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Tytuł artykułu

Lineaments in the Shamakhy–Gobustan and Absheron Hydrocarbon Containing Areas Using Gravity Data

Wybrane pełne teksty z tego czasopisma
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
In this study, we purposed to investigate the edge of geostructures and position of existing faults of the Shamakhy–Gobustan and Absheron hydrocarbon containing regions in Azerbaijan. For this purpose, the horizontal gradient, analytic signal, tilt angle, and hyperbolic of tilt angle methods were applied to the first vertical derivative of gravity data instead of Bouguer gravity data. We obtained the maps that show the previous lineaments which were designated by considering the maximum contours of horizontal gradient, analytic signal maps, and zero values of tilt angle, hyperbolic of tilt angle maps. The geometry of basement interface was also modeled utilizing the Parker–Oldenburg algorithm to understand the sediment thickness and coherency or incoherency between the gravity values and basement topography. The lineaments were held a candle to most current tectonic structure map of the study area. It was seen that the techniques used in this study are very effective to determine the old and new lineaments in the Shamakhy–Gobustan and Absheron regions. The epicenter distribution of earthquakes within the study area supports the new lineaments which are extracted by our interpretation. We concluded that better comprehension of Azerbaijan geostructures and its effect on the large scale works will be provided by means of this study.
Czasopismo
Rocznik
Strony
39--49
Opis fizyczny
Bibliogr. 31 poz.
Twórcy
autor
  • Department of Geophysics, Engineering Faculty, Karadeniz Technical University, Trabzon, Turkey
autor
  • Department of Geophysics, Engineering Faculty, Karadeniz Technical University, Trabzon, Turkey
  • Department of Geodynamics and Seismology, Institute of Geology and Geophysics, Azerbaijan National Academy of Sciences, Baku, Azerbaijan
Bibliografia
  • 1. Alizadeh AA, Guliyev IS, Kadirov FA, Eppelbaum LV (2016) Geosciences of Azerbaijan. Geology 1:237
  • 2. Altınoğlu FF, Sarı M, Aydın A (2015) Detection of lineaments in Denizli Basin of Western Anatolia region using bouguer gravity data. Pure Appl Geophys 172:415–425
  • 3. Ansari AH, Alamdar K (2011) A new edge detection method based on the analytic signal of tilt angle (ASTA) for magnetic and gravity anomalies. Iran J Sci Technol 35(A2):81–88
  • 4. Arısoy MÖ, Dikmen Ü (2011) Potensoft: MATLAB-based Software for potential field data processing, modelling and mapping. Comput Geosci 37:935–942
  • 5. Bilim F (2007) Investigation into the lineaments and thermal structure of Kütahya-Denizli Region Western Anatolia from using aeromagnetic, gravity and seismological data. Phys Earth Planet Inter 165:135–146
  • 6. Bochud M (2011) Tectonics of the eastern greater caucasus in Azerbaijan. In: GeoFocus, Vol 30, thesis No: 1733, PhD thesis in tectonics and general geology at the University of Fribourg (25 Oct 2011), Switzerland
  • 7. Brunet MF, Granath JW, Wilmsen M (2009) South Caspian to Central Iran basins: introduction. In: Brunet MF, Wilmsen M, Granath JW (eds) South Caspian to Central Iran basins, vol 312. The Geological Society of London, London, pp 1–10 (Special publication)
  • 8. Cooper GRJ, Cowan DR (2006) Enhancing potential field data using filters based on the local phase. Comput Geosci 32(10):1585–1591
  • 9. Cordell L, Grauch VJS (1985) Mapping basement magnetization zones from aeromagnetic data in the San Juan Basin, New Mexico. In: Hinze WJ (ed) The utility of regional gravity and magnetic anomaly maps. Society of Exploration Geophysicists, Tulsa, pp 181–197
  • 10. Evjen HM (1936) The place of the vertical gradient in gravitational interpretations. Geophysics 1:127–136
  • 11. Gomez-Ortiz D, Agarwal BNP (2005) 3DINVER.M: a MATLAB program to invert the gravity anomaly over a 3-D horizontal density interface by Parker–Oldenburg’s algorithm. Compu Geosci 31:513–520
