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I. MEGA SS
ANATOLIA (Eastern Turkey),
Ìs≥7.8. After
catastrophic earthquake in Japan we have considered mega-earthquake
possibility in SS
Anatoly in the east of Turkey with magnitude Ì≥7.8.
In Communications
from
March 2,
2010 and on
March 9,
2010 it was told
about a critical situation in the east of Turkey. Forecasts of strong
earthquake there became on the basis of
SS
Armenian Uplands with Ìs≥6.6. Actually,
preparation of strong earthquake which we predicted and expected in
SS
Armenian Uplands in 2010 has outgrown in preparation mega earthquakes which
now we will predict in Mega SS
Anatoly Ìs≥7.8. Mega
SS
Anatoly treats the category of
badly defined. Here were two
earthquakes Ararat in
1840 and Erzincan
1939 on the North Anatolian
Fault
(NAF).
As a result we have one authentic come to the end seismic cycle. In Tab.1
and in Fig.1 values and a fragment of a track preparation of
catastrophic earthquake with Ì=7.9 on the beginning of June, 2011 are
resulted. As the system is badly defined, we have calculated
attractor
on points of earthquakes 1903 and 1939 (a yellow line on a Fig.1):
K=0.809W+1.049
1903-1939
(1)
For May 2011 K=16.792. Substituting in
eq.(1)
we will find critical value of entropy Wk=19.449. At seismic calm entropy
will reach this value
by the end of 2012. Strong earthquake with Ì=7.9
is already prepared. The rupture model at expected
catastrophe
which we resulted in the form of animation
NAF
move01, remains in force.
|
|
Date |
Fi |
La |
K |
W |
Ks |
Ms |
Pê |
Pw |
P |
Place |
|
1 |
1737.10.17 |
51.10 | 158.00 |
- |
- |
8.6? | S Kamchatka | ||||
|
2 |
1841.05.17 |
52.50 | 159.50 |
- |
- |
8.4? | SE Kamchatka | ||||
|
3 |
1952.11.04 |
52.30 |
161.00 |
17.599 |
20.248 |
18.0 |
9.0 |
SE Kamchatka | |||
|
4 |
2011.05.30 |
|
|
17.449 |
20.047 |
92.78% | 80.70% | 74.98% |
|
|
Date |
Fi |
La |
K |
W |
Ks |
Ms |
Pê |
Pw |
P |
Place |
|
1 |
1907.04.15 |
16.70 |
99.20W |
- |
- |
17.2 | 8.4 | Guerrero Coast | |||
|
2 |
1932.06.03 |
19.57 |
104.42W |
17.478? |
19.612? |
17.2 |
8.4 |
Jalisco-Colima Coast | |||
|
3 |
1985.09.19 |
18.19 |
102.53W |
17.592 |
20.038 |
17.0 |
8.2 |
Michoacan Coast, | |||
|
4 |
2011.05.30 |
|
|
17.153 |
19.379 |
16.7 |
8.2 | 49.84% | 48.46% | 24.15% |
|
|
Date |
Fi |
La |
K |
W |
Ks |
Ms |
Pê |
Pw |
P |
Place |
|
1 |
1762.04.02 |
21.50 |
92.00 |
17.555? |
20.444? |
17.7 |
8.8 |
Arakan |
|||
|
2 |
1897.06.12 |
26.00 |
90.50 |
17.249? |
19.569? |
17.6 |
8.7 |
Assam, Shillong Plateau |
|||
|
3 |
2011.05.30 |
|
|
17.611 |
20.531 |
17.7 |
8.8 |
Àðàêàí |
|
|
Date |
Fi |
La |
K |
W |
Ks |
Ms |
Pê |
Pw |
P |
Place |
|
1 |
1840.07.02 |
39.50 |
43.90 |
- |
- |
Ararat |
|||||
|
2 |
1939.12.26 |
39.70 |
39.70 |
16.707 |
19.343 |
16.7 |
7.8 |
NAF | |||
|
3 |
2011.05.30 |
|
|
16.792 |
19.431 |
16.9 |
7.9 |
NAF |
Fig.4. The track diagram Mega SS Myanmar. On earthquake-indicators it is found attractor (a yellow line). Hypothetical points of instability of earthquakes 1762 and 1897 are shown. Till the end of 2012 track will be in instability area in a coastal zone of Arakan in the Northeast of Bengal Bay.
