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THE
EARTHQUAKE AND TSUNAMI OF 13 JANUARY 2007 IN THE KURIL ISLANDS
George Pararas-Carayannis
INTRODUCTION
On 13 January 2007, less than
two months after the great earthquake of 15 November 2006, another
great earthquake occurred off the east coast of the Kuril Islands.
In spite of the quake's large magnitude, only a relatively small
tsunami was generated. A tsunami warning was issued in Japan
and for a large region of the Western Pacific. A watch was issued
for Hawaii, Alaska and the Northwest Pacific. Only a small tsunami
was recorded or observed in Hokkaido, Japan, and at distant locations
in the Pacific.
Date and Time of Occurrence
- The earthquake
occurred on the 13th of January 2007 (04:23:36 UTC). This was
also the local date and time in the epicentral region. The date
and time of the event east of the International Time Zone was
Friday, 12 JAN 2007, 0623 PM (Pacific Standard Time)
Epicenter Location - Latitude: 46.288°N, 154.448°E,
near the Kuril Islands, Russia (USGS NEIC -WDCS-D)
Distances - According to the USGS the earthquake
occurred:
505 km (315 miles) SSW of Severo-Kuril'sk, Kuril Islands, Russia
525 km (325 miles) ENE of Kuril'sk, Kuril Islands
1710 km (1060 miles) NE of TOKYO, Japan
7260 km (4510 miles) NE of MOSCOW, Russia
Magnitude - A Moment magnitude of 8.3 and
a Richter magnitude of 8.1 were initially assigned to this event
by the Pacific Tsunami Warning Center.
Focal Depth - 10 km (6.2 miles).
Aftershocks - There were many aftershocks after
the main quake.
Aftershock Distribution
of the 13 January 2007 Earthquake (USGS graphic).
Geologic Setting
The Kuril volcanic
arc of 56 islands separates the Sea of Okhotsk from the Pacific
Ocean. It extends for 1300km (700mile) from the northern Japanese
island of Hokkaido, Japan to Russia's Kamchatka Peninsula.
Earthquake Focal Mechanism
- The focal mechanism
of this earthquake was moderately well controlled and corresponded
to normal faulting.
Seismicity of the
Northern Japan/Kuril island Region - The Kuril islands and Japan is a region of high
seismic activity and accounts for about 20 per cent of the world's
earthquakes. There was significant seismic activity in the region
since September 2006, which culminated with a great earthquake
in November 15, 2006. Several large earthquakes occurred also
in December 2006. The 13 January event was the second great earthquake
in less than two months.
There have been several earthquakes with magnitude 8.0 or greater
prior to the 17 January 2007 event. Great earthquakes occurred
in 1952 (near Kamchatka), 1963, 1994, and 2003 and in November
15, 2006.
Tectonic
Setting of the Northern Japan/Kuril Island Region
The overall tectonics
of northeast Asia is complicated. Whether the Sea of Okhotsk
and the northern Japanese islands are part of the North American
plate or of a separate Okhotsk microplate that is part of Eurasia
has not been determined. On the Pacific Ocean side, earthquake
slip vectors along the Kuril and Japan trenches are consistent
with either a Pacific-North America or a Pacific-Okhotsk plate
motion. We will assume that the Pacific-North America plate motion
is better supported and that the Okhotsk microplate is part of
North America block.
The Kuril island arc is located between the Kamchatka Peninsula
and the Japanese island of Hokkaido. The Kuril Trench has been
formed by subduction of the Pacific plate under the North American
plate. It extends from the offshore central area of Kamchatka
to Hokkaido.
The tectonics of the Southern Kuril Islands-Northern Hokkaido
region are very different than those along the southern portion
of the Japanese Trench. The South Kuril Islands are part of the
Kuril arc in the Okhotsk plate which has been colliding westward
against the Northeast Japan arc, along the Hidaka Collision Zone
(HCZ), where new continental crust is created by active arc-arc
collision.
Postulated Delamination-wedge-subduction
- Deep seismic reflection
studies (Ito, Kazuka @Abe, 2001) show the lower crust of the
Kuril arc to be delaminated at a depth of about 23 km. As stated,
studies indicate that the upper half (above 23 km) - consisting
of the earth's upper crust and the upper portion of lower crust
of the Kuril arc - is thrusting over the Northeast Japan arc
along the Hidaka Main Thrust (HMT) (Ito, Kazuka @Abe, 2001).
However, the lower half (below 23 km) - consisting of the lower
portion of lower crust and upper mantle material - is descending
downward. Such delamination and horizontal displacement - as
it will be discussed further - may account for the small tsunamis
associated with both the 13 January 2007 and the 15 November
2006 earthquakes.
