PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

Determination of Slip-Rate by Optical Dating of Lake Bed Sediments from the Dasht-E-Bayaz Fault, Ne Iran

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The Dasht-e-Bayaz left-lateral strike-slip fault in northeastern Iran ruptured in two destructive earthquakes in 1968 and 1979. The western half of the Dasht-e-Bayaz fault cuts across the dry lake-bed in the Nimbluk valley and has no measurable relief except for at a few localised jogs in the fault trace. We provide the first quantitative constraint on the slip-rate of the Dasht-e-Bayaz fault averaged over the Holocene. The western part of the fault cuts across the Nimbluk valley; the flat surface of which is composed of lake-bed sediments. Small streams cut into the surface of the lake-beds are displaced across the fault by 26 ± 2 m. Two OSL samples of the lake-bed sediments are successfully dated at 8.6 ± 0.6 and 8.5 ± 1.0 ka, from which we calculate a minimum slip-rate of 2.6 mm/yr. This minimum slip rate remains constant with the previously proposed Holocene slip rate of 2.5 mm/yr and within the range of the Holocene slip rate of 2.4 ± 0.3 mm/yr estimated before on the central section of the Doruneh fault.
Słowa kluczowe
Wydawca
Czasopismo
Rocznik
Strony
148--157
Opis fizyczny
Bibliogr. 28 poz., rys.
Twórcy
autor
  • Institute of Geophysics, Tehran University, Kargar Shomali, Tehran, Iran
  • The School of Geography, University of Oxford, south park road, Oxford OX1 3QY, UK
autor
  • Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX1 3AN, UK
autor
  • Department of geology, Birjand University, P.o.Box 131, Birjand, Iran
  • 4Department of geology, Birjand University, P.o.Box 131, Birjand, Iran
autor
  • Geological Survey of Iran, Azadi Square, Meraj Avenue, P.O. Box 11365-4563, Tehran, Iran
Bibliografia
  • 1. Ambraseys NN and Melville CP, 1982. A history of Persian earthquakes. Cambridge University Press, UK.
  • 2. Ambraseys NN and Tchalenko JS, 1969. The Dasht-e-Bayaz (Iran) earthquake of August 31, 1968: a field report. Bulletin of the Seismological Society of America 59: 1751–1792.
  • 3. Armitage SJ and Bailey RM, 2005. The measured dependence of laboratory beta dose rates on sample grain size. Radiation Measurements 39: 123–127, DOI 10.1016/j.radmeas.2004.06.008.
  • 4. Berberian M, 1976. Contribution to the seismotectonics of Iran (Part II). Report No. 39. Geological Survey of Iran.
  • 6. Berberian M and Yeats RS, 1999a. Patterns of historical earthquake rupture in the Iranian Plateau. Bulletin of the Seismological Society of America 89: 120–139.
  • 7. Berberian M and Yeats RS, 1999b. Contribution of archaeological data to studies of earthquake history in the Iranian Plateau. Journal of Structural Geology 23: 563–584, DOI 10.1016/S0191- 8141(00)00115-2.
  • 8. Berberian M, Jackson JA, Qorashi M, Khatib MM, Priestley K, Talebian M and Ghafuri-Ashtiani M, 1999. The 1997 May 10 Zirkuh (Qa’enat) earthquake (Mw 7.2): faulting along the Sistan suture zone of eastern Iran. Geophysical Journal International 136: 671– 694, DOI 10.1046/j.1365-246x.1999.00762.x.
  • 9. Bøtter-Jensen L, Bulur E, Duller GAT and Murray AS, 2000. Advances in luminescence instrument systems. Radiation Measurements 32: 523–528, DOI 10.1016/S1350-4487(00)00039-1.
  • 10. Engdahl ER, van der Hilst R and Buland R, 1998. Global teleseismic earthquake relocation with improved travel times and procedures for depth determination. Bulletin of the Seismological Society of America 88: 722–743.
  • 11. Farr TG and Kobrick M, 2000. Shuttle Radar Topography Mission produces a wealth of data. Eos, Transactions American Geophysical Union 81: 583–585, DOI 10.1029/EO081i048p00583.
  • 12. Fattahi M, Walker R, Hollingsworth J, Bahroudi A, Nazari H, Talebian M, Armitage S, and Stokes S, 2006. Holocene slip-rate on the Sabzevar thrust fault, NE Iran, determined using optically stimulated luminescence (OSL). Earth and Planetary Science Letters 245: 673–684, DOI 10.1016/j.epsl.2006.03.027.
  • 13. Fattahi M, Walker RT, Khatib MM, Dolati A and Bahroudi A, 2007. Slip-rate estimate and past earthquakes on the Doruneh fault, eastern Iran. Geophysical Journal International 168: 691–709, DOI 10.1111/j.1365-246X.2006.03248.x.