Fig.1. The track diagram Mega SS Anatoly. On earthquakes 1903 and 1939 it is found attractor (a yellow line). Till the end of 2012 track will be in a zone of instability of the North Anatolian Fault in the east of Turkey.
Table 1.
Parameters of instability strong earthquakes with Ìs≥7.8 in Mega SS Anatoly are
resulted.
II. MEGA SS MYANMAR,
Ìs≥8.4.
In the Message from March
27,
2011
forecasts of mega-earthquake did on the basis of
SS
Myanmar
with Ìs≥7.8. In system mega-earthquake
with Ì=8.8 is already prepared, therefore the further monitoring we will do
in Mega
SS
Myanmar
with Ìs≥8.4. The information very poor,
two accidents 1762, 1897 (see
Tab.2) and not come to the end last seismic cycle are known. The
subduction
zone of Arakan is locked since 1762, almost 250 years. Last catastrophic
earthquake in Mega
SS
has occurred in the north of system in 1897. This earthquake has caused
destructions in territory 300000 êì2 with average radius 250 km (the maximum
displacement - to 11 m, 1500 persons were lost) in India, Butane, Bangladesh,
the western Myanmar.
In system in the north of bay of Bengal collision of the Indian plate with
SE
Asia has generated preserved (now inactive)
subduction
zone in the form of a huge funnel "the filled up" 20 km a layer of
sedimentary
rocks. At movement of a
huge elastic Indian plate to
NE, its segment around bay
of Bengal is deformed and plunges, is more true on an hour hand is braided
and pressed under
SE
Asia. This segment of the Indian plate is pressed in the north under a
plateau Shillong, and in the east is linked to the Arakan micro-plate which
shows seismic activity on
right lateral strick-slip
of Sagaing,
Kabaw
and Kaldan faults
(see
Fig.2,3). All these processes are supervised within the limits of
seismic system. When entropy reaches critical
value
(approximately 100-150 years of times) the Arakan microplate is strengthened
(the above-stated internal active
faults are locked) then
periodically works either a zone Shillong or Arakan. Now turn beyond Araka.
In a Fig.3 red line potentially dangerous
locked
area on a
subduction
plane to depths of 30-35 km where the big pressure are presumably
concentrated is shown. The power diagram and the stored experience show that
catastrophic earthquake with Ì=8.8 here
is prepared.
This is confirmed by
GPS
observations. For
instability area on the track diagram in case of Myanmar,
in comparison with Japan and Chile, static
production
of entropy prevails over the dynamic. It means that
the
process
is
slower
and long "ripen" in time, and
loss of
stability (subduction)
can
occur
suddenly, without preliminary seismic activity.
In Tab.2 and Fig.4 values and
track
fragment of preparation of catastrophic earthquake with Ì=8.8 on the
beginning of June, 2011 are resulted. The saved up entropy is equal W=20.531.
This value
inferior
only to record value of entropy of recent earthquake in Japan (W=20.586). As
the system is badly defined, we have calculated
attractor
on points of earthquake-indicators (a yellow line on Fig.4):
K=0.373W+9.949
(2)
For May 2011 K=17.611. Substituting in
eq.(2) we will find
critical value of entropy Wk=20.542. At seismic calm entropy will reach this
value
by February, 2013. So, till the end of 2012 on
NE Bay of Bengal there can
be a catastrophic earthquake with Ì=8.8 and a powerful tsunami.
