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N. Ambraseys (1963)
The Buyin-Zara (Iran) earthquake of September, 1962 a field reportBulletin of the Seismological Society of America, 53
T. Taymaz, J. Jackson, R. Westaway (1990)
Earthquake mechanisms in the Hellenic Trench near CreteGeophysical Journal International, 102
(1968)
citation_author=Amursski G.I.; citation_author=Tiunov K.V.; citation_author=Khrikov B.A.; citation_author=Shlezinger A.E.; citation_publisher=Akademii Nauk SSSR, Moscow; Structure and tectonic position of the Great Balkhan
H. Lyon‐Caen, P. Molnar (1985)
Gravity anomalies, flexure of the Indian Plate, and the structure, support and evolution of the Himalaya and Ganga BasinTectonics, 4
(1981)
Late Cenozoic plate tectonics of the Black Sea-Caspian region
R. Mccaffrey, G. Abers (1988)
SYN3: A Program for Inversion of Teleseismic Body Wave Forms on Microcomputers
(1979)
Geodynamics, in Okeanologiya.Geofizika Okeanshogo Dna. Nauka, Moscow, 2
Kenneth Smith, J. Brune, K. Priestley (1991)
The seismic spectrum, radiated energy, and the Savage and Wood inequality for complex earthquakesTectonophysics, 188
Ali Nowroozi (1973)
A reply to discussion on “Focal mechanism of earthquakes in Persia, Turkey, West Pakistan, and Afghanistan and plate tectonics of the Middle East”Bulletin of the Seismological Society of America
(1981)
Structure of the Sedimentary Cover of the Black Sea Basin, in
W. Futterman (1962)
Dispersive body wavesJournal of Geophysical Research, 67
J. Fredrich, R. Mccaffrey, D. Denham (1988)
Source Parameters of Seven Large Australian Earthquakes Determined By Body Waveform InversionGeophysical Journal International, 95
(1994)
Aftershocks of the 1990 western Iran (MW 7.3) earthquakeBull. seism. Soc. Am.
H. Lyon‐Caen, R. Armijo, J. Drakopoulos, J. Baskoutass, N. Delibassis, R. Gaulon, V. Kouskouna, J. Latoussakis, K. Makropoulos, P. Papadimitriou, D. Papanastassiou, G. Pedotti (1988)
The 1986 Kalamata (South Peloponnesus) Earthquake: Detailed study of a normal fault, evidences for east-west extension in the Hellenic ArcJournal of Geophysical Research, 93
N. Lek, L. John (1984)
Determination of earthquake source parameters from inversion of body waves
M. Berberian, S. Arshadi (1976)
ON THE EVIDENCE OF THE YOUNGEST ACTIVITY OF THE NORTH TABRIZ FAULT AND THE SEISMICITY OF TABRIZ CITY
I. Rezanov, S. Chamo (1969)
Reasons for absence of a 'granitic' layer in basins of the South Caspian and Black Sea typeCanadian Journal of Earth Sciences, 6
(1972)
Focal mechanism of earthquakes in Persia, Turkey, West Pakistan and Afghanistan and plate tectonics of the Middle EastBull. seism. Soc. Am., 62
M. Zoback, M. Zoback, V. Mount, J. Suppe, J. Eaton, J. Healy, D. Oppenheimer, P. Reasenberg, L. Jones, C. Raleigh, I. Wong, O. Scotti, C. Wentworth (1987)
New Evidence on the State of Stress of the San Andreas Fault SystemScience, 238
P. Molnar (1992)
Chapter 18 Brace-Goetze Strength Profiles, The Partitioning of Strike-slip and Thrust Faulting at Zones of Oblique Convergence, and the Stress-Heat Flow Paradox of the San Andreas FaultInternational Geophysics, 51
N. Ambraseys, C. Melville (1982)
A history of Persian earthquakes
R. Mccaffrey, J. Nábělek (1987)
Earthquakes, gravity, and the origin of the Bali Basin: An example of a Nascent Continental Fold-and-Thrust BeltJournal of Geophysical Research, 92
M. Berberian, G. King (1981)
Towards a paleogeography and tectonic evolution of Iran: ReplyCanadian Journal of Earth Sciences, 18
K. Kadinsky-Cade, M. Barazangi, J. Oliver, B. Isacks (1981)
Lateral variations of high-frequency seismic wave propagation at regional distances across the Turkish and Iranian plateausJournal of Geophysical Research, 86
(1964)
citation_author=Rustanovich D.N.; citation_author=Shinakova E.I.; citation_publisher=Izvestiya Akademii Nauk SSSR, Seriya Geofizika; Some results of a study of the Askhabad earthquake of 1948
S. Adamia, M. Lordkipanidze, G. Zakariadze (1977)
Evolution of an active continental margin as exemplified by the Alpine history of the CaucasusTectonophysics, 40
J. Tchalenko (1975)
Seismicity and structure of the Kopet Dagh (Iran, U. S. S. R.)Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 278
J. Tchalenko, J. Braud (1974)
Seismicity and structure of the Zagros (Iran): the Main Recent Fault between 33 and 35° NPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 277