The postulated Amurian
Microplate (After Wei D. and Seno T. 1998)
As a result of such kinematic processes, the wedge of the Northeast
Japan arc is intruded into the delaminated Kuril arc, as the
Pacific plate is subducting northward beneath both of the above
mentioned structures, thus continuing the arc-arc collision (and
continental crust production). The complex, seismo-tectonic kinematic
process of this region has been named "Delamination-wedge-subduction
system" - which may apply also to other areas where active
arc-arc collision and concurrent subduction take place.
Accordingly, Hokkaido - Japan's northernmost island - extends
northeast into Kuril Islands and is composed of multiple compressed
island arcs. The northern half of Honshu (north of Tokyo), which
is Japan's main island, represents a typical mature island arc,
while the southern half of the island represents also a typical
mature island arc, as the Philippine Sea plate subducts below
the Eurasian plate.
The Postulated Amurian
Microplate - On the
western side, the Sea of Japan/East Sea is a complex basin between
Japan and the Korea/Okhotsk Sea Basin. It represents another
subplate with apparent rotational movement as it interacts against
the Okhotsk microplate, along the inland sea boundary of the
Hidaka Collision Zone (HCZ). Based on recent studies of seismicity
and earthquake focal mechanisms (Wei and Seno, 1998) a postulated
Amurian microplate (AM) has been discriminated from the Eurasian
plate (EU), which includes part of North China, Mongolia and
Siberia and includes the Sea of Japan/East Sea. The postulated
microplate is presumably in contact with the Eurasian plate (EU),
the Okhotsk microplate (OK) and the Phillipine Sea plate (PH).
This Amurian microplate appears to rotate in a counterclockwise
direction, while the Okhotsk microplate appears to rotate in
a clockwise direction. Movement and rotation along the eastern
boundary of this postulated Amurian microplate along the Sea
of Japan/East Sea appears to have been the region where two large
tsunamigenic earthquakes occurred recently (in 1983 and in 1993).
Sakhalin Island, north
of Hokkaido, which separates the Sea of Japan from the Sea of
Okhotsk, is probably the result of transpressional tectonics
along the North America-Eurasia (Okhotsk microplate) boundary.
Epicenters
of Recent Earthquakes in the Region
THE
TSUNAMI OF 13 JANUARY 2007
A relatively small
tsunami was generated by the great earthquake of 13 January 2007,
which was recorded in the immediate region and at distant locations
in the Pacific.
Observations
and Records of Tsunami Wave Activity
JAPAN
Hanasaki - At Hanasaki (Hokkaido, Japan),
at 0605Z the tide gauge registered a 10cm Japan 0.1m/0.3ft amplitude
wave with period of about 28 minutes.
Nemuro - A small tsunami wave of about
40cm (16 inches) was recorded at 9:29 p.m. at the port of Nemuro
on Japan's northernmost island of Hokkaido.
Kushiro - 0.05 m/0.15ft.
Ofunato - 0.06m/0.2 ft
Kamaishi - 0.07cm/0.2ft
Miyako - 0.08cm/ 0.26ft
US and the Pacific
(showing time of first wave arrival)
The Pacific Tsunami
Warning Center reported the following heights and times of first
waves arrival
WAKE 0837Z 0.09M 10MIN
MIDWAY 0911Z 0.18M 10MIN
HILO HAWAII 1148Z 0.12M 14MIN
KAHULUI MAUI 1126Z 0.14M 16MIN
NAWILIWILI KAUAI 1208Z 0.09M 10MIN
ADAK AK 0831Z 0.04M 18MIN
DART NW PAC 0735Z 0.03M 08MIN
SHEMYA AK 0712Z 0.32M 06MIN
Tsunami
Watches, Warnings and Advisories
The Japanese Meteorological
Organization issued a tsunami warning for Japan. The Pacific
Tsunami Warning Center issued a tsunami warning for a broad area
in the Western Pacific Ocean. The Alaska Tsunami Warning System
issued a Tsunami Warning for the Alaska coastal areas from Sand
Point, Alaska to Attu, Alaska. A Tsunami Watch was issued for
British Columbia and Alaska coastal areas from the north tip
of Vancouver I., British Columbia to Sand Point, Alaska. Advisories
were issued only for California, Oregon, Washington, and the
British Columbia.
Tsunami
Generating Area
Based on earthquake
aftershock distribution of the first 24 hours, a tentative estimate
of the tsunami generating area can be obtained. The earthquake
involved a block of about 80x 150 nautical miles.
