FAST TRACK PAPER: Extraction of absolute P velocity from receiver functions

Astronomy and Astrophysics – Astronomy

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Composition Of The Continental Crust, Body Waves

Scientific paper

Receiver functions constitute an important tool in regional and global studies of crust and upper-mantle structure and are frequently employed to constrain crustal thickness and bulk VP/VS ratio. The methods commonly used to compute these parameters assume a known crustal P velocity; however, this quantity trades off with crustal thickness. We demonstrate that P velocity and VP/VS ratio can be readily computed through solution of a linear system of equations incorporating traveltimes of direct conversions and free-surface reverberations, representing a range of horizontal slowness. Determination of crustal thickness follows trivially. We apply this approach to data from station HYB on the Indian craton to determine bulk VP/VS ratio, P velocity and thickness of 1.79 +/- 0.007, 6.1 +/- 0.13 kms-1 and 30.5 +/- 0.8 km, respectively. The addition of average crustal P velocity to the suite of parameters accessible from receiver function data may prove useful in constraining bulk crustal composition and its secular evolution.

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