Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10964, United States
Department of Earth and Environmental Sciences, Columbia University, New York, New York 10027, United States
Rasheed Ajala
Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10964, United States
Viewed
Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 835 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
682
121
32
835
59
24
31
HTML: 682
PDF: 121
XML: 32
Total: 835
Supplement: 59
BibTeX: 24
EndNote: 31
Views and downloads (calculated since 24 Nov 2023)
Cumulative views and downloads
(calculated since 24 Nov 2023)
Total article views: 647 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
494
121
32
647
59
24
31
HTML: 494
PDF: 121
XML: 32
Total: 647
Supplement: 59
BibTeX: 24
EndNote: 31
Views and downloads (calculated since 05 Jul 2024)
Cumulative views and downloads
(calculated since 05 Jul 2024)
Total article views: 188 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
188
0
0
188
0
0
HTML: 188
PDF: 0
XML: 0
Total: 188
BibTeX: 0
EndNote: 0
Views and downloads (calculated since 24 Nov 2023)
Cumulative views and downloads
(calculated since 24 Nov 2023)
Viewed (geographical distribution)
Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 835 (including HTML, PDF, and XML)
Thereof 806 with geography defined
and 29 with unknown origin.
Total article views: 647 (including HTML, PDF, and XML)
Thereof 629 with geography defined
and 18 with unknown origin.
Total article views: 188 (including HTML, PDF, and XML)
Thereof 177 with geography defined
and 11 with unknown origin.
We investigate the upper-crustal structure of the Rukwa–Tanganyika rift zone in East Africa, where the Tanganyika rift interacts with the Rukwa and Mweru-Wantipa rifts, coinciding with abundant seismicity at the rift tips. Seismic velocity structure and patterns of seismicity clustering reveal zones around 10 km deep with anomalously high Vp / Vs ratios at the rift tips, indicative of a localized mechanically weakened crust caused by mantle volatiles and damage associated with bending strain.
We investigate the upper-crustal structure of the Rukwa–Tanganyika rift zone in East Africa,...