  • 12. Gunn PJ (1975) Linear transformations of gravity and magnetic fields. Geophys Prospect 23(2):300–312
  • 13. International Seismological Centre (ISC) (2014), On-line Bulletin, http://www.isc.ac.uk, Internatl. Seismol. Cent., Thatcham, United Kingdom. Accessed 04 April 2017
  • 14. Kadirov FA (2000) Application of the Hartley transform for interpretation of gravity anomalies in the Shamakhy-Gobustan and Absheron oil- and gas-bearing regions Azerbaijan. J Appl Geophys 45:49–61
  • 15. Kadirov FA, Babayev G, Gadirov A (2012a) Analysis of horizontal to vertical spectra of microseismics for Baku City. In: Problems of Cybernetics and Informatics (PCI), 2012 IV International Conference
  • 16. Kadirov FA, Babayev G, Gadirov A, Safarov RT, Mukhtarov AS (2012b) Microzonation of the Baku city using miktrotremor measurements, In: Problems of reduction of natural hazards and risks, International scientific and practical conference “GEORISK 2012”. In 2 Vols. Volume 1. Moscow. Peoples’ Friendship University of Russia (PFUR), 384:94-98
  • 17. Kadirov FA, Ahadov BG, Gadirov AH, Babayev GR, Mammadov SG, Safarov RT (2015) Microtremor survey and spectral analyses of H/V ratio for Baku city (Azerbaijan). In: Proceedings of Azerbaijan national academy of sciences, the sciences of earth, no:3
  • 18. Kumar NJ, Singh AP, Rao MRKP, Chandrasekhar DV, Singh B (2009) Gravity signatures derived crustal structure and tectonics of Achankovil shear zone Southern India. Gondwana Res 16:45–55
  • 19. Miller HG, Singh V (1994) Potential field tilt -a new concept for location of potential field sources. J Appl Geophys 32:213–217
  • 20. Nabighian MN (1972) The Analytic Signal of two dimensional magnetic bodies with polygonal cross section: its properties and use for automated anomaly interpretation. Geophysics 37:507–517
  • 21. Oldenburg DW (1974) The inversion and interpretation of gravity anomalies. Geophysics 39:526–536
  • 22. Oruç B (2010) Edge detection and depth estimation using a tilt angle map from gravity gradient data of the Kozaklı-Central Anatolia Region Turkey. Pure Appl Geophys. https://doi.org/10.1007/s00024-010-0211-0
  • 23. Oruç B, Keskinsezer A (2008) Structural setting of the northeastern Biga Peninsula (Turkey) from tilt derivatives of gravity gradient tensors and magnitude of horizontal gravity components. Pure Appl Geophys 165:1913–1927
  • 24. Oruç B, Sertçelik İ, Kafadar Ö, Selim HH (2013) Structural interpretation of the Erzurum Basin Eastern Turkey, using curvature gravity gradient tensor and gravity inversion of basement relief. J Appl Geophys 88:105–113CrossRefGoogle Scholar
  • 25. Parker RL (1973) The rapid calculation of potential anomalies. Geophys J R Astr Soc 31:447–455
  • 26. Radjabov MM (1978) Study of the structure of the earth’s crust-consolidated complex of the Azerbaijan using deep seismic sounding and refracted wave-correlation method data the Structure of the Earth’s Crust and Upper Mantle in the Central and East Europe. Naukova Dumka, Kiev, pp 205–211 (In Russian)
  • 27. Saintot A, Brunet M-F, Yakovlev F, Sebrier M, Stephenson RA, Ershov AV, Chalot-Prat F, Mccann T (2006) The Mesozoic-Cenozoic tectonic evolution of the Greater Caucasus. Geol Soc Lond Mem 32:277–289
  • 28. Salem A, Williams S, Fairhead D (2008) Interpretation of magnetic data using tilt-angle derivatives. Geophysics 73:1–10
  • 29. Shikhalibeyli ESh (1972) Location of Azerbaijan in general structure of the Caucasus and surrounding folded region. In: Azizbekov ShA (ed) Geology of the USSR Azerbaijan, vol XLVII. Nedra, Moscow, pp 286–290
  • 30. Spector A, Grant FS (1970) Statistical models for interpreting aeromagnetic data. Geophysics 35:293–302
  • 31. Vincent SJ, Morton AC, Carter A, Gibbs S, Barabadze TG (2007) Oligocene uplift of the western Gre ater Caucasus: an effect of initial Arabia-Eurasia collision. Terra Nova 19:160–166
Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2018)
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-9b77c650-cf4a-4c6b-a7dd-80ad0b88debe
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