Wet Mantle Transition Zone beneath the Indian shield? Constraints from P-to-S Receiver Functions Analysis

Author:

Kharita Akash1ORCID,Mukhopadhyay Sagarika1

Affiliation:

1. Indian Institute of Technology Roorkee

Publisher

Wiley

Reference71 articles.

1. The isolation of receiver effects from teleseismic P waveforms;Ammon C. J.;Bulletin - Seismological Society of America,1991

2. On the nonuniqueness of receiver function inversions;Ammon C. J.;Journal of Geophysical Research, 95(B10). https://doi.org/10.1029/JB095IB10P15303,1990

3. Whole-mantle convection and the transition-zone water filter;Bercovici D.;Nature,2003

4. Bina C. Solid G. H.-J. of G. R. & 1994 undefined ??. (1994). Phase transition Clapeyron slopes and transition zone seismic discontinuity topography. Wiley Online Library 99(B8) 853-868. https://doi.org/10.1029/94JB00462

5. Inversion of receiver functions without deconvolutionapplication to the Indian craton;Bodin T.;Geophysical Journal International,2013

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