Fig.3. Schematic cut on profile WE from Fig.2. In the north of Bengal Bay, in zone of dipping of the Indian plate under SE Asia the Arakan seismoactive microplate which is linked to the Indian plate was formed. The subduction zone (blue lines) is seismically locked and covered 20 km. layer of sedimentary rocks. It in the north rests and pressed under the Plateau Shillong. Within 250-300 years periodically activated subduction zone is in the north of Plato Shillong in the coastal zone of Arakan, causing the big destructions and tsunami waves. By the end of 2012 the locked zone between the Indian plate and the Arakan microplate can work. Here mega-earthquake with Ì=8.8 is prepared.
Fig.2. Seismic sources 1762 and 1897 in the north of Bengal Bay. 20 km sedimentary thickness and preserved subduction zone on profile WE is shown on Fig.3. By a red line potentially dangerous locked area on a plane of subduction to depths of 30-35 km where the big pressure are presumably concentrated is shown.
Table 2. Parameters of instability of strong earthquakes with Ìs≥8.4 in Mega SS Myanmar are resulted.
III. MEGA SS MEXICO,
Ìs≥8.2.
In the Bulletin 003 from
September 17,
2010
forecasts of strong earthquakes in the central Mexico did on the basis of
SS
with Ìs≥7.8. There we predicted that "the
Situation in system remains critical, the track is in
attractor. Dangerously in a
coastal zone in the south-southwest
of Oaxaca,
strong earthquake with Ì=7.9 here is expected. There is a deficiency of
energy equal to energy of earthquake-indicator with Ì=7.2. Most likely
earthquake will be trigger or will have strong
foreshock
with Ì=7.2... Depending on development of seismicity danger can migrate in a
coastal zone Acapulco (staff of Guerrero). The situation will be resolved to
the middle of 2011". This forecast lasts till the end of 2012. For the
forecast Mega earthquakes Mexico responsible for preparation of catastrophic
earthquakes with Ìs≥8.2 (see
Fig.5) has been allocated Mega
SS. Taking into account
strong
aftershocks
as such earthquakes have ranked 1907, M8.2 (Guerrero Coast), 1932, M8.4 (Jalisco-Colima
Coast, fatalities 45), 1985, M8.2 (Michoacan Coast, 9500 people killed) (see
Tab.3).
In Tab.3 and
on
Fig.6 values and fragment of track preparation of catastrophic
earthquake with Ì=8.2 on the beginning of June, 2011 are resulted. It is
visible that the track has the big deficiency of energy
earthquake-indicators and while is much more low
attractor, zones of
instability 1932 and 1985. Monitoring in systems with lower threshold
magnitudes shows that the next five years in the central Mexico the cascade
of strong earthquakes with Ì=7.2-7.9 is expected. From Fig.6 it is visible
that only after such activization mega-earthquake preparation in the central
Mexico by 2016 is possible. We will estimate when there can be an
earthquake-indicator with Ì=7.9. We have calculated instability area on
points of strong earthquake-indicators (yellow line on Fig.5):
K=0.718W+3.209
(2)
For May 2011 K=17.153. Substituting in
eq.(2) we will find
critical value of entropy Wk=19.421. At seismic calm entropy will reach this
value
by February-March, 2013. So before this date in a coastal zone of Oaxaca
preparation of strong earthquake with Ì=7.9 is possible. The probability
such earthquakes is resulted
on
Fig.7 and in Tab.3.
Table 3. Parameters
instability of strong earthquakes with Ìs≥8.2 in Mega SS Mexico are resulted.
V. THE COMPARATIVE ANALYSIS OF PREPARATIONS OF MEGA-EARTHQUAKES. All seismic systems for mega-earthquakes are badly defined therefore quality of the forecast the bad. We will carry out the comparative analysis of their tracks. On Fig.11 in the above described systems tracks of preparations of mega-accidents are combined with addition of a track for California. In California and Anatoly seismotectonic situation are a little similar. These are zones of transform faults. Tracks of California and Anatoly also are similar and are grouped slightly more low. Seismic systems on Kamchatka, Mexico and Bay of Bengal are in zones of subduction. Their tracks also are similar and are grouped a little above. In Tab.5 parameters of tracks on the beginning of June, 2011 and a prognostic waiting time of mega-accidents are resulted.