Recent Earthquakes
and Tsunamis in the Kuril Islands Region
The last great earthquake
in the near the Kuril Islands region had occurred on Wednesday,
November 15, 2006 at 11:14:16 (UTC) (See http://drgeorgepc.com/Tsunami2006Kurils.html).
That earthquake had an epicenter at 46.616°N, 153.224°E
at about 100 nautical miles to the southwest of the 13 January
2007 earthquake. It was a deeper earthquake with hypocenter focal
depth of about 40km/25miles and it was followed by a number of
large aftershocks, some of which exceeded magnitude 6+. Tsunami
watches and warnings were issued for a large section of the Pacific
basin, however only a small tsunami of about 30cm/1.0ft. was
recorded at Hanasaki, and 25cm/0.8ft at Hushiro, Japan At tide
stations at Shemya and at Amchitka, Alaska the tsunami waves
of amplitude 20cm/0.65ft and 8cm/0.25ft were recorded, respectively.
However, the region
remained seismically active. Following the 15 November 2006 great
earthquake several smaller events occurred in the region during
November and December 2006 and in January 2007.
Epicenter of the 1994
Earthquake - Tsunami Generation Area
On Thursday, 7 December
2006 (19:10:21, UTC) a shallow (16 km focal depth) earthquake
(magnitude 6.3) occurred at 46.16N 154.38E. This could have been
a large aftershock of the 15 November 2006 earthquake or an independent
event.
On Tuesday. 26 December 2006, (15:19:46.000 UTC) a shallow focus
(depth 6 miles (10 km)) earthquake (Magnitude: 5.60 Mb) occurred
at 48.4630 N., 154.6940 and it appears to be a precursor event
of the 12 January 2007 great earthquake and approximately 120
nautical miles to the north.
On Saturday, December
30, 2006 (at 12/30/2006 11:16:45.100 UTC) a much deeper earthquake
of unknown magnitude and depth of about 124 miles (200 km)) occurred
at 46.772 N., 152.914
USGS
Graphic of Epicenters and Aftershocks of the November 15, 2006
and the January 13, 2007 Earthquakes
Past Earthquakes
and Tsunamis in the Northern Japan/Kuril Island Region (since
1963)
Review of the historic
record indicates that the following tsunamis were generated in
recent years near Kamtchatka, the Kuril Islands, Northern Japan
and the Sea of Japan:
October 13, 1963
- Kuril Islands (MS=8.1,
I=2.5) - Urup tsunami.
June 16, 1964 - Sea of Japan - (MS=7.5) - Niigata
tsunami (26 dead).
August 11, 1969 - Kuril Islands (MS=7.8, I=2.0)
- Shikotan tsunamis.
November 22, 1969
- Kamchatka (MS=7.7,
I =3.0) - Ozernoy tsunami.
May 25, 1983 - Northern part of Sea of Japan
(MS= 7.7) - (104 dead).
January 15, 1993
- Japan / Hokkaido
(MS=7.8) - Kushiro tsunami, one dead.
July 12, 1993 - Japan Sea (MS=7.7, I=3.0) -
Okushiri tsunami (Maximum Wave Height 30.2m) (more than 200 dead).
October 4, 1994 - South Kuril Islands/Northern
Japan Hokkaido (MS=8.1, I=2.6) - Shikotan tsunami (8 dead in
Kuril Islands).
Dynamics
of Pacific and North American (Okhotsk subplate) Tectonic Plate
Interactions along the Central and Southern Kuril Trench. Possible
Mechanisms Controlling Tsunami Generation.
It would have been
expected that the great earthquake of 13 January 2007 (Mw 8.2)
- as well as the great earthquake (Mw 8.3) of November 15, 2006
would have generated much greater, Pacific-wide tsunamis. Neither
one did. The reason is that the geometry of subduction and tectonic
interactions along volcanic arcs are different than those of
other tectonic collision boundaries - thus unique in tsunami
generation for this particular region. The Pacific plate subduction
along the southern Kuril Trench results in mega continental tension
gashes that are parallel to the direction of convergence (Gelabert
et al. 2001). Also the tension along convergent boundaries results
in steep dipping faults that may be normal, strike-slip or thrust
faults.
To understand the
dynamics of tsunami generation by large earthquakes in this region,
we must look at the geometry of subduction processes and the
mechanics of arc collision that create volcanic arcs such as
the Kuril Islands and extensional back-arc basins - such as the
Sea of Okhotsk.
Subduction and Arc-Arc
Collision - Subduction
along the Japan and Kuril Trenches has been primarily responsible
for many large historical earthquakes and catastrophic tsunamis
on the Pacific side of Northern Japan and the South and Central
Kuril island region (see section above about the tectonic setting).
