Seismic Evidence for Plume- and Craton-Influenced Upper Mantle Structure Beneath the Northern Malawi Rift and the Rungwe Volcanic Province, East Africa

Ashley Grijalva, Andrew Arnold Nyblade, Kyle A. Homman, Natalie J. Accardo, James B. Gaherty, Cynthia J. Ebinger, Donna J. Shillington, Patrick R.N. Chindandali, Gabriel Mbogoni, Richard Wambura Ferdinand, Gabriel Mulibo, J. P. O'Donnell, Marsella Kachingwe, Gabrielle Tepp

Research output: Contribution to journalArticle

3 Citations (Scopus)

Abstract

P and S wave tomographic models have been developed for the northern Malawi rift and adjacent Rungwe Volcanic Province (RVP) using data from the Study of Extension and maGmatism in Malawi aNd Tanzania project and data from previous networks in the study area. The main features of the models are a low-velocity zone (LVZ) with δVp = ~−1.5–2.0% and δVs = ~−2–3% centered beneath the RVP, a lower-amplitude LVZ (δVp = ~−1.0–1.3% and δVs = ~−0.7–1%) to the southeast of the RVP beneath the center and northeastern side of the northern Malawi rift, a shift of the lower-amplitude anomaly at ~−10° to −11° to the west beneath the central basin and to the western side of the rift, and a fast anomaly at all depths beneath the Bangweulu Craton. The LVZ widens further at depths >~150–200 km and extends to the north beneath northwestern Malawi, wrapping around the fast anomaly beneath the craton. We attribute the LVZ beneath the RVP and the northern Malawi rift to the flow of warm, superplume mantle from the southwest, upwelling beneath and around the Bangweulu Craton lithosphere, consistent with high 3He/4He values from the RVP. The LVZ under the RVP and northern Malawi rift strongly indicates that the rifted lithosphere has been thermally perturbed. Given that volcanism in the RVP began about 10 million years earlier than the rift faulting, thermal and/or magmatic weakening of the lithosphere may have begun prior to the onset of rifting.

Original languageEnglish (US)
Pages (from-to)3980-3994
Number of pages15
JournalGeochemistry, Geophysics, Geosystems
Volume19
Issue number10
DOIs
StatePublished - Oct 1 2018

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Malawi
mantle structure
cratons
plumes
craton
upper mantle
volcanology
low velocity zone
Earth mantle
plume
low speed
lithosphere
anomalies
anomaly
Faulting
Tanzania
upwelling water
province
East Africa
P waves

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Geochemistry and Petrology

Cite this

Grijalva, Ashley ; Nyblade, Andrew Arnold ; Homman, Kyle A. ; Accardo, Natalie J. ; Gaherty, James B. ; Ebinger, Cynthia J. ; Shillington, Donna J. ; Chindandali, Patrick R.N. ; Mbogoni, Gabriel ; Ferdinand, Richard Wambura ; Mulibo, Gabriel ; O'Donnell, J. P. ; Kachingwe, Marsella ; Tepp, Gabrielle. / Seismic Evidence for Plume- and Craton-Influenced Upper Mantle Structure Beneath the Northern Malawi Rift and the Rungwe Volcanic Province, East Africa. In: Geochemistry, Geophysics, Geosystems. 2018 ; Vol. 19, No. 10. pp. 3980-3994.
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abstract = "P and S wave tomographic models have been developed for the northern Malawi rift and adjacent Rungwe Volcanic Province (RVP) using data from the Study of Extension and maGmatism in Malawi aNd Tanzania project and data from previous networks in the study area. The main features of the models are a low-velocity zone (LVZ) with δVp = ~−1.5–2.0{\%} and δVs = ~−2–3{\%} centered beneath the RVP, a lower-amplitude LVZ (δVp = ~−1.0–1.3{\%} and δVs = ~−0.7–1{\%}) to the southeast of the RVP beneath the center and northeastern side of the northern Malawi rift, a shift of the lower-amplitude anomaly at ~−10° to −11° to the west beneath the central basin and to the western side of the rift, and a fast anomaly at all depths beneath the Bangweulu Craton. The LVZ widens further at depths >~150–200 km and extends to the north beneath northwestern Malawi, wrapping around the fast anomaly beneath the craton. We attribute the LVZ beneath the RVP and the northern Malawi rift to the flow of warm, superplume mantle from the southwest, upwelling beneath and around the Bangweulu Craton lithosphere, consistent with high 3He/4He values from the RVP. The LVZ under the RVP and northern Malawi rift strongly indicates that the rifted lithosphere has been thermally perturbed. Given that volcanism in the RVP began about 10 million years earlier than the rift faulting, thermal and/or magmatic weakening of the lithosphere may have begun prior to the onset of rifting.",
author = "Ashley Grijalva and Nyblade, {Andrew Arnold} and Homman, {Kyle A.} and Accardo, {Natalie J.} and Gaherty, {James B.} and Ebinger, {Cynthia J.} and Shillington, {Donna J.} and Chindandali, {Patrick R.N.} and Gabriel Mbogoni and Ferdinand, {Richard Wambura} and Gabriel Mulibo and O'Donnell, {J. P.} and Marsella Kachingwe and Gabrielle Tepp",
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Grijalva, A, Nyblade, AA, Homman, KA, Accardo, NJ, Gaherty, JB, Ebinger, CJ, Shillington, DJ, Chindandali, PRN, Mbogoni, G, Ferdinand, RW, Mulibo, G, O'Donnell, JP, Kachingwe, M & Tepp, G 2018, 'Seismic Evidence for Plume- and Craton-Influenced Upper Mantle Structure Beneath the Northern Malawi Rift and the Rungwe Volcanic Province, East Africa', Geochemistry, Geophysics, Geosystems, vol. 19, no. 10, pp. 3980-3994. https://doi.org/10.1029/2018GC007730

