Zobrazeno 1 - 10
of 27
pro vyhledávání: '"M. R. Abbassi"'
Publikováno v:
Annals of Geophysics, Vol 46, Iss 5 (2003)
The North Tabriz Fault is a major seismogenic fault in NW Iran. The last damaging earthquakes on this fault occurred in 1721, rupturing the southeastern fault segment, and in 1780, rupturing the northwestern one. The understanding of the seismic beha
Externí odkaz:
https://doaj.org/article/4d43ed33ed2c4a43830da58969d54beb
Autor:
Z. Mohammadi Asl, M. R. Abbassi
Publikováno v:
Open Journal of Earthquake Research. :19-36
Active tectonics in the south part of Alborz Mountain (Iran) has greatly influenced the drainage system and geomorphic expressions. The metropolis of Tehran is located at the southern foothills of the Alborz Mountains at the abrupt topographic bounda
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e71248bdf1f1101990f93c0f287e5d7d
https://doi.org/10.4236/ojer.2019.81002
https://doi.org/10.4236/ojer.2019.81002
Publikováno v:
International Journal of Heat and Fluid Flow. 67:30-41
While large-scale motions are most energetic in the logarithmic region of a high-Reynolds-number turbulent boundary layer, they also have an influence in the inner-region. In this paper we describe an experimental investigation of manipulating the la
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::298af130058f4573cef1c3a941d8d835
https://doi.org/10.1016/j.ijheatfluidflow.2017.05.003
https://doi.org/10.1016/j.ijheatfluidflow.2017.05.003
Publikováno v:
Tectonophysics
Tectonophysics, 2016, 693 (B, SI), pp.304-326. ⟨10.1016/j.tecto.2016.01.030⟩
Tectonophysics, Elsevier, 2016, 693 (B, SI), pp.304-326. ⟨10.1016/j.tecto.2016.01.030⟩
Tectonophysics, 2016, 693 (B, SI), pp.304-326. ⟨10.1016/j.tecto.2016.01.030⟩
Tectonophysics, Elsevier, 2016, 693 (B, SI), pp.304-326. ⟨10.1016/j.tecto.2016.01.030⟩
International audience; Zagros Folded and thrust Belt (ZFTB) is a Cenozoic mountain belt in SSW of Iran and northeast of Arabia that resulted from closure of Neo-Tethys and collision between Arabia passive margin and Central Iran active margin. At th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3edb7e624eb8487e14172e774c6e651a
https://doi.org/10.1016/j.tecto.2016.01.030
https://doi.org/10.1016/j.tecto.2016.01.030
Autor:
Régis Braucher, Khaled Hessami, Esmaeil Shabanian, Olivier Bellier, Yassaman Farbod, Didier Bourlès, M. R. Abbassi, Lucilla Benedetti
Publikováno v:
Tectonics. 35:386-406
The Doruneh Fault System (DFS) is one of the major active strike-slip faults in the Arabia-Eurasia collision zone. Despite its geological activity, no large (M ≥ 6.5) historical or instrumental earthquakes have been recorded along it. To date, the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::51d2c48ea93774ad65c4652e42815b15
https://doi.org/10.1002/2015tc003862
https://doi.org/10.1002/2015tc003862
Autor:
M. R. Abbassi, Ivan Marusic, Dougal T. Squire, Woutijn J. Baars, K. M. Talluru, Nicholas Hutchins
Publikováno v:
Experiments in Fluids. 57
The mean wall shear stress, $$\overline{\tau }_w$$ , is a fundamental variable for characterizing turbulent boundary layers. Ideally, $$\overline{\tau }_w$$ is measured by a direct means and the use of floating elements has long been proposed. Howeve
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a4f96741eacee00cdbebbc9512ea6a9a
https://doi.org/10.1007/s00348-016-2168-y
https://doi.org/10.1007/s00348-016-2168-y
Publikováno v:
Journal of Seismology. 16:233-251
The Doroud segment of the Main Recent Fault (“MRF”) is studied by installing a local seismic network of 35 short-period stations for a period of 13 weeks from 21 June 2007 to 19 September 2007 in the Silakhur region of the Zagros continental coll
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::94a689d1b35438f8ce6d0e79feac7735
https://doi.org/10.1007/s10950-011-9266-3
https://doi.org/10.1007/s10950-011-9266-3
Autor:
M. R. Abbassi, A. Abbassi, Denis Hatzfeld, F. Yamini-Fard, A. Nasrabadi, Mohammad Tatar, Keith Priestley
Publikováno v:
Journal of Geodynamics
Journal of Geodynamics, Elsevier, 2010, 49 (2), pp.68-78. ⟨10.1016/j.jog.2009.09.044⟩
Journal of Geodynamics, Elsevier, 2010, 49 (2), pp.68-78. ⟨10.1016/j.jog.2009.09.044⟩
International audience; Inversion of local earthquake travel times and joint inversion of receiver functions and Rayleigh wave group velocity measurements were used to derive a simple model for the velocity crustal structure beneath the southern edge
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8ab933658d74516484e933a71ebe1af6
https://doi.org/10.1016/j.jog.2009.09.044
https://doi.org/10.1016/j.jog.2009.09.044
Autor:
Vincent Regard, Didier Bourlès, M. R. Abbassi, J. C. Thomas, S.-H. Soleymani, Esmaeil Shabanian, Jean-Luc Mercier, F. Gasse, Olivier Bellier, Régis Braucher
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 242:36-53
A key area for the understanding of the southeastern Iran geodynamics, the Hormoz Strait area, was investigated. Tectonically active, it provides useful sequences of Quaternary deposits whose deposition may have ended either when the climate dried or
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c5e02fae1f5bcd5ef1a17b7c96a808e1
https://doi.org/10.1016/j.palaeo.2006.05.012
https://doi.org/10.1016/j.palaeo.2006.05.012
Publikováno v:
Earthquake Spectra. 21:113-123
The Bam fault zone is a major active fault zone in southeastern Iran. Geomorphic evidence indicates that it has been responsible for repeated faulting events since the late Pleistocene. The 26 December 2003 Bam earthquake was associated with a 14 km
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::12d383bb91dfce08fe23fe44e022d1a5
https://doi.org/10.1193/1.2103167
https://doi.org/10.1193/1.2103167