Most of the tsunamis had destructive near-field effects but limited
far-field impact. The only recent exception may be the 1952 Kamtchatka
earthquake - which occurred much further north - and generated
a tsunami with significant Pacific-wide, impact. The geometry
of subduction appears to be different along the Kamtchatka peninsula
than in the Central and South Kuril Island region.
High Rate of Subduction in the Hokkaido/Kuril Island Region -
The Pacific plate converges into northeastern Asia (the Okhotsk
subplate which is believed to be part of the North American plate,
separated from the Eurasian plate (along the postulated Amurian
microplate?) by the Hidaka Collision Zone (HCZ)). The rate of
tectonic convergence along the Kamchatka, Kuril and Japan trenches
is estimated at about 8-9 m per century - which is a very high.
Hokkaido, which extends northeast into the Kuril Islands, is
composed of multiple compressed island arcs.
In the past two centuries, this fast rate of subduction has triggered
several large earthquakes with magnitudes of up to 8 or more
along the southern Kuril trench, near the island of Hokkaido.
However, these historical earthquakes have ruptured segments
of the trench and of the fore arc region that have been only
in the range of 100-200 km long. Thus, these must be considered
as characteristic of most plate-boundary recent earthquakes for
this volcanic arc region - although, there is geologic evidence
that great earthquakes with multi-segment ruptures have occurred
also in the past which have resulted in extremely large tsunamis.
However, earthquakes with multi-segment ruptures are infrequent
and none is known to have occurred within recorded history.
Ground Movements
and Effects of Rotation -
Apparently, the grinding motion of the North Pacific Plate against
this Okhotsk microplate, results in large earthquakes - such
as those of 1963 and 1994 - but apparently with less vertical
subduction and more rotational movement. For example, the 1994
quake resulted in only about 50 cm of land subsidence but in
extensive lateral movement at Shikotan Island. A greater amount
of subsidence would have been expected, given the earthquake's
large magnitude.
Also, the October 4, 1994 earthquake generated a destructive
local tsunami with runup height of up to 10 meters in the South
Kuril Islands but the far field effects were not significant.
Maximum runup along the coast of Hokkaido, Japan, was 1.8 meters
(at Nemuro). Maximum runup in the Hawaiian islands was 0.8 meters
(at Kahului, Maui).
Crustal Displacements
and Rupture Length Effects -
Tsunamis are generated by relatively shallow crust disturbances
associated with large earthquakes and long ruptures. The extent
of crustal displacements and the length of earthquake ruptures
- as inferred from the distribution of aftershocks - are major
factors in the tsunami generation mechanism and on whether there
will be significant far field tsunami impact.
The crustal area in the Southern Kuril Islands and Northern Hokkaido,
along the northern part of the Japan and Kuril Trenches, appears
to be highly fractured. As described previously, the South Kuril
Islands are part of the Kuril arc in the Okhotsk microplate which
has been also colliding westward against the Northeast Japan
arc, along the Hidaka Collision Zone (HCZ), where new continental
crust is created by active arc-arc collision.
Crustal displacements appear to be occurring along these boundaries
of highly fractured subplates that may not be longer than 200-300
km and probably much less. It appears that these fractured smaller
plates - truncated by oblique asperities - limit the length of
ruptures and extent of crustal displacements, and therefore,
the amount of energy imparted for tsunami generation.
Multi-segment ruptures
- The majority of
earthquakes in the central and southern Kuril islands and the
Hokkaido region - even those of large magnitude - usually involve
single segment ruptures along the Kuril trench - segments truncated
by oblique asperities. Such earthquakes with relatively short
single segment ruptures do not generate very large Pacific-wide
tsunamis. Most of the destructive effects of the tsunamis are
local in the Kuril Islands and northern Hokkaido region.
Recent historical
earthquakes in the region have been associated with single segment
ruptures. The Kuril Island Earthquakes of 13 October 1963 (Ms
= 8.1; Mw = 8.5) the 19 October 1963 (Ms = 7.2; Mw = 7.8) and
the October 4, 1994, were such single segment events. They did
generate destructive local tsunamis but the far field effects
were not significant. However, what may be significant is that
these two major earthquakes occurred a week apart in the same
region. Also, that the second earthquake on 19 October 1963 occurred
somewhat east of the 13 October 1963 event.
