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The Mw 7.6, Kashmir Earthquake of October 8, 2005.

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The Mw 7.6, Kashmir Earthquake of October 8, 2005
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Page 1: The Mw 7.6, Kashmir Earthquake of October 8, 2005.

The Mw 7.6, Kashmir Earthquake of October 8, 2005

Page 2: The Mw 7.6, Kashmir Earthquake of October 8, 2005.

The Mw 7.6, Kashmir Earthquake of October 8, 2005

N-S ground displacements measured from ASTER Images of October 27, 2005 and November 14, 2000

Page 3: The Mw 7.6, Kashmir Earthquake of October 8, 2005.

The Mw 7.6, Kashmir Earthquake of October 8, 2005

N-S ground displacements measured from ASTER Images of October 27, 2005 and November 14, 2000

The Horizontal slip on the fault was about 5 m over a distance of about 70 km

5 m

Page 4: The Mw 7.6, Kashmir Earthquake of October 8, 2005.
Page 5: The Mw 7.6, Kashmir Earthquake of October 8, 2005.

Amplitude of Horizontal slip

Horizontal fault slip vectors

2m

Page 6: The Mw 7.6, Kashmir Earthquake of October 8, 2005.
Page 7: The Mw 7.6, Kashmir Earthquake of October 8, 2005.
Page 8: The Mw 7.6, Kashmir Earthquake of October 8, 2005.
Page 9: The Mw 7.6, Kashmir Earthquake of October 8, 2005.
Page 10: The Mw 7.6, Kashmir Earthquake of October 8, 2005.
Page 11: The Mw 7.6, Kashmir Earthquake of October 8, 2005.

Estimated Rupture Area of major Himalayan earthquakes

Page 12: The Mw 7.6, Kashmir Earthquake of October 8, 2005.

According to GPS measurements and microseismic monitoring the Main Himalaya Thrust fault is locked over a width of 100-150km (yellow aera).The Accumulation rate of deficit of seismic moment is estimated 4.3 1019 Nm/yr , this is enough to drive a a Mw 7.6 (like the 2005 Kashmir EQ) earthquake every 7 years, or a Mw 8.2 (like the Bihar-Nepal earthqiake of 1934 every 100yr).

1934

1833

1505 ?


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