65–117.
  • [10]. Kozlu, H., İskenderun Baseni jeolojisi ve petrol olanakları :TPAO Rapor no.1921, 1982.
  • [11]. Kozlu, H., Doğu Akdeniz Bölgesinde yer alan Neojen basenlerinin (İskenderun Misis-Andırın) tektono-stratigrafi birimleri ve bunların tektonik gelişimi. Ç.Ü. Fen Bilimleri Enstitüsü Jeoloji Mühendisligi Anabilim Dalı, Doktora Tezi, 1997; 188s.
  • [12]. Schmidt, G., Stratigrafic nomenclature for the Adana region petroleum distirict VII.Petroleum Administration Pub. Bull., 1961.
  • [13]. Kozlu, H., Stratigraphy and structural evolution around Misis–Andırın (SE Turkey). 7th Turkish Petroleum Congress, Ankara, Geology Announcements, pp (1987) 104–116.
  • [14]. Donat, D., Sinanlı-Samandağ ve Arsuz-İskenderun (Hatay) Yöresi Miyo-Pliyosen Geçişinde Yer Alan Çökellerin Mikropaleontolojik İncelemesi ve Ortamsal Yorumu, Ç.Ü. Fen Bilimleri Enstitüsü Jeoloji Mühendisligi Anabilim Dalı, Yüksek Lisans Tezi, 2009; 133s.
  • [15]. Kozlu, H., Tectono-stratigraphic units of the Neogene basins (İskenderun, Misis– Andırın) and their tectonic evolution in the eastern Mediterranean region. Çukurova Univ. Natural Science Institute, Adana–Turkey, unpublished Ph.D. Thesis, 1997; 189 p.
  • [16]. Tekin, E., Varol, B., & Ayyıldız, T. Sedimentology and paleoenvironmental evolution of Messinian evaporites in the Iskenderun–Hatay basin complex, Southern Turkey. Sedimentary Geology, 229-4 (2010) 282-298.
  • [17]. Ruble et al., Tim Ruble, Richard J. Heck, A. Drozd William Practical Geochemical Methods to Assess Unconventional Reservoirs Weatherford International Ltd., 2015.
There are 17 citations in total.

Details

Primary Language English
Journal Section Engineering Sciences
Authors

Esef Kılınç 0000-0002-5510-1568

Meryem Yeşilot Kaplan

Publication Date June 29, 2018
Submission Date June 1, 2018
Acceptance Date June 7, 2018
Published in Issue Year 2018Volume: 39 Issue: 2

Cite

APA Kılınç, E., & Yeşilot Kaplan, M. (2018). Source Rock Characterictic of The Kızıldere Clays (ARSUZ-HATAY). Cumhuriyet Science Journal, 39(2), 524-530. https://doi.org/10.17776/csj.429709