Skip to main content

Advertisement

Log in

DEM-derived geomorphic indices for assessment of tectonic activity at the Dara anticlinal oil structure within the Zagros fold-thrust belt, southwestern Iran

  • Original Paper
  • Published:
Arabian Journal of Geosciences Aims and scope Submit manuscript

Abstract

The Dara anticline is one of the anticlinal oil structures in the Zagros fold-and-thrust belt that were formed in the Dezful Embayment west of the Kazerun fault zone. Determination of the tectonically active parts of this structure is important for structural analysis and oil exploration. Consequently, we have used Arc GIS software to analyze active tectonics indexes including the following: hypsometric integral and hypsometric curve (Hi, Hc); elongation ratio (Bs, Re); drainage asymmetry factor (AF); valley floor width to height ratio (Vf); stream gradient index (SL); and swath profile with remote sensing applied to a digital elevation model (DEM). These methods indicate the amount of active longitudinal growth of the Dara anticline. The tectonic activity analyses show that both the northwest and southeast noses of the Dara anticline are more active than the middle parts and that the SE nose is more active than NW nose.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11

Similar content being viewed by others

References

  • Ahmadian J, Murata M, Nadimi A, Ozawa H, Kozai T (2014) Active tectonics of Iran deduced from earthquakes, active faulting and GPS evidences. Bulletin of Center for collaboration in Community, Naruto University of Education 28:11–22

    Google Scholar 

  • Al-Taj M, Shakour F, Atallah M (2007) Morphotectonic indices of the Dead Sea transform, Jordan. Geogr Fis Din Quat 30:5–11

    Google Scholar 

  • Beygi S, Nadimi A, Safaei H (2016) Tectonic history of seismogenic fault structures in Central Iran. J Geosci 61:127–144

    Article  Google Scholar 

  • Bull WB, McFadden LD (1977) Tectonic geomorphology north and south of the Garlock fault, California. In: Geomorphology in arid regions. Proceedings of the eighth annual geomorphology symposium; Sep 23-24. State University of New York, Binghamton

    Google Scholar 

  • Burberry CM, Cosgrove JW, Guoliu J (2008) Spatial arrangement of fold types in the Zagros simply folded belt, Iran, indicated by landform morphology and drainage pattern characteristics. J Maps:417–430

  • Carrubal S, Perottil CR, Buonaguro R, Calabro R, Carpi R, Naini M (2006) Structural pattern of the Zagros fold-and-thrust belt in the Dezful Embayment (SW Iran). Geological Society of America, Boulder Special Paper

    Google Scholar 

  • Dehbozorgi M, Pourkermani M, Arian M, Matkan AA, Motamedi H, Hosseiniasl A (2010) Quantitative analysis of relative tectonic activity in the Sarvestan area, central Zagros, Iran. Geomorphology 121:329–341

    Article  Google Scholar 

  • Ehsani J, Arian M (2015) Quantitative analysis of relative tectonic activity in the Jarahi-Hendijan basin area, Zagros, Iran. Geosci J 19(4):751–765

    Article  Google Scholar 

  • Elias Z, Sissakian VK, Al-Ansari N (2019) Assessment of the tectonic activity in northwestern part of the Zagros Mountains, Northeastern Iraq by using geomorphic indices. Geotech Geol Eng:1–13

  • Fakhari M, McQuillan H (1993) Bushehr geological map scale 1: 250000. National Iranian Oil Company, Tehran

    Google Scholar 

  • Hare PW, Gardner T (1985) Geomorphic indicators of vertical neotectonism along converging plate margins, Nicoya Peninsula, Costa Rica. Allen and Unwin, Boston, pp 75–104

    Google Scholar 

  • Hesami-Azar K, Jamali F, Tabasi H (2003) Active Fault of Iran (Map). IIEES (International Institute of Earthquake Engineering and Seismology), Tehran

    Google Scholar 

  • Hormozi Moghadam H (2017) Structural analyses of the Dara anticline, as one of the oil fields of Zagros fold-thrust belt [master’s thesis]. Urmia University: Iran

  • Hovius N (2000) Macro scale process systems of mountain belt erosion. Geomorphology and Global Tectonics, pp 77–105

  • Keller E (1977) Adjustments of drainage to bed rock in regions of contrasting tectonic frame work. Geol Soc Am Abstr Programs 9:1046

    Google Scholar 

  • Keller E, Pinter N (1996) Active tectonics: earthquake, uplift and landscape. Printice Hall, Upper Saddle River

    Google Scholar 

  • Keller EA, Pinter N (2002) Active tectonics, earthquakes, uplift and landscape, 2nd edn. Prentice Hall, Upper Saddle River 362 p

