ISSN:
1420-9136
Source:
Springer Online Journal Archives 1860-2000
Topics:
Geosciences
,
Physics
Notes:
Summary P- andS-wave travel times of 56 shallow earthquakes with their epicentres in and around the Andaman Sea, as recorded by the Indian Seismological Observatories situated at Madras, Visakhapatnam, Calcutta and Port Blair, have been analysed statistically. The travel times from Δ=1 ° to 17 ° can be represented by one straight-line segment. When epicentres of all the earthquakes are considered, scatter in the travel-time data is greater and the corresponding apparentP- andS-wave velocities have been found to be 8.56±0.20 km/sec and 4.84±0.36 km/sec respectively. On the other hand, if epicentres of the narrow seismic zone situated along the western border of the Andaman Sea alone are considered, the apparentP- andS-wave velocities have been found to be 8.24±0.09 km/sec and 4.74±0.10 km/sec respectively. The O-JB residuals are found to be consistently negative for the second set of epicentres which is indicative of an inclined Mohorovicic discontinuity in the Bay of Bengal region.
Type of Medium:
Electronic Resource
URL:
http://dx.doi.org/10.1007/BF00876149
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