EconPapers    
Economics at your fingertips  
 

SITE CHARACTERIZATION USING UPHOLE SEISMIC REFRACTION TECHNIQUE IN PINDIGA, GOMBE IN NIGERIA

Etim D. Uko (), Asaba A. Emmanuel and Olatunji S. Ayanninuola
Additional contact information
Etim D. Uko: Department of Physics, Rivers State University, PMB 5080, Port Harcourt, Nigeria
Asaba A. Emmanuel: Department of Physics, Nassarawa State University, PMB 1022, Keffi, Nigeria.
Olatunji S. Ayanninuola: Department of Physics, Nassarawa State University, PMB 1022, Keffi, Nigeria.

Earth Sciences Malaysia (ESMY), 2022, vol. 6, issue 1, 76-81

Abstract: Six uphole seismic refraction profiles were acquired in Pindiga Field, Gombe in Nigeria, using seismic uphole refraction method. The aim of the study was parameterize the site of lithology, near-surface stratigraphy, and velocity for geotechnical and velocity regimes for seismic data processing. The data was recorded using Stratavisor Model NZXP Recorders, processed and interpreted using OMNI, Petrel, Landmark, UDISYS, SeisUp, WavePack, Excel softwares. The results of the interpreted data reveal three-layer cases having dominant geologic lithologic sequences of sandstone, clay and silt, and intercalation of laterite, ironstone, coal and gravels up to a depth of 65m. The sand is an admixture of the various sizes but demarcation is based on the size as define by Wentworth scale of classification. In the First Weathered Layer, the velocity varies between 363ms-1 and 453ms-1 with an average of 391ms-1. In the Second Weathered Layer, the velocity varies between 702ms-1 and 870ms-1 with an average of 834ms-1. For the Third Weathered Layer, the velocity varies between 1012ms-1 and 2104ms-1 with an average of 1182ms-1. In the Consolidated Layer, the velocity varies between 1012ms-1 and 2104ms-1 with an average of 1182ms-1. Velocity regime varies between 1235ms-1 and 2500ms1 with an average of 1556ms-1. First Weathered Layer, the thickness varies between 2.6m and 4.7m with an average of 3.45m. Second Weathered Layer, the thickness varies between 0.9m and 41.5m with an average of 22.75m. Third Weathered Layer, the thickness varies between 12.5m and 45.9m with an average of 26.43m. The lithology, depth and velocity results of this work can be used to characterize a site, and also be applied in the processing of seismic reflection survey data.

Keywords: Weathered Layer; Uphole; Seismic; Refraction; Gombe; Nigeria (search for similar items in EconPapers)
Date: 2022
References: View references in EconPapers View complete reference list from CitEc
Citations:

Downloads: (external link)
https://earthsciencesmalaysia.com/archives/ESMY/1esmy2022/1esmy2022-76-81.pdf (application/pdf)

Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.

Export reference: BibTeX RIS (EndNote, ProCite, RefMan) HTML/Text

Persistent link: https://EconPapers.repec.org/RePEc:zib:zbesmy:v:6:y:2022:i:1:p:76-81

DOI: 10.26480/esmy.01.2022.76.81

Access Statistics for this article

Earth Sciences Malaysia (ESMY) is currently edited by Dr. Mohd Nadzri Md Reba

More articles in Earth Sciences Malaysia (ESMY) from Zibeline International Publishing
Bibliographic data for series maintained by Zibeline International Publishing ( this e-mail address is bad, please contact ).

 
Page updated 2025-03-20
Handle: RePEc:zib:zbesmy:v:6:y:2022:i:1:p:76-81