Njinju, Emmanuel A; Atekwana, Estella A (2025): A file of processed gravity data for the Rukwa-Tanganyika Rift Zone, including the sediment- and mantle-corrected gravity data and the Moho depth estimates derived from power spectral analysis [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.984227
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Published: 2025-09-16 • DOI registered: 2025-10-15
Abstract:
The Rukwa-Tanganyika Rift Zone (RTRZ), experiencing multiphase rifting, forms the nonvolcanic southern part of the Western Branch of the East African Rift. We investigate the crustal structure beneath the RTRZ to understand how strain migrates beneath multiphase rifts. We use Bouguer gravity data from the World Gravity Map 2012 (Balmino et al., 2012; Bonvalot et al., 2012) and power spectral analysis to estimate the depth to Moho beneath the RTRZ. We correct for the effect of sediments and the deep mantle from the Bouguer gravity data. The deep mantle gravity is obtained by scaling the S40RTS global seismic tomography model (Ritsema et al., 2011) into equivalent deep mantle density anomalies using a velocity-to-density scaling factor of 0.15 (e.g., Behn et al., 2004; Conrad et al., 2007; Conrad & Behn, 2010). The gravity anomaly g(r) of the deep mantle is forward calculated from the deep mantle density anomalies using the Gauss-Legendre Quadrature (GLQ) elemental integration. Similarly, the gravitational effect of the known sedimentary basins (from CRUST1.0; Laske et al., 2013) is forward calculated numerically using the GLQ elemental integration (Asgharzadeh et al., 2007; Uieda et al., 2016; Uieda & Barbosa, 2017). Here we include a data file of the processed gravity data for the RTRZ, including the sediment- and mantle-corrected gravity data and the Moho depth estimates derived from power spectral analysis of the gravity data. The dataset consists of eight columns representing the different parameters measured with units in []: (1) Longitude (2) Latitude (3) Bouguer_GRAVITY_WGM2012 [mGal] (4) Sediment_Thickness [m] (5) Moho Depths [km] (6) Mantle_Gravity [mGal] (7) Sediment_Gravity_Effect [mGal] (8) Gravity_Effect_of_Deep_Mantle_and_Sediments [mGal].
Supplement to:
Njinju, Emmanuel A; Atekwana, Estella A (2025): A Gravity Study of the Crustal Structure Beneath the Young Amagmatic Rukwa-Tanganyika Rift Zone. Tectonics, 44(8), e2024TC008722, https://doi.org/10.1029/2024TC008722
References:
Asgharzadeh, M F; von Frese, Ralph R B; Kim, Hyung Rae; Leftwich, T E; Kim, Jae Woo (2007): Spherical prism gravity effects by Gauss-Legendre quadrature integration. Geophysical Journal International, 169(1), 1-11, https://doi.org/10.1111/j.1365-246X.2007.03214.x
Balmino, G; Vales, N; Bonvalot, S; Briais, Anne (2012): Spherical harmonic modelling to ultra-high degree of Bouguer and isostatic anomalies. Journal of Geodesy, 86(7), 499-520, https://doi.org/10.1007/s00190-011-0533-4
Behn, Mark D; Conrad, Clinton P; Silver, Paul G (2004): Detection of upper mantle flow associated with the African Superplume. Earth and Planetary Science Letters, 224(3-4), 259-274, https://doi.org/10.1016/j.epsl.2004.05.026
Bonvalot, S; Balmino, G; Briais, Anne; Kuhn, M; Peyrefitte, A; Vales, N; Biancale, Richard; Gabalda, G; Reinquin, F; Sarrailh, M (2012): World Gravity Map. Commission for the Geological Map of the World. Eds. BGI-CGMW-CNES-IRD, Paris
Conrad, Clinton P; Behn, Mark D (2010): Constraints on lithosphere net rotation and asthenospheric viscosity from global mantle flow models and seismic anisotropy. Geochemistry, Geophysics, Geosystems, 11(5), 2009GC002970, https://doi.org/10.1029/2009GC002970
Conrad, Clinton P; Behn, Mark D; Silver, Paul G (2007): Global mantle flow and the development of seismic anisotropy: Differences between the oceanic and continental upper mantle. Journal of Geophysical Research: Solid Earth, 112(B7), 2006JB004608, https://doi.org/10.1029/2006JB004608
Laske, Gabi; Ma, Zhitu; Masters, Guy; Pasyanos, Mike: CRUST 1.0: a new Global Crustal Model at 1x1 degrees.
Ritsema, Jeroen; Nyblade, Andrew A; Owens, Thomas J; Langston, Charles A; VanDecar, John C (1998): Upper mantle seismic velocity structure beneath Tanzania, east Africa: Implications for the stability of cratonic lithosphere. Journal of Geophysical Research: Solid Earth, 103(B9), 21201-21213, https://doi.org/10.1029/98JB01274
Uieda, Leonardo; Barbosa, Valéria C F (2017): Fast nonlinear gravity inversion in spherical coordinates with application to the South American Moho. Geophysical Journal International, 208(1), 162-176, https://doi.org/10.1093/gji/ggw390
Uieda, Leonardo; Barbosa, Valéria C F; Braitenberg, Carla (2016): Tesseroids: Forward-modeling gravitational fields in spherical coordinates. Geophysics, 81(5), F41-F48, https://doi.org/10.1190/geo2015-0204.1
Coverage:
Median Latitude: -8.500000 * Median Longitude: 32.000000 * South-bound Latitude: -10.000000 * West-bound Longitude: 30.000000 * North-bound Latitude: -7.000000 * East-bound Longitude: 34.000000
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | LONGITUDE | Longitude | Njinju, Emmanuel A | Geocode | ||
| 2 | LATITUDE | Latitude | Njinju, Emmanuel A | Geocode | ||
| 3 | Bouguer anomaly | Bouguer | mGal | Njinju, Emmanuel A | see reference(s) | Bouguer GRAVITY WGM2012 |
| 4 | Thickness | Thick | m | Njinju, Emmanuel A | see reference(s) | Sediment Thicknes |
| 5 | Mohorovicic Discontinuity depth | Depth Moho | km | Njinju, Emmanuel A | see reference(s) | |
| 6 | Gravity | Gravity | mGal | Njinju, Emmanuel A | see reference(s) | Mantle Gravity |
| 7 | Gravity | Gravity | mGal | Njinju, Emmanuel A | see reference(s) | Sediment Gravity Effect |
| 8 | Gravity | Gravity | mGal | Njinju, Emmanuel A | see reference(s) | Gravity Effect of Deep Mantle and Sediments |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
66066 data points
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