    Google Scholar 

  • Keller E, Rockwell T (1984) Tectonic geomorphology, quaternary chronology and paleoseismology. In: Costa JE, Fleisher PJ (eds) Development and application of geomorphology. Springer Verlag, Berlin, pp 203–239

    Chapter  Google Scholar 

  • Mitchell SG, Montgomery DR (2006) Influence of a glacial buzzsaw on the height and morphology of the Cascade Range in central Washington State, USA. Quat Res 65(1):96–107

    Article  Google Scholar 

  • Mohajjel M, Rasouli A (2014) Structural evidence for superposition of transtension on transpression in the Zagros collision zone: Main Recent Fault, Piranshahr area, NW Iran. J Struct Geol 62:65–79

    Article  Google Scholar 

  • Montgomery DR, Balco G, Willett SD (2001) Climate, tectonics, and the morphology of the Andes. Geology 29(7):579–582

    Article  Google Scholar 

  • Mouthereau F, Lacombe O, Vergés J (2012) Building the Zagros collisional orogen: timing, strain distribution and the dynamics of Arabia/Eurasia plate convergence. Tectonophysics 532–535:27–60

    Article  Google Scholar 

  • Pedrera A, Pérez-Peña JV, Galindo-Zaldívar J, Azañón JM, Azor A (2009) Testing the sensitivity of geomorphic indices in areas of low-rate active folding (eastern Betic Cordillera, Spain). Geomorphology 105(3):218–231

    Article  Google Scholar 

  • Pérez-Peña JV, Azor A, Azañón JM, Keller EA (2010) Active tectonics in the Sierra Nevada (Betic Cordillera, SE Spain): insights from geomorphic indexes and drainage pattern analysis. Geomorphology 119(1):74–87

    Article  Google Scholar 

  • Ramsey LA, Walker RT, Jackson J (2008) Fold evolution and drainage development in the Zagros mountains of Fars province, SE Iran. Basin Res 20:23–48

    Article  Google Scholar 

  • Safaei H (2009) The continuation of the Kazerun fault system across the Sanandaj–Sirjan zone (Iran). J Asian Earth Sci 35:391–400

    Article  Google Scholar 

  • Schumm SA (1956) Evolution of drainage systems and slopes in badlands at Perth Amboy, New Jersey. Geol Soc Am Bull 67(5):597–646

    Article  Google Scholar 

  • Sepehr M, Cosgrove JW (2005) Role of the Kazerun fault zone in the formation and deformation of the Zagros fold-thrust belt, Iran. Tectonics 24:1–13

    Article  Google Scholar 

  • Silva P, Goy J, Zazo C, Bardaji T (2003) Fault - generated mountain fronts in Southeast Spain: geomorphologic assessment of tectonic and seismic activity. Geomorphology. 50:203–225

    Article  Google Scholar 

  • Verrios S, Zygouri V, Kokkalas S (2004) Morphotectonic analysis in the Eliki fault zone (Gulf of Corinth, Greece). Bull Geol Soc Greece 36:1706–1715

    Article  Google Scholar 

  • Waikar ML, Nilawar AP (2014) Morphometric analysis of a drainage basin using geographical information system: a case study. Int J Multidiscip Curr Res 2:179–184

    Google Scholar 

  • Walcott RC, Summerfield M (2008) Scale dependence of hypsometric integrals: an analysis of southeast African basins. Geomorphology. 96(1):174–186

    Article  Google Scholar 

  • Zaberi M, Grutzner C, Navabpour P, Ustaszewski K (2019) Relative timing of uplift along the Zagros Mountain Front Flexure (Kurdistan Region of Iraq): constrained by geomorphic indices and landscape evolution modeling. Solid Earth 10:663–682

    Article  Google Scholar 

  • Zebari M (2013) Geometry and evolution of fold structures within the high folded zone: Zagros fold-thrust belt, Kurdistan region-Iraq [master’s thesis]. Lincoln, Nebraska

Download references

Acknowledgements

The support of Urmia University and facilities provided by the National Iranian South Oilfields Company are gratefully acknowledged.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Akram Alizadeh.

Additional information

Responsible Editor: Zeynal Abiddin Erguler

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Alizadeh, A., Hormozi Moghadam, H. & Seraj, M. DEM-derived geomorphic indices for assessment of tectonic activity at the Dara anticlinal oil structure within the Zagros fold-thrust belt, southwestern Iran. Arab J Geosci 13, 192 (2020). https://doi.org/10.1007/s12517-020-5156-8

Download citation

  • Received:

  • Accepted:

  • Published:

  • DOI: https://doi.org/10.1007/s12517-020-5156-8

Keywords

Navigation