Seismic Evidence for Plume- and Craton-Influenced Upper Mantle Structure Beneath the Northern Malawi Rift and the Rungwe Volcanic Province, East Africa. / Grijalva, Ashley; Nyblade, Andrew Arnold; Homman, Kyle A.; Accardo, Natalie J.; Gaherty, James B.; Ebinger, Cynthia J.; Shillington, Donna J.; Chindandali, Patrick R.N.; Mbogoni, Gabriel; Ferdinand, Richard Wambura; Mulibo, Gabriel; O'Donnell, J. P.; Kachingwe, Marsella; Tepp, Gabrielle.

In: Geochemistry, Geophysics, Geosystems, Vol. 19, No. 10, 01.10.2018, p. 3980-3994.

Research output: Contribution to journalArticle

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AU - Grijalva, Ashley

AU - Nyblade, Andrew Arnold

AU - Homman, Kyle A.

AU - Accardo, Natalie J.

AU - Gaherty, James B.

AU - Ebinger, Cynthia J.

AU - Shillington, Donna J.

AU - Chindandali, Patrick R.N.

AU - Mbogoni, Gabriel

AU - Ferdinand, Richard Wambura

AU - Mulibo, Gabriel

AU - O'Donnell, J. P.

AU - Kachingwe, Marsella

AU - Tepp, Gabrielle

PY - 2018/10/1

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N2 - P and S wave tomographic models have been developed for the northern Malawi rift and adjacent Rungwe Volcanic Province (RVP) using data from the Study of Extension and maGmatism in Malawi aNd Tanzania project and data from previous networks in the study area. The main features of the models are a low-velocity zone (LVZ) with δVp = ~−1.5–2.0% and δVs = ~−2–3% centered beneath the RVP, a lower-amplitude LVZ (δVp = ~−1.0–1.3% and δVs = ~−0.7–1%) to the southeast of the RVP beneath the center and northeastern side of the northern Malawi rift, a shift of the lower-amplitude anomaly at ~−10° to −11° to the west beneath the central basin and to the western side of the rift, and a fast anomaly at all depths beneath the Bangweulu Craton. The LVZ widens further at depths >~150–200 km and extends to the north beneath northwestern Malawi, wrapping around the fast anomaly beneath the craton. We attribute the LVZ beneath the RVP and the northern Malawi rift to the flow of warm, superplume mantle from the southwest, upwelling beneath and around the Bangweulu Craton lithosphere, consistent with high 3He/4He values from the RVP. The LVZ under the RVP and northern Malawi rift strongly indicates that the rifted lithosphere has been thermally perturbed. Given that volcanism in the RVP began about 10 million years earlier than the rift faulting, thermal and/or magmatic weakening of the lithosphere may have begun prior to the onset of rifting.

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