The January 13, 2007 earthquake - like those of November 15,
2006, of 1994 and of 1963 - occurred on the Pacific side boundary
of the smaller tectonic subplate which includes the Sea of Okhotsk
and possibly a portion of the northern part of the Sea of Japan
/ East Sea (Pararas-Carayannis, 1995). It appears that the pair
of earthquakes of November 15, 2006 and January 13, 2007, which
occurred in less than two months in the same general region,
was similar to the pair of events that occurred in 1963. The
January 13, 2007 event occurred somewhat east of the previous
event. One possible explanation for the occurrence of great earthquakes
in the same region within the short time frame may be crustal
delamination processes and the mechanics of volcanic arc collision
that create extensional back-arc basins (such as the Sea of Okhotsk).
Crustal Delamination,
Transpressional Effects and Back Arc Migration - If crustal delamination occurs
below 23 km as postulated (Ito, Kazuka @Abe, 2001) such process
would also account for the smaller tsunami as there is less vertical
movement of crustal material below 23 km and more lateral movement
above. As it was pointed out, the 1994 earthquake resulted in
only about 50 cm of land subsidence but extensive lateral movement
at Shikotan Island.
The earthquake of
November 15, 2006 had a focal depth of 28.5 km. Given the short
rupture of the earthquake and the focal depth below the delamination
boundary of 23 km this would explain why no major tsunami was
generated that had significant far field effects. Most of the
earthquake's energy went into lateral transpressional movement
along this boundary of subduction - filling the void caused by
Kuril arc migration by pushing the subducting (and denser) plate
horizontally towards the extensional basin (Sea of Okhotsk) -
as in 1994. Such migration would also account for the close sequence
of a pair of the great earthquakes, the first occurring on November
15, 2006 and the second occurring in January 13, 2007- slightly
to the east and shallower.
Can the
Kuril Island/Hokkaido region generate tsunamis that can have
significant far field destructive effects (Pacific-wide)?
Based on the stratigraphic distribution of deposits of historical
tsunamis found in Japan, it has been inferred that unusually
large tsunamis have occurred in this region. The significant
runup of these tsunamis leads to the conclusion that they were
generated by earthquakes which ruptured two or more segments
along the Japan Trench or along the central and southern Kuril
Trench. Such events are extremely rare but may occur every 500
years or more and could have significant regional and far field
impact.
REFERENCES
AND FURTHER READING
The following are
selected references for further reading on the kinematics of
tectonic interactions along the Japanese and Kuril Island arcs
which historically have produced numerous destructive tsunamis.
GELABERT, B., SABAT, F., RODRIGUEZ-PEREA, A. , and FORNS, J.,
2001. ON THE ORIGIN OF ARCUATE FOLDED BELTS AND BACK-ARC BASINS,
GSA Annual Meeting, November 5-8, 2001 Session No. 137
Iida, K., D. C. Cox,
and G. Pararas-Carayannis (1967). Preliminary catalog of tsunamis
occurring in the Pacific Ocean, Hawaii Institute of Geophysics
Report 67-10, Univ. of Hawaii, 274pp.1962.
Nakamura, K., V. Renard, J. Angelier, J. Azema, J. Bourgois,
C. Deplus, K. Fujioka, Y. Hamano, P. Huchon, H. Kinoshita, P.
Labaume, Y. Ogawa, T. Seno, A. Takeuchi, M. Tanahashi, A. Uchiyama,
and J. L. Vigneresse. Oblique and near collision subduction,
Sagami and Suruga troughs -Preliminary results of French-Japanese
1984 KAIKO cruise, leg 2 Earth Planet. Sci. Lett. 83 229-242
1987.
Ogawa, Y., T. Seno, H. Akiyoshi, H. Tokuyama, K. Fujioka, and
H. Taniguchi, 1989. Structure and development of the Sagami Trough
and off-Boso triple junction. Tectonophysics 160 135-150, 1989
Kawakatsu, H., and T. Seno, 1983. Triple seismic zone and the
regional variation of seismicity along the northern Honshu arc.
J. Geophys. Res. 88 4215-4230 1983 __
Pararas-Carayannis G. 1983, The Earthquake and Tsunami of 26
May 1983 in the Sea of Japan
http://drgeorgepc.com/Tsunami1983Japan.html
Pararas-Carayannis
G. 1994, The Earthquake and Tsunami of The Earthquake and Tsunami
of October 4, 1994 in the Kuril Islands
http://drgeorgepc.com/Tsunami1994RussiaKurils.html
Pararas-Carayannis
G. The November 4,1952 Kamchatka Earthquake and Tsunami
http://drgeorgepc.com/Tsunami1952.html
Seno, T. and D. G.
