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The bedrock of the study area is composed of quartz, biotite, muscovite, garnet, chlorite, sillimanite, K-feldspar (orthoclase and microcline), and plagioclase (Figure 3).
According to the regional geological data [2], the bedrock of the study area mainly consists of age-unknown gneisses and igneous rocks (anorthosite, diorite), Jurassic sedimentary rocks and Cretaceous igneous rocks (syenite, granodiorite, quartz porphyry, dykes).
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Since then, the tools that the new Nobel laureates developed have become bedrock for the study of so-called topological phases of matter perhaps the hottest field in condensed matter physics.
Dubbed the "DMP theory" in the economists' honor, it has become the bedrock for the study of labor markets and explains why people are sure to be out of work even when the number of vacant jobs equals the number of job seekers, so-called equilibrium unemployment.
These high demand for groundwater resource and the variability of its occurrence in basement terrains have made it mandatory to investigate the hydrogeological setting and to validate the groundwater yield of the basement aquifers across the various bedrock terrains of the study area within Ibarapa region of SW Nigeria.
Open image in new window Fig. 8 Bedrock iso-resistivity map of the study area.
Hence, qualitative method also involved generating the thickness map of the saprolite and the resistivity maps of both the bedrock and that of the former to classify groundwater prospect of the various bedrock terrains across the study area.
Open image in new window Fig. 9 Fractured bedrock locations on geological map of the study area.
The seismic velocity values, engineering, consolidation, and strength parameters show that the bedrock at northern and southern parts of the study area is characterized by less competent rock quality, while the central part is characterized by more competent rock quality.
Bedrock wells in the study area.
Finally, bedrock containing fluorine minerals is responsible for the high F− in the groundwater of the study area.
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