Show simple item record

dc.contributor.author Laletsang, K.
dc.contributor.author Modisi, M.P.
dc.contributor.author Shemang, E.M.
dc.contributor.author Moffat, L.
dc.contributor.author Moagi, O.R.
dc.date.accessioned 2009-09-22T09:57:58Z
dc.date.available 2009-09-22T09:57:58Z
dc.date.issued 2007
dc.identifier.citation Laletsang, K. et al (2007) Shallow seismic refraction and magnetic studies at Lake Ngami, The Okavango Delta, Northwest Botswana, Journal of African Earth Sciences, Vol. 48, pp. 95–99 en_US
dc.identifier.issn 1464-343X
dc.identifier.uri http://hdl.handle.net/10311/376
dc.description.abstract A seismic refraction analysis was carried out on data acquired on an 8.5 km profile at Lake Ngami, NW Botswana, to determine the structure and stratigraphy underlying the lake. The seismic spread comprised a 48-channel seismograph with a 9.5 m receiver and source spacing. The seismic source comprised 10 hammer blows on an aluminum plate, from which a vertical stack was recorded. The data were processed with WinSismTM version 10 program using the intercept time method. A total field magnetic survey was also carried out along the same line. The seismic refraction profile shows a low velocity layer (400–1600 m/s) extending from the surface at the southern end of the line to a maximum depth of 30 m in the middle of the profile, returning to a depth of 20 m from 4.5 km to the northern end of the line. The low velocity layer consists of the unconsolidated sediments and is underlain by more compact and saturated material with seismic velocities of 1600–3600 m/s. This material is interpreted to comprise semi- to fully consolidated sandstone. The base of these sandstones, however, could only be mapped near the southern end of the line out to 2 km. High seismic velocity rocks (3600–5000 m/s), interpreted to be weathered to fresh basement, were mapped below the sandstones at the southern end of the line. The magnetic profile shows a high at the beginning of the line which progressively declines to a low at 3 km. The field strength increases rapidly over the next 1.5 km to reach a plateau level at 4.5 km. The magnetic high at the beginning of the line corresponds to shallow basement which is mapped in the refraction profile. The magnetic low at 3 km is indicative of a thickened sediment section at this location. The southern end of the line with high seismic velocities comprises basement rocks located in the footwall block of the Kunyere Border Fault of the Okavango Rift. The step-wise downthrown hanging wall block consists of the low to intermediate velocity basin deposits in the northern part of the profile. en_US
dc.language.iso en en_US
dc.publisher Elsevier www.elsevier.com/locate/jafrearsci en_US
dc.subject Lake Ngami en_US
dc.subject Okavango rift en_US
dc.subject Stratigraphy; Seismic velocity en_US
dc.subject Magnetic profile en_US
dc.title Shallow seismic refraction and magnetic studies at Lake Ngami, The Okavango Delta, Northwest Botswana en_US
dc.type Published Article en_US


Files in this item

This item appears in the following Collection(s)

Show simple item record

Search UBRISA


Advanced Search

Browse

My Account