Gonzalez. 1987. Faulting caused by earthquakes beneath the outer
slope of the Japan Trench. J. Phys. Earth 35 381-407 1987
Seno, T. 1999. Is northern Honshu a microplate? Tectonophysics
115 177-196 1985 __Seno, T. Syntheses of the regional stress
fields of the Japanese islands The Island Arc 8 66-79 1999
Seno, T., and Y. Yamanaka. 1998. Arc stresses determined by slabs:
Implications for mechanisms of back-arc spreading Geopys. Res.
Lett. 25 3227-3230 1998
Seno, T., and Y. Yamanaka. 1996. Double seismic zones, compressional
deep trench - outer rise events and superplumes in Subduction
Top to Bottom, edited by G. E. Bebout, D. W. Scholl, S. H. Kirby,
and J. P. Platt Geophys. Monogr. 96 347-355 1996
Seno, T., and B. Pongsawat, 1981. A triple-planed structure of
seismicity and earthquake mechanisms at the subduction zone off
Miyagi Prefecture, northern Honshu, Japan Earth Planet. Sci.
Lett. 55 25-36, 1981
Seno, T., and G. C. Kroeger. 1983 A reexamination of earthquakes
previously thought to have occurred within the slab between the
trench axis and double seismic zone, northern Honshu J. Phys.
Earth 31 195-216 , 1983
Seno, T., and T. Takano, 1989. Seismotectonics at the trench-trench-trench
triple junction off central Honshu Pure Appl. Geophys. 129 27-40,
1989
Seno, T., T. Sakurai, and S. Stein, 1996. Can the Okhotsk plate
be discriminated from the North American plate? J. Geophys. Res.
101 11305-11315, 1996
Seno, T. 1999. Earthquake Research Institute, University of Tokyo,
Bunkyo-ku, Tokyo 113-0032, Japan The Island Arc, 8, 66-79, 1999
Tanioka, Y., and K. Satake (1996). Fault parameters of the 1896
Sanriku tsunami earthquake estimated from tsunami numerical modeling,
Geophys. Res. Letters, 23-13,1549-1552.
Walker Daniel A.,
2005. OCEAN-WIDE TSUNAMIS, MAGNITUDE THRESHOLDS, AND 1946 TYPE
EVENTS. Science of Tsunami Hazards, Vol. 23, No. 2, page 4 (2005)
Watanabe, T., T. Koyaguchi,
and T. Seno. Tectonics stress controls on ascent and emplacement
of magmas J. Volcanol. Geotherm. Res. 91 65-78, 1999
Wei D. and Seno T.
1998. Determination of the Amurian Plate Motion. In Mantle Dynamics
and Plate Interactions in East Asia, edited by Martin Flower
, GeoDynamics Series., AGU, 1998
BIBLIOGRAPHY
ON THE SEISMOTECTONICS OF THE KURIL ISLAND/HOKKAIDO REGION
Aver£yanova V. N. (1975).
Depth seismotectonics
of island arcs. Moscow, 1975,
in Russian.
Belyaevsky N. A., Rodnikov A. G. (1972). Crustal structure of the island arcs and Far
Eastern Seas. Article 1. Island Arcs.
International Geology Review, v. 14, No. 2, 1972.
Bikenina S. K., Anosov G. I., Argentov V. V. and Sergeev
K. F. (1987). The
Earth crust structure of the southern part of Okhotsk Sea according
to seismic data. Nauka, Moscow,
1987, 87 pp., in Russian.
Bogdanov N. A. (1988). Deep
basin tectonics of margin seas. Nedra,
Moscow, 1988, 221 pp., in
Russian.
Boldyrev S. A., Gainanov A. G. and Stroev P. A. (1993). Density inhomogeneities of the
lithosphere and dynamics of the North-West Pacific active belt. In: Marine Gravity Investigations (P.A.Stroev,
ed.). National Geophysical Committee, Moscow, 1993,
106-119, in Russian with English abstract.
Burmin V. Yu., Savrina L. A. and Kugaenko Yu. V. (1992). Velocity section of the upper
mantle of the Okhotsk Sea region with using deep foci earthquakes
data. Volcanology and Seismology,
No. 2, 1992, 64-75, in Russian.
Deep seismic
sounding of the Earth crust of Sakhalin-Hokkaido seaside zone.(1971)
Eds. S. M. Zverev and Y. V. Tulina. Nauka, Moscow, 1971,
286 pp., in Russian.
Fedotov S. A., Chernyshev S. D., Chernysheva G. V. and Vikulin
A. V. Determination
of the boundaries of earthquakes sources with M>=7 3/4, peculiarities
of seismic cycle and long-term seismic prediction for the Kurile-Kamchatka
arc. Volcanology and Seismology,
No. 6, 1980, 52-67, In Russian.
