Linear, undulating paired magnetic highs and lows mark the edges of Triassic-Jurassic sills at the western edge of the Taoudeni Basin whose susceptibilities range from 15-33 x 10-3 SI (dolerites, micrograbbros, Excel spreadsheet). These anomalies cross broad wavelength positive anomalies presumably due to deeper sources (Fig. 23). Calculated depths to the top