Gravity Evidence for a Larger Limpopo Belt in Southern Africa and Geodynamic Implications

R.T. Ranganai; A.B. Kampunzu; E.A. Atekwana; B.K. Paya; J.G. King; D.I. Koosimile; E.H. Stettler

doi:10.3997/2214-4609-pdb.143.19.2

Gravity Evidence for a Larger Limpopo Belt in Southern Africa and Geodynamic Implications
By R.T. Ranganai, A.B. Kampunzu, E.A. Atekwana, B.K. Paya, J.G. King, D.I. Koosimile and E.H. Stettler
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 7th SAGA Biennial Technical Meeting and Exhibition, Oct 2001, cp-143-00076
DOI: https://doi.org/10.3997/2214-4609-pdb.143.19.2

Abstract

The Limpopo Belt of southern Africa is the oldest and best documented Archaean orogenic belt around the<br>world. Various contentious models have been used to explain the tectonic evolution and present structure of<br>the Belt: ensialic deformation, subduction and continental collision, mantle recycling, and terrane accretion<br>(e.g., Holzer et al., 1999).

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2001-10-09

2024-04-27

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Gravity Evidence for a Larger Limpopo Belt in Southern Africa and Geodynamic Implications

Abstract

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Laboratory measurements of guided‐wave propagation within a fluid‐saturated fracture