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Originally posted by dreamfox1
Originally posted by MariaLida
Sry dreamfox1 I was little late I do search but meanwhile you make post ..
2013-01-09 01:41:53.0 15min ago 25.40 N 94.94 E 80 6.0 MYANMAR-INDIA BORDER REGION
static1.emsc.eu...
www.emsc-csem.org...
Magnitude M 6.0
Region MYANMAR-INDIA BORDER REGION
Date time 2013-01-09 01:41:53.0 UTC
Location 25.38 N ; 94.96 E
Depth 86 km
Distances 395 km NW Mandalay (pop 1,208,099 ; local time 08:11:53.2 2013-01-09)
122 km NE Imphal (pop 223,523 ; local time 07:11:53.2 2013-01-09)
56 km SE Phek (pop 15,118 ; local time 07:11:53.2 2013-01-09)edit on 8-1-2013 by MariaLida because: (no reason given)
No problem the more info the better
This earthquake occurred on the Carlsberg Ridge, a mid-ocean ridge system that is located in the Arabian sea between India and Northern Africa. The ridge marks the boundary between the Indian and African plates and near the epicenter the Indian plate is moving away from the African Plate at a rate of 33 mm/yr in a northeasterly direction. The Carlsberg Ridge is a slow-spreading ridge with rough topography and a depth that varies from 1700-4400 meters.
Mid-ocean ridges are divergent plate boundaries, where two tectonic plates move apart from each other. New oceanic crust is formed as magma rises up between the two diverging plates. Active spreading ridges are offset by zones known as transform faults, where plates slide horizontally past each other neither destroying or forming crust. This gives the plate boundary a zig-zag pattern. Ocean ridges represent the longest, linear uplifted features of the earth's surface and are marked by a belt of shallow earthquakes. Earthquakes can be caused by the release of tensional stress in the uplifted ridge or by the horizontal movement of plates along the transform faults.
J. Geophys. Res., 111, B04302
Rupture characteristics of the 2003 Mw 7.6 mid-Indian Ocean earthquake: Implications for seismic properties of young oceanic lithosphere
Michael Antolik 1,3,
Rachel E. Abercrombie 2,
Jianfeng Pan 1,
Göran Ekström 1
Author Information
1 Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts, USA
2 Department of Earth Sciences, Boston University, Boston, Massachusetts, USA
3 Now at Quantum Technology Services, Inc., Cocoa Beach, Florida, USA.
Email: Michael Antolik ([email protected])
Publication History
Issue published online: 13 APR 2006
Article first published online: 13 APR 2006
Manuscript Accepted: 20 DEC 2005
Manuscript Revised: 12 OCT 2005
Manuscript Received: 16 APR 2005
Abstract
Keywords:
seismology;
tectonics;
Indian Ocean
[1] Analysis of broadband seismograms from the 15 July 2003 large earthquake (M 7.6) in the central Indian Ocean reveals an unusual source process. The source duration of longer than a minute is more than twice as long as expected from earthquake scaling relations, yet ∼80% of the moment release occurred in two energetic asperities near the end of the rupture. These two asperities were located in lithosphere with an age of 7 Ma or greater. A previous study has suggested that strike-slip earthquakes in oceanic lithosphere having much longer than expected source durations also have a slow, dissipative rupture process characterized by low radiated seismic energy (and therefore low apparent stress). We find no evidence for a slow rupture process to the 2003 earthquake. Instead, the long duration appears to be due only to nucleation close to the actively spreading Carlsberg Ridge, in lithosphere younger than 7 Ma. Younger oceanic lithosphere may be able to generate small to moderate earthquakes but be unable to sustain slip in a large event due to steady release of strain in aseismic creep events. Large strike-slip earthquakes within oceanic lithosphere may occur only in the central portions of long transform faults or in intraplate regions, rupturing energetic asperities like those that failed in the mid-Indian Ocean earthquake and leading to the observation that oceanic strike-slip earthquakes have the largest apparent stresses among the global population of shallow earthquakes.
Originally posted by MariaLida
reply to post by dreamfox1
Swarm still going ..
Probably this EQ swarm will have influences on Indonesia and Indian plate again after Myanmar EQ ..
