Upper Mantle Structure in and around the Indian sub-continent

Authors

  • RK DUBE

DOI:

https://doi.org/10.54302/mausam.v20i1.5428

Abstract

The structure of the Upper Mantle has been studied from the P-wave travel times, using the computation of Dowling and Nuttli. Results indicate the presence of a low velocity layer 140 km below the M-discontinuity and its thickness is estimated as about 50 km. A steep velocity gradient below the low velocity layer explains the observed results.

Downloads

Download data is not yet available.

Downloads

Published

1969-01-01

Issue

Vol. 20 No. 1 (1969): MAUSAM

Section

Shorter Contribution

Categories

License

Copyright (c) 2022 MAUSAM

Creative Commons License

This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.

All articles published by MAUSAM are licensed under the Creative Commons Attribution 4.0 International License. This permits anyone.

Anyone is free:

  • To Share - to copy, distribute and transmit the work
  • To Remix - to adapt the work.

Under the following conditions:

  • Share - copy and redistribute the material in any medium or format
  • Adapt - remix, transform, and build upon the material for any purpose, even
    commercially.

How to Cite

[1]
“Upper Mantle Structure in and around the Indian sub-continent”, MAUSAM, vol. 20, no. 1, pp. 47–52, Jan. 1969, doi: 10.54302/mausam.v20i1.5428.