IV. MEGA SS KAMCHATKA, Ìs≥8.4. In the Bulletin 003 from September 17, 2010 we did monitoring and the forecast of strong earthquakes of Kamchatka with Ìs≥7.8. While strong earthquakes on Kamchatka aren't expected. In 1952 there was a catastrophic earthquake with Ì=9.0 at ocean near to a southern extremity of the Kamchatka peninsula, Russia. The tsunami formed at it (the height of waves reached 13–18m) has almost completely destroyed Severo-Kurilsk (island Paramushir) and has led to death more than 2 thousand persons. Catastrophic earthquakes occurred in 1737 and 1841. Under historical data these earthquakes also have formed powerful waves of tsunami. We have decided to estimate possibility of repetition of such accident. On frequency, the next strong earthquake it is necessary for 2059. In revealed Mega SS Kamchatka we have only one authentically come to the end seismic cycle for earthquake 1952 (see Tab.4). On Fig.8,9 contours Mega SS Kamchatka and a fragment of the track diagram are resulted. We have reconsidered and have specified values of instability for earthquake 1952. On size of cumulative energy and entropy the Kamchatka earthquake moves on the third place after Japanese 2011 and the Chilean 1960 earthquakes. The track preparation of catastrophic earthquake while has deficiency energy of earthquake-indicators. At seismic calm entropy will reach a hypothetical zone of instability by the end of 2016. Earthquake with Ì=8.7 by then can be prepared. At activization of earthquake-indicators the situation can change. Probability of earthquake high, but a situation not dangerous (see Fig.10).
Fig.7. Dynamics growth of probability mega earthquakes with Ì≥8.2 in Mega SS Mexico for June 1, 2011.
Table 4. Parameters of instability of strong
earthquakes with Ìs≥8.4 in Mega SS Kamchatka are resulted.
The average period of frequency is 107 years.
Fig.10. Dynamics growth of probability mega earthquakes with Ì≥8.4 in Mega SS Kamchatka for June 1, 2011.
Fig.5. Mega SS Mexico Ì≥8.2. Are shown sources area mega earthquakes 1932 and 1985. Mega earthquake isn't prepared yet. Till the end of 2012 earthquake with Ì=7.9 in a coastal part of Oaxaca is expected. The potential sources are shown by red mugs.
Fig.8. Mega SS Kamchatka Ì≥8.4. Are shown sources area mega earthquakes 1737, 1841 and 1952. Mega earthquake isn't prepared yet and till the end of 2016 it is not expected.
Fig.11. The combined track diagram of preparation of mega-earthquakes in the east of Turkey, in California, Mexico, on SE Kamchatka and Myanmar on the beginning of June 2011.
Fig.9. The track diagram Mega SS Kamchatka. The track on the beginning of June 2011 has the big deficiency of entropy in comparison with a track 1952. The hypothetical area of instability (yellow line) is estimated. By 2016 earthquake with Ì=8.7 in a coastal part of Kamchatka can be prepared.
Fig.6. The track diagram Mega SS Mexico. The track has the big deficiency energy of earthquake-indicators and while is much more low attractor mega earthquakes with Ì≥8.2. On earthquakes-indicators the line of instability for strong earthquakes-indicators (yellow line) is found. Till the end of 2012 earthquake with Ì=7.9 in a coastal part is expected.
|
|
Place |
K |
W |
Ms |
Forecast |
|
1 |
East Turkey, NAF |
16.792 |
19.431 |
7.9 |
Before end 2012 |
|
2 |
Bay of Bengal, Arakan |
17.611 |
20.531 |
8.8 |
Before end 2012 |
|
3 |
California |
17.078 |
19.768 |
8.1 |
Before March 2014 |
|
4 |
Central Mexico |
17.153 |
19.379 |
8.2 |
Before 2017 |
|
5 |
SE Kamchatka (RF) |
17.449 |
20.047 |
8.4 |
After 2017 |
Table 5. Values of parameters of a track for mega earthquakes on the beginning of June 2011 and prognostic time of their expectation are resulted.
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