Articles | Volume 15, issue 7
https://doi.org/10.5194/se-15-747-2024
https://doi.org/10.5194/se-15-747-2024
Research article
 | 
05 Jul 2024
Research article |  | 05 Jul 2024

Propagating rifts: the roles of crustal damage and ascending mantle fluids

Folarin Kolawole and Rasheed Ajala

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)

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.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 20 Nov 2024
Download
Short summary
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.