2013-01-09 13:32:01.936min ago 1.85 S 67.94 E 10 4.5 CARLSBERG RIDGE
2013-01-09 10:51:32.03hr 17min ago 1.93 S 68.00 E 20 4.9 CARLSBERG RIDGE
2013-01-09 10:35:52.03hr 32min ago 1.93 S 67.93 E 10 4.6 CARLSBERG RIDGE
2013-01-09 10:27:47.03hr 40min ago 1.91 S 67.88 E 10 4.9 CARLSBERG RIDGE
2013-01-09 10:08:45.03hr 59min ago 1.97 S 67.71 E 10 4.8 CARLSBERG RIDGE
2013-01-09 09:40:53.04hr 27min ago 1.88 S 67.94 E 10 4.8 CARLSBERG RIDGE
2013-01-09 09:02:40.05hr 05min ago 1.96 S 67.88 E 10 4.8 CARLSBERG RIDGE
2013-01-09 06:50:38.07hr 17min ago 1.88 S 68.01 E 10 4.8 CARLSBERG RIDGE
2013-01-09 06:21:56.07hr 46min ago 1.88 S 68.03 E 5 4.8 CARLSBERG RIDGE
2013-01-09 05:27:05.08hr 41min ago 1.81 S 67.93 E 10 5.0 CARLSBERG RIDGE
2013-01-09 04:46:29.09hr 22min ago 1.85 S 67.93 E 10 4.9 CARLSBERG RIDGE
2013-01-08 23:42:57.0 2.23 S 67.97 E 10 4.7 CARLSBERG RIDGE
2013-01-08 23:38:44.0 1.96 S 68.03 E 10 4.7 CARLSBERG RIDGE
2013-01-08 23:31:49.0 1.95 S 68.08 E 10 4.6 CARLSBERG RIDGE
www.emsc-csem.org...
Stanford geophysicists are well represented at the meeting of the American Geophysical Union this week in San Francisco. Included among the many presentations will be several studies that relate to predicting – and preparing for – major earthquakes in the Himalaya Mountains and the Pacific Northwest.
The AGU Fall Meeting is the largest worldwide conference in the geophysical sciences, attracting more than 20,000 Earth and space scientists, educators, students, and other leaders. This 45th annual fall meeting is taking place through Dec. 7 at the Moscone Convention Center in San Francisco.
Originally posted by MariaLida
Originally posted by MariaLida
reply to post by dreamfox1
Swarm still going ..
Probably this EQ swarm will have influences on Indonesia and Indian plate again after Myanmar EQ ..
2013-01-09 13:32:01.936min ago 1.85 S 67.94 E 10 4.5 CARLSBERG RIDGE
2013-01-09 10:51:32.03hr 17min ago 1.93 S 68.00 E 20 4.9 CARLSBERG RIDGE
2013-01-09 10:35:52.03hr 32min ago 1.93 S 67.93 E 10 4.6 CARLSBERG RIDGE
2013-01-09 10:27:47.03hr 40min ago 1.91 S 67.88 E 10 4.9 CARLSBERG RIDGE
2013-01-09 10:08:45.03hr 59min ago 1.97 S 67.71 E 10 4.8 CARLSBERG RIDGE
2013-01-09 09:40:53.04hr 27min ago 1.88 S 67.94 E 10 4.8 CARLSBERG RIDGE
2013-01-09 09:02:40.05hr 05min ago 1.96 S 67.88 E 10 4.8 CARLSBERG RIDGE
2013-01-09 06:50:38.07hr 17min ago 1.88 S 68.01 E 10 4.8 CARLSBERG RIDGE
2013-01-09 06:21:56.07hr 46min ago 1.88 S 68.03 E 5 4.8 CARLSBERG RIDGE
2013-01-09 05:27:05.08hr 41min ago 1.81 S 67.93 E 10 5.0 CARLSBERG RIDGE
2013-01-09 04:46:29.09hr 22min ago 1.85 S 67.93 E 10 4.9 CARLSBERG RIDGE
2013-01-08 23:42:57.0 2.23 S 67.97 E 10 4.7 CARLSBERG RIDGE
2013-01-08 23:38:44.0 1.96 S 68.03 E 10 4.7 CARLSBERG RIDGE
2013-01-08 23:31:49.0 1.95 S 68.08 E 10 4.6 CARLSBERG RIDGE
www.emsc-csem.org...
Himalayas and Pacific Northwest could experience major earthquakes, Stanford geophysicists say
Stanford Report, December 5, 2012
A big one in the Himalayas
Measuring small tremors in the Pacific Northwest
Cascadia quake simulations
Stanford geophysicists are well represented at the meeting of the American Geophysical Union this week in San Francisco. Included among the many presentations will be several studies that relate to predicting – and preparing for – major earthquakes in the Himalaya Mountains and the Pacific Northwest.
The AGU Fall Meeting is the largest worldwide conference in the geophysical sciences, attracting more than 20,000 Earth and space scientists, educators, students, and other leaders. This 45th annual fall meeting is taking place through Dec. 7 at the Moscone Convention Center in San Francisco.
news.stanford.edu...
Earthquake Risk Perception among Citizens in Kathmandu, Nepal
www.massey.ac.nz...
phys.org...
www.lalitpur.org.np...
www.huffingtonpost.com...edit on 9-1-2013 by MariaLida because: (no reason given)
Originally posted by dreamfox1
5.0 Off the west coast of northern Sumatra 2013-01-09 21:05:01 0.758°N 92.727°E 14.9
edit on 7/30/2012 by dreamfox1 because: updates