P. Molnar, Hélène Lyon-Caent (1989)
Fault plane solutions of earthquakes and active tectonics of the Tibetan Plateau and its marginsGeophysical Journal International, 99
(1962)
Main characteristics of deep waves registered by deep seismic sounding in the central part of the Caspian Sea, Deep Sounding of the Earths Crust in the USSR, MoscowGosloptekhizdat
M. Berberian (1983)
The southern Caspian: A compressional depression floored by a trapped, modified oceanic crust"Canadian Journal of Earth Sciences, 20
J. Jackson, D. McKenzie (1984)
Active tectonics of the Alpine—Himalayan Belt between western Turkey and PakistanGeophysical Journal International, 77
(1989)
The Caspian earthquake of March 6, Earthquakes in the U.S.S.R. in 1986Akademii Nauk SSSR, 58
J. Jackson, P. Molnar (1990)
Active faulting and block rotations in the Western Transverse Ranges, CaliforniaJournal of Geophysical Research, 95
(1968)
History of the geotectonic development of the depression of the Caspian SeaIzvestiya Akademii Nauk SSSR, Seriya Geologicheskaya, 10
(1972)
Formation history of the deep Black Sea basin as compared with deep basins of the MediterraneanGeotektonika, 5
T. Fitch (1972)
Plate convergence, transcurrent faults, and internal deformation adjacent to Southeast Asia and the western PacificJournal of Geophysical Research, 77
(1977)
A reconnaissance of the seismicity and tectonics at the northern border of the Arabian plateRev. Geogr. Phys. Geol. Dyn, 19
E.Sh. Shikalibeily, B. Grigoriants (1980)
Principal features of the crustal structure of the south-caspian basin and the conditions of its formationTectonophysics, 69
J. Jackson, T. Fitch (1979)
Seismotectonic implications of relocated aftershock sequences in Iran and TurkeyGeophysical Journal International, 57
L. Zonenshain, X. Pichon (1986)
Deep basins of the Black Sea and Caspian Sea as remnants of Mesozoic back-arc basinsTectonophysics, 123
Y. Neprochnov (1968)
Structure of the earth's crust of epi-continental seas: Caspian, Black, and MediterraneanCanadian Journal of Earth Sciences, 5
(1970)
citation_author=Mdlovitsky Y.P.; citation_author=Levin L.E.; citation_author=Milashin A.P.; citation_author=Zorina Y.G.; citation_publisher=Nedra, Moscow; Gruppa Youshnykh Morey. Tektonika I Neftegazonosnost Okrunnykh I Vnutrennykh Morey SSSR
(1986)
Deep basins of the Black Sea and Caspian Sea as remnants of Mesozoic back-arc basins, in Evolution of the TethysTectonophysics, 123
J. Jackson, T. Fitch (1981)
Basement faulting and the focal depths of the larger earthquakes in the Zagros mountains (Iran)Geophysical Journal International, 64
(1977)
The Black Sea: A marginal basin, geophysical and geological data, in
(1980)
New data on the time of formation of the Black Sea deep basinDokl. Akad. Nauk SSSR, 252
V. Mount, J. Suppe (1987)
State of stress near the San Andreas fault: Implications for wrench tectonicsGeology, 15
(1988)
The 1986 Kalamata (S. Peloponessos) earthquake: Detailed study of a normal fault and tectonic implicationsJ. geophys. Res., 93
T. Heaton, H. Kanamori (1984)
Seismic potential associated with subduction in the northwestern United StatesBulletin of the Seismological Society of America, 74
(1982)
citation_author=Ambraseys N.N.; citation_author=Melville C.P.; citation_publisher=Cambridge University Press, Cambridge; A History of Persian Earthquakes
D. McKenzie, J. Jackson (1983)
The relationship between strain rates, crustal thickening, palaeomagnetism, finite strain and fault movements within a deforming zoneEarth and Planetary Science Letters, 65
(1988)
citation_author=McCaffrey R.; citation_author=Abers G.; citation_publisher=Hanscom Air Force Base, MA; SYN3: A program for inversion of teleseismic body wave forms on microcomputers
M. Berberian, M. Qorashi, J. Jackson, K. Priestley, T. Wallace (1992)
The Rudbar-Tarom earthquake of 20 June 1990 in NW Persia: Preliminary field and seismological observations, and its tectonic significanceBulletin of the Seismological Society of America, 82
(1972)
citation_author=Fedynsky V.V.; citation_author=Fomenko K.E.; citation_author=Garkalenkov J.A.; citation_author=Goncharov V.P.; citation_author=Khrychem B.A.; citation_author=Malovitsky Y.P.; citation_author=Milashin A.P.; citation_author=Neprochnov Y.P.; citation_author=Ushakov S.A.; citation_publisher=International Geological Congress, Montreal, P.Q. Section; The Earth's crust of the inland seas and continental depressions of the west Tethys region, 3
