Abstract
A recent study involving the use of seismic refraction and D.C. resistivity methods was carried out in the Barkumbo valley in Bauchi town. The results of the study revealed a general deepening of the central floor of the valley towards its northern and southern edges. A low depth-to-basement occurs northwards along some of the selected profiles. In addition, the margins of some of the profiles revealed a greater depths-to-basement. These areas appear to be parallel to the dominant fracture pattern (N-S and E-W) and are most likely related to it. Towards the southern end of the area, the high areas join to form a basin. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 47-51 |
| Number of pages | 5 |
| Journal | Journal of Mining & Geology |
| Volume | 29 |
| Issue number | 2 |
| Publication status | Published - 1993 |
All Science Journal Classification (ASJC) codes
- Water Science and Technology
- Geophysics
- Geology
- Economic Geology
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