Structure of the crust-uppermost mantle beneath the Ethiopian volcanic province using ambient seismic noise and teleseismic P wave coda autocorrelation-Reference-Cited by-同舟云学术

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Structure of the crust-uppermost mantle beneath the Ethiopian volcanic province using ambient seismic noise and teleseismic P wave coda autocorrelation

Published:2023-12 Issue: Volume:869 Page:230092
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Alemayehu Sisay,Aoudia Abdelkrim,Ayele Atalay,Pachhai Surya,Thapa Hari Ram,Ebinger C.J.,Kherchouche Radia,Guidarelli Mariangela,Kim Seongryong

Funder

Abdus Salam International Centre for Theoretical Physics

Addis Ababa University

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference114 articles.

1. Group velocity tomography of the Indo-Eurasian collision zone;Acton;J. Geophys. Res. Solid Earth,2010

2. A review of earthquake source parameters in the main Ethiopian rift;Alemayehu;Int. J. Geophys.,2023

3. Upper mantle temperature and the onset of extension and break-up in Afar, Africa;Armitage;Earth Planet. Sci. Lett.,2015

4. Stratigraphic framework of the northeastern part of the Ethiopian flood basalt province;Ayalew;Bull. Volcanol.,2021

5. Spatial and temporal variations of seismicity in the Horn of Africa from 1960 to 1993;Ayele;Geophys. J. Int.,1997

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