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Farimani, A. A-Moridi
- Study on Gourband Fault Activity on the Basis of Neotectonic Evidences (northeast of Torbat-e-Jam)
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Authors
Affiliations
1 Department of Geology, Science and Research Branch, Islamic Azad University, Hesarak, Tehran, IR
2 Department of geology, University of Birjand, Iran, PO Box: 56, Birjand, IR
3 Department of geology, University of Sistan & Balochestan, IR
1 Department of Geology, Science and Research Branch, Islamic Azad University, Hesarak, Tehran, IR
2 Department of geology, University of Birjand, Iran, PO Box: 56, Birjand, IR
3 Department of geology, University of Sistan & Balochestan, IR
Source
Indian Journal of Science and Technology, Vol 5, No 11 (2012), Pagination: 3642-3646Abstract
Gourband is the largest fault in the Alluvial Sediments of Torbt-e-Jam Plain. This fault is extended from northwest to southeast. Regarding its adjacency to the town and various villages, it is important to study Geotectonic activity. It is found that there are various geomorphologic abnormities along Gourband Fault. In this research, the effect of current movements of this fault on the structural Geomorphology of this zone has been studied. Fault scarps redirecting rivers and channels, folds of quaternary deposits and discoloration of sediments in the fault fields are important geomorphologic indicators that found in the desert site and in association with movement on Gourband Fault. The dip of fault is 50-60 degrees. The reverse component causes uplifting that forms maintains and it controls the current topography of the areas. Also, direct of waterways indicates direct of moving strike- slip of fault. Regarding dextral displacement of these waterways, it is found dextral strike-slip movement in the fault. Elevation of Neogene's Sediments of the fault surface indicates uplifting and reverse component in the fault.Keywords
Fault Scarps Torbat-e-Jam, Geomorphology, IranFull Text
References
- Aqanbaty A, (2004). Geological Survey of Iran, Geological and Mineral Exploration.
- Berberian M, Qarshi M, Arjangravesh b, MohajerAshjy, or., (1992). Research and Neotectonics, seismotectonics and seismic hazard - big and faulting in the expanse around Qazvin, Geological and Mineral Exploration country report No. 61.
- Jami M. (2011). Risk analysis of earthquake faulting in The expanse of plains Torbat e jam, geology master’s thesis.University of Sistan and Baluchestan.
- Salarvnd I. (2006). Risk assessment of earthquake - faulting in the expanse of Nehbandan, geology master’s thesis.University of Sistan and Baluchestan.
- PourKermani M, solgi A (2009), Morphotectonic, Copyright MIT, Islamic Azad University, Tehran, Iran,.
- Mohsen Pvrkrmany, Arian, Mehran (2001). Structural geomorphology of northeastern Kurdistan, Sistan and Baluchestan University Journal of Humanities. Seventh year.No. 16.
- Pour-Mohammadi, B (1996), Morphotectonic Karkheh River, Proceedings of the Fourth Seminar on River Engineering. Chamran University martyr.
- Sadat, Mir Ali Akbar (1996). Tectonic map of Iran, published by the Geological Survey.
- NainiAlavi M, 1:100000 map Torbat Geology, Geological Survey and GSI.pp, 151.
- Moghimi E (2005), Alluvial cone of the wind and change processes in the Lut Desert, Journal of Geographical Research. Number 52.
- Bull W B, Mcfadden L D, Tectonic geomorphology north and south of the Garlok fault, California. 8th Annual geomorphology sym., New York. 1977 Enertec, Saveh site confirmation studies, preliminary report, phase 1B investigation. Vol 1, Geology and seismology. Atomic Energy Organization of Iran, Tehran, 1978.
- Eduard A. Koster., (2005). The Physical Geography of Western Europe, ISBN 0199277753, Ch. 2: Neotectonics,.
- Spyros B. Pavlides., (1989).Looking for a definition of neotectonics, Terra Nova, Vol. 1, No. 3, pp. 233-235, University of Nevada, Reno.”Center for Neotectonic Studies
- Becker A., (1993) “ An attempt to define a “neotectonic period” for central and northern Europe”, International Journal of Earth Sciences, Vol. 82, pp.67-83, No. 1, doi:10.1007/BF00563271.
- Rockwell T. K. Keller, E. A. and Johnson, D. L., (1987). tectonic geomorphology of alluvial fans and mountain fronts near ventura California in: Tectonic geomorphology (edited Morisawa, M. and Hack, J. T.) Allen and Uniwin, Boston183-208.
- Vedder J G, Wallace R E, (1970). Map showing recently active breaks along the Son Andreas and related faults between Cholame valley and Tejon Pass, U.S. Geologic Survey, California.
- R. Tejero, J M. Gonzalez-Casado, D. Gomez-Ortiz, and F. Sanchez-Serrano(2006). Insights into the “tectonic topography” of the present-day landscape of the Central Iberian Peninsula (Spain), Geomorphology 76, pp.280-294.
- Stockline, J, Eftekhar - Nezad, J, and Hushmandzadeh, A (1973). Central Lut reconnaissance: East Iran. Geol. Surv. Iran. Rep: 22.
- Q.C. Sung, Y.C. Chen, K.Y. Cheng (2004). Geomorphic evidence and kinematic model for the Quaternary Transfer Faulting of the Pakuashan Anticline, Central Taiwan. Journal of Asian Earth Science (SCI) 24, pp.389-404.