Frolova T. I., Perchuk L. L. and Burikova I. A. Magmatism and transformation
of the Earth crust of the active margins.
Nauka, Moscow, 1989, 261 pp., in Russian.
Geology-geophysical
atlas of the Kuril-Kamchatka island system. Deep structure of
the North-East Japan Arc and its relationship to seismic and
volcanic activity. Eds. K.F.Sergeev
and M.L.Krasny. Institute of Marine Geology and Geophysics,
1987, 40 pp.
Hilde T. W. C., Uyeda S. and Kroenke L. Evolution of the Western Pacific and its Margin.
Tectonophysics, v. 38, No. 1/2,
1977, 145-165.
Honza, E., and K. Tamaki, The Bonin Arc, in The Ocean Basins
and Margins, edited by A. E. M. Nairn
et al., Vol. 7, pp. 459-502, Plenum Co., New York, 1985.
Isezaki N., Yosui M. and Uyeda S. Possible spreading centers in the Japan Sea.
In: Geological-geophysical researches of the transition zone
from the Asiatic continent to the Pacific Ocean. Sov. radio,
Moscow, 1976, 72-80.
Jolivet, L., and K. Tamaki, Neogene kinematics in the Japan
Sea region and volcanic activity of the NE-Japan arc, in Proc. ODP, Sci. Results, edited by Tamaki,
K., Suyehiro, K., Allan, J., McWilliams, M., et al., Vol. 127/128,
Pt.2, pp. 1311-1331, College Station, TX (Ocean Drilling TAMU),
1992.
Jolivet, L., K. Tamaki, and M. Fournier, Japan Sea, opening history and mechanism: a synthesis, J. Geophys. Res., 99, 22237-22259, 1994.
Khain V. E., Lomize M. G. Geotectonics
with elements of geodynamics. Moscow
State University, 1995, 480 pp, in Russian.
Kimura, G., and K. Tamaki, Tectonic framework of the Kuril
Arc since its initiation, in Formation
of Active Ocean Margins, edited by N. Nasu et al., pp. 641-676,
Terrapub., Tokyo, 1985.
Kimura, G., and K. Tamaki, Collision, rotation, and back-arc
spreading: the case of the Okhotsk and Japan Seas, Tectonics, 5, 389-401, 1986.
Kobayashi, K., M. Nakanishi, K. Tamaki,
and Y. Ogawa, Outer
slope faulting associated with the western Kuril and Japan trenches, Geophys. J. Int., 134, 356-372, 1998.
Krasny M. L. Geophysical
fields and deep structure of the Okhotsk-Kuril region.
Dalnevost. Otdel. Akad. Nauk USSR,
Vladivostok, 1990, 161 pp.,
in Russian.
Lyapishev A. M., Sychev P. M. and Semenov V. Yu. Structure of electroconductivity
of the upper mantle of Kuril Basin of Okhotsk Sea. Tihookeanskaya Geologia, No. 4, 1987,
45-50, in Russian.
Oscorbin L. S. Sakhalin seismicity. In: Seismic Zoning of Sakhalin
(S.L.Solov'ev, ed.).
SakhKNII, Vladivostok, 1977, in Russian.
Pisciotto, K., K. Tamaki et al., Exploring the Japan Sea, Geotimes, 1989.
Rodnikov A. G. About
tectonics of Iturup Island. Vestnik
MGU, Geology, No. 6, 1968,
92-94, in Russian.
Rodnikov A. G. Island
arcs of the western part of the Pacific Ocean.
Nauka, Moscow, 1979, 152 pp., in Russian.
Rodnikov A. G., Khain V. E. On the trend in evolution of the Earth's crust
in the north-western part of the Pacific mobile belt. In: Island
Arcs and Marginal Sea (S.Asano and
G.Udintsev, eds.). Tokai University Press, 1971, 65-76,
in Japanese.
Rodnikov A. G., Rodnikova R. D. The Japan - Sakhalin Island Arc. Nauka, Moscow, 1974, 74 pp., in Russian.
Rodnikov A. G., Rodkin M. V., Ermakov B. V. et al. The Okhotsk Sea Geotraverse.
27th
General Assembly IASPEI, Wellington, NZ., 1994, S8.51.
Rogozhin E. A.
Focal mechanism of the Neftegorsk (Sakhalin) earthquake of May
27(28), 1995. Geotectonics, No.
2, 1996, 45-53, in Russian.
Semenov R. M., Pavlenov V. A. and Charahinov V. V. Catastrophic earthquake at the
north Sakhalin (short seismogeological characteristic). Dokl. Akad. Nauk SSSR, v. 351, No. 4, 1996,
535-538, in Russian.
