Subcrustal Low Velocity Layers in Central India and their Implications |
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Authors: | A S N Murty H C Tewari Prakash Kumar P R Reddy |
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Institution: | (1) National Geophysical Research Institute, Uppal Road, Hyderabad, 500 007, India |
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Abstract: | A 2-D subcrustal velocity model for the central Indian continental lithosphere has been derived by travel time and relative
amplitude modeling of a digitally normalized analog seismic record section of the Hirapur-Mandla DSS profile, using a ray-tracing
technique. Some prominent wave groups with apparent velocities slightly higher than the Moho reflection phase (PMP) are identified on the normalized record sections assembled with a reduction velocity of 6 km s−1. We interpret these phases as the wide-angle reflections from subcrustal lithospheric boundaries. Comparison of synthetic
seismograms with the observed record section shows that the observed phases cannot be explained either by multiples or by
the P-to-S converted phase (PMS) from the Moho. Subcrustal velocity models either with a velocity increase or with a single low velocity layer (LVL) also
do not provide a satisfactory fit. We infer that a subcrustal velocity model with two alternate LVLs (velocity 7.2 km s−1), separated by a 6-km thick high velocity layer (velocity 8.1 km s−1), can satisfy both the observed travel times and amplitudes. The prominent reflection phases are modeled at depths of 49,
51, 57 and 60 km. It is inferred that the subcrustal lithosphere in the central Indian region has a lamellar structure with
varying structural and mechanical properties. The alternating LVLs, occurring at relatively shallow depths below Moho, may
be associated with the zones of weakness and lower viscosity suggesting continued mobility, with a possible thermal source
in the upper mantle. This explains the source of observed high heat flow values in the central Indian region. |
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Keywords: | Wide-angle reflection upper mantle synthetic seismograms narmada zone low velocity layers seismic velocity |
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