SEDIMENTOLOGICAL ANALYSIS OF VOLTA BASIN ROCKS IN THE BUILSA SOUTH DISTRICT (UPPER EAST) AND MAMPRUGU-MOAGDURI DISTRICT (NORTH EAST) RESPECTIVELY IN GHANA
ABSTRACT
SEDIMENTOLOGICAL ANALYSIS OF VOLTA BASIN ROCKS IN THE BUILSA SOUTH DISTRICT (UPPER EAST) AND MAMPRUGU-MOAGDURI DISTRICT (NORTH EAST) RESPECTIVELY IN GHANA
Journal: Earth Sciences Pakistan (ESP)
Author: Emmanuel Owusu-Budu, Matthew Coffie Wilson,Chiri Godfrey Amedjoe, Emmanuel Mensah
This is an open access article distributed under the Creative Commons Attribution License CC BY 4.0, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited
Doi: 10.26480/esp.01.2024.75.83
Geological field mapping was conducted in the Builsa South District in the Upper-East Region (Field Sheet 1002D1) and the Mamprugu-Moagduri District in the North-East Region of Ghana (Field Sheet 1002D3), with rock samples taken for geochemical and petrographic studies to investigate mineralogical composition, texture, and microstructures in the rocks; the Kwahu/Bombouaka Group, the oldest sequence, unconformably overlies the Birimian basement complex rocks and is itself unconformably overlain by sediments forming the Oti Group, with the Yabraso Sandstone Formation as the only member of the Kwahu/Bombouaka Group and the Bimbila Formation as the only constituent of the Oti Group; eight sedimentary facies were identified based on lithological characteristics in the outcrops, with three (F1, F2, F3) belonging to the Yabraso Formation and five (F4, F5, F6, F7, F8) belonging to the Bimbila Formation, where the Yabraso Sandstone Formation exhibits a fining-upward sequence and is classified as quartz arenites with a few samples plotting as sub-arkose based on Folk’s (1974) classification, while the Bimbila Formation is stratigraphically divided into four units, from oldest to youngest: Bimbila limestones, weakly micaceous siltstones and mudstones, Bimbila sandstones, and Bimbila silexites.
| Pages | 75-83 |
| Year | 2024 |
| Issue | 1 |
| Volume | 8 |


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