Semenova G. I., Zorina Yu. G., Kunin N. Ya. and Rodnikov
A. G. Upper mantle
zoning of the Pacific with using geophysical investigation data. In: Structure and Dynamic of Transition Zones
from Continent to Ocean. (V.V.Belousov, M.E.Artem'ev and A.G.Rodnikov,
eds.). Nauka, Moscow, 1986, 57-65, in Russian.
Sergeev K. F. Tectonics
of Kuril island system. Nauka,
Moscow, 1976, 239 pp., in Russian.
Snegovskoi S. S. Reflection
method investigations and tectonics of the southern part of Okhotsk
Sea and adjacent frontier area of the Pacific.
Nauka, Novosibirsk, 1974, 86 pp., in Russian.
Soloviev S. L., Oscorbin L. S. and Ferchev M. D. Earthquakes at Sakhalin. Nauka, Moscow, 1967, 178 pp., in Russian.
Structure of
the Okhotsk Sea floor. Ed. V. V.
Beloussov, Nauka, Moscow, 1981, 176 pp., in Russian.
Structure of
the floor of the north-western Pacific.
Eds. Yu. M. Pushcharovsky and Yu. P. Neprochnov. Nauka, Moscow,
1984, 231 pp., in Russian.
Structure and
dynamics of the lithosphere and asthenosphere of the Okhotsk
Sea region. Eds. A. G. Rodnikov,
I. K. Tuezov and V. V. Charahinov. National Geophysical Committee,
Nauka, Moscow, 1996, 340 pp., in Russian.
Sychev P. M. Deep
and surface tectonics processes of the north-western Pacific
mobil belt. Nauka, Moscow, 1979,
208 pp., in Russian.
Tamaki, K., Two modes of back-arc spreading, Geology, 13, 475-478, 1985.
Tamaki, K., and E. Honza, Incipient
subduction and obduction along the eastern margin of the Japan
Sea, Tectonophys., 119, 381-406,
1985.
Tamaki, K., Geological structure of the Japan Sea and its
tectonic implications, Bull. Geol.
Surv. Japan, 39, 269-365, 1988.
Tamaki, K., and E. Honza, Global tectonics and formation
of marginal basins: a role of the western Pacific, Episodes, 14, 224-230, 1991.
Tamaki, K., Opening tectonics of the Japan Sea, in Backarc
Basins: Tectonics and Magmatism,
edited by B. Taylor, pp. 407-420, Plenum Press, New York, 1995.
Tamaki, K., and I. I. Bersenev, Morphology of the Japan Sea,
in Gelogy and Geophysics of the Japan Sea (Japan-USSR Monograph
Series, Vol 1), edited by N. Isezaki, I. I. Bersenev, K. Tamaki,
B. Ya. Karp, and E. P. Lelikov, pp. 35-39, Terra Scientific Publishing
Company (Terrapub), 1996.
Tamaki, K., and N. Isezaki, Tectonic
synthesis of the Japan Sea based
on the collaboration of the Japan-USSR Monograph Project, in
Gelogy and Geophysics of the Japan Sea (Japan-USSR Monograph
Series, Vol 1), edited by N. Isezaki, I. I. Bersenev, K. Tamaki,
B. Ya. Karp, and E. P. Lelikov, pp. 483-487, Terra Scientific
Publishing Company (Terrapub), 1996.
Tarakanov R. Z. Structure
of the focal zone of the Kuril-Kamchatka island arc.
In: The Earth Crust of the Island Arc and Far East Seas (N. A.
Beliaevsky, A. G. Gainanov and A. G. Rodnikov, eds.), Nauka,
Moscow, 1972, 215-234, in Russian.
Tectonics of
the north-western Pacific Ocean.
Ed. A. G. Rodnikov. Nauka, Moscow, 1983, 120 pp., in
Russian.
Tuezov I. K. The
lithosphere of transition zone from Asia to Pacific. Nauka, Novosibirsk, 1975, 232 pp.,
in Russian.
Vasilenko N. F., Bogdanova E. D. Horizontal movements of the Earth surface in
zone of the central Sakhalin deep fault.
Pacific Geology, No. 3, 1986, 45-49, in Russian.
Vasiliev B. I. The
main features of the geological structure of North-West part
of Pacific. Vladivostok, 1988,
192 pp., in Russian.
Zlobin T. K. Lithosphere
sructure in the region of the Iturup Island from seismic data.
Pacific Geology, No. 3, 1989, 33-41, in Russian.
Zlobin T. K., Zlobina L. M. The Earth crust structure of the Kuril Island
system. Pacific Geology, No. 6,
1991, 24-35, in Russian.
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