Journal of Himalayan Geology, Volume 6Wada Institute of Himalayan Geology, 1995 - Geology |
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Page 1
The top layer with an estimated thickness of 12 +0.5 km has P and S wave
velocities of 5.9 +0.2 km / s and 3.4 + 0.1 km / s respectively . These corresponds
to a Poisson's ratio ( 0 ) of 0.23 for this layer . The second layer is approximately 5
km ...
The top layer with an estimated thickness of 12 +0.5 km has P and S wave
velocities of 5.9 +0.2 km / s and 3.4 + 0.1 km / s respectively . These corresponds
to a Poisson's ratio ( 0 ) of 0.23 for this layer . The second layer is approximately 5
km ...
Page 6
The standard deviation of the fit in this case is 0.073 s with the S wave velocity
estimate of 3.4 +0.1 km / s . The average density of the upper crustal material is
estimated by Verma and Mukhopadhyay ( 1977 ) to be 2.96 gm / cc . The V / V
ratio ...
The standard deviation of the fit in this case is 0.073 s with the S wave velocity
estimate of 3.4 +0.1 km / s . The average density of the upper crustal material is
estimated by Verma and Mukhopadhyay ( 1977 ) to be 2.96 gm / cc . The V / V
ratio ...
Page 16
We note that all these estimates lie in the range of 15 to 20 km . HATANAKA , Y. &
SHIMAZAI , K. , 1988. Rupture process ... studied here is shown in figure 7. The
final fault plane solution estimated is given in table - 5 . The matching is good in ...
We note that all these estimates lie in the range of 15 to 20 km . HATANAKA , Y. &
SHIMAZAI , K. , 1988. Rupture process ... studied here is shown in figure 7. The
final fault plane solution estimated is given in table - 5 . The matching is good in ...
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Contents
START | 1 |
GET FILE NAME | 72 |
S MUKHOPADHYAYA K N KHATTRI R CHANDER Seismic Velocity and Related Elastic Parameters | 6 |
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