J. Jackson (1992)
Partitioning of strike‐slip and convergent motion between Eurasia and Arabia in eastern Turkey and the CaucasusJournal of Geophysical Research, 97
T. Taymaz, J. Jackson, D. McKenzie (1991)
Active tectonics of the north and central Aegean SeaGeophysical Journal International, 106
Summary The south Caspian Basin is a relatively aseismic block within the Alpine-Himalayan Belt, but is surrounded by zones of high seismicity. We used the focal mechanisms of 16 earthquakes whose source parameters we determined from inversion of body waves and the mechanisms of 15 other earthquakes to determine the style of faulting in the seismic belts surrounding the south Caspian Basin. Earthquakes beneath the Talesh Mountains of north-west Iran and immediately off-shore in the south-west Caspian Sea have shallow thrust mechanisms, showing that the continental crust of north-west Iran is overthrusting the ‘oceanic-like’ crust of the south Caspian Basin. Earthquakes south of the Caspian Sea in northern Iran show a mixture of focal mechanisms. Both high-angle reverse faulting and left-lateral strike-slip faulting mechanisms are observed in the high Alborz Mountains. Farther south, on the edge of the central Iran plateau, oblique left-lateral reverse mechanisms are observed. It appears that the NE direction of shortening between central Iran and the south Caspian Basin is partitioned into pure left-lateral strike-slip and thrusting in the WNW-trending high Alborz, but is accommodated by oblique faulting in lower elevations. Earthquakes in the Kopet Dag Mountains east of the Caspian Sea also show a mixture of high-angle reverse and strike-slip faulting mechanisms and may be another example of the partitioning of oblique slip into strike slip and thrust motion. Normal faulting mechanisms at centroid depths of 35–50 km dominate in the belt of seismicity that extends across the central Caspian Sea. The significance of the normal faulting earthquakes is enigmatic. It is improbable that these events represent the motion between the southern Caspian Basin and Eurasia for they imply a sense of motion that is incompatible with the observed topography and folding in the sediments. Two shallow earthquakes at about 12 km depth in this belt, one a small event and the other a large second subevent of a multiple earthquake, have thrusting mechanisms suggesting that shortening occurs as the continental crust of the northern Caspian Sea is thrust over the ‘oceanic-like’ crust of the southern Caspian Basin. Shortening is also suggested by the orientations of folds in the sedimentary cover south of the central Caspian Sea seismic belt. We suggest that this shortening does indeed represent a NNE motion of the Caspian Sea relative to Eurasia, but that the motion is slow and has not produced many earthquakes. The deeper, normal-faulting events may be related to bending or down-dip extension of the incipient subducted slab. If the motion of the Caspian Sea relative to Eurasia is indeed slow, then the motion in the Alborz between central Iran and the south Caspian Basin will be almost the same as that between Iran and Eurasia, as has previously been assumed. The combined effect of the overthrusting of the south Caspian Basin by the Talesh-Alborz Mountains in the south, and by the continental crust of the northern Caspian Sea in the north will lead to the eventual destruction of the south Caspian Basin and the possible formation of an intermediate-depth, dipping seismic zone within the continental interior, similar to that presently observed in the Hindu Kush. Caspian Basin, earthquake-source mechanism, faulting, Iran, tectonics References Adamia S.A. Lordkipanidze M.B. Zakariadze G.S. , 1977 . Evolution of an active continental margin as exemplified by the Alpine history of the Caucasus Tectonophysics , 40 , 183 – 199 . Google Scholar Crossref Search ADS WorldCat Ambraseys N.N. , 1963 . The Buyin-Zara (Iran) earthquake of September, 1962: a field report Bull. seism. Soc. Am. , 53 , 705 – 740 . OpenURL Placeholder Text WorldCat Ambraseys N.N. Melville C.P. , 1982 . A History of Persian Earthquakes , Cambridge University Press , Cambridge . 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Geophysical Journal International – Oxford University Press
Published: Jul 1, 1994
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