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
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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: 873 (including HTML, PDF, and XML)
Thereof 845 with geography defined
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Total article views: 685 (including HTML, PDF, and XML)
Thereof 668 with geography defined
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Total article views: 188 (including HTML, PDF, and XML)
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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,...