  • 13. Haghipour A and Amidi M, 1980. Geotectonics of the Ghaenat earthquakes of NE Iran (Nov 14th to Dec. 9. 1979). Bulletin of the Seismological Society of America 70: 1751–1757.
  • 14. Jackson J, 2001. Living with earthquakes: know your faults. Journal of Earthquake Engineering 5(Supplement 001): 5–123, DOI 10.1080/13632460109350530.
  • 15. Jackson J and McKenzie D, 1984. Active tectonics of the Alpine- Himalayan belt between Turkey and Pakistan. Geophysical Journal of the Royal Astronomical Society 77: 185–264, DOI 10.1111/j.1365-246X.1984.tb01931.x.
  • 16. Meyer B and Le Dortz K, 2007. Strike-slip kinematics in Central and Eastern Iran: estimating fault slip-rates averaged over the Holocene. Tectonics 26: TC5009, DOI 10.1029/2006TC002073.
  • 17. Murray AS and Wintle AG, 2000. Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol. Radiation Measurements 32: 57–73, DOI 10.1016/S1350-4487(99)00253-X.
  • 18. Nowroozi AA and Mohajer-Ashjai A, 1980. Faulting of Kurizan and Koli (Qaenat Iran) earthquakes of November 1979: a field report. Iranian Petroleum Institute Bulletin 78: 8–20.
  • 19. Ritz J-F, Brown E, Bourles D, Philip H, Schlupp A, Raisbeck G, Yiou F and Enkhtuvshin B, 1995. Slip rates along active faults estimated with cosmic-ray exposure dates: applications to the Bogd fault, Gobi-Altai, Mongolia. Geology 23: 1019–1022, DOI 10.1130/0091-7613(1995)023<1019:SRAAFE>2.3.CO;2.
  • 20. Rhodes E, 2000. Observations of thermal transfer OSL signals in glacigenic quartz, Radiation Measurements 32: 595–602, DOI 10.1016/S1350-4487(00)00125-6.
  • 21. Tchalenko JS and Ambraseys NN, 1970. Structural analysis of the Dasht-e-Bayaz (Iran) earthquake fractures. Geological Society of America Bulletin 81: 41–60.
  • 22. Tchalenko JS and Berberian M, 1975. Dasht-e-Bayaz fault, Iran: Earthquake and earlier related structures in bed-rock. Geological Society of America Bulletin 86: 703–709.
  • 23. Van der Woerd J, Klinger Y, Sieh K, Tapponnier P, Ryerson FJ and Mériaux AS, 2006. Long-term slip rate of the southern San Andreas fault, from 10Be-26Al surface exposure dating of an offset alluvial fan. Journal of Geophysical Research: Solid Earth: 111: B04407, DOI 10.1029/2004JB003559.
  • 24. Vernant P, Nilforoushan F, Hatzfeld D, Abassi MR, Vigny C, Masson F, Nankali H, Martinod J, Ashtiani A, Bayer R, Tavakoli F and Chery J, 2004. Present-day crustal deformation and plate kinematics in the Middle East constrained by GPS measurements in Iran and northern Oman. Geophysical Journal International 157: 381– 398, DOI 10.1111/j.1365-246X.2004.02222.x.
  • 25. Walker R and Jackson J, 2004. Active tectonics and late Cenozoic strain distribution in central and eastern Iran. Tectonics 23: TC5010, DOI 10.1029/2003TC001529.
  • 26. Walker R, Jackson J and Baker C, 2004. Active faulting and seismicity of the Dasht-e-Bayaz region, eastern Iran. Geophysical Journal International 157: 265–282, DOI 10.1111/j.1365- 2966.2004.02179.x.
  • 27. Walker RT, Bergman EA, Szeliga W and Fielding EJ, 2011. Insights into the 1968–1997 Dasht-e-Bayaz and Zirkuh earthquake sequences, eastern Iran, from calibrated relocations, InSAR and high-resolution satellite imagery. Geophysical Journal International 187: 1577–1603, DOI 10.1111/j.1365-246X.2011.05213.x.
  • 28. Walpersdorf A, Manighetti I, Mousavi Z, Tavakoli F, Vergnolle M, Jadidi A, Hatzfeld D, Aghamohammadi A, Bigot A, Djamour Y, Nankali H and Sedighi M, 2014. Present-day kinematics and fault slip rates in eastern Iran, derived from 11 years of GPS data. Journal of Geophysical Research: Solid Earth 119: 1359–1383, DOI 10.1002/2013JB010620.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-3b906a05-3abd-490b-9915-055734c7d734
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.