Articles | Volume 10, issue 6
https://doi.org/10.5194/se-10-1857-2019
https://doi.org/10.5194/se-10-1857-2019
Research article
 | 
04 Nov 2019
Research article |  | 04 Nov 2019

Anisotropic P-wave travel-time tomography implementing Thomsen's weak approximation in TOMO3D

Adrià Meléndez, Clara Estela Jiménez, Valentí Sallarès, and César R. Ranero

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Adrià Meléndez on behalf of the Authors (04 Jul 2019)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (05 Jul 2019) by Michal Malinowski
RR by Anonymous Referee #2 (04 Sep 2019)
ED: Publish subject to minor revisions (review by editor) (04 Sep 2019) by Michal Malinowski
AR by Adrià Meléndez on behalf of the Authors (06 Sep 2019)  Author's response   Manuscript 
ED: Publish as is (11 Sep 2019) by Michal Malinowski
ED: Publish as is (18 Sep 2019) by CharLotte Krawczyk (Executive editor)
AR by Adrià Meléndez on behalf of the Authors (23 Sep 2019)  Manuscript 
Download
Short summary
A new code for anisotropic travel-time tomography is presented. We describe the equations governing the anisotropic ray propagation algorithm and the modified inversion solver. We study the sensitivity of two medium parameterizations and compare four inversion strategies on a canonical model. This code can provide better understanding of the Earth's subsurface in the rather common geological contexts in which seismic velocity displays a weak dependency on the polar angle of ray propagation.