Abstract
Rayleigh wave group and phase velocity measurements obtained from ambient noise and earthquake data at 51 broadband stations were used to construct the first 3-D crustal and upper mantle shear wave velocity model of Botswana. The model shows low crustal velocities associated with the Passarge and Nosop sedimentary basins, whereas the Kaapvaal, Zimbabwe, Maltahohe, and Congo Cratons are recognized by high mantle velocities. The lowest upper mantle shear wave velocity, beneath northeastern Botswana, is associated with the southwestern branch of the East African Rift System. This low-velocity mantle anomaly appears to be linked to the crust of the Okavango Rift Zone and the location of the 3 April 2017 Mw 6.5 earthquake in central Botswana. We suggest that fluids or melt at the base of the crust from the southward continuation of the East African Rift Zone triggered the intraplate earthquake in an extensional tectonic setting.
Original language | English |
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Article number | e2019GL085598 |
Number of pages | 12 |
Journal | Geophysical Research Letters |
Volume | 47 |
Issue number | 4 |
DOIs | |
Publication status | Published - 28 Feb 2020 |
Funding
This work was funded by the Netherlands Organization for Scientific Research (NWO), Grant ALW-GO-AO/11-30. We thank Arie van Wettum (Utrecht University) and the deployment team of the Botswana Geoscience Institute for their efforts to install and maintain the NARS-Botswana network. Data used in this study can be accessed from the IRIS data management center (http://ds.iris.edu/ds/).
Keywords
- ambient noise
- continental rift
- craton
- earthquakes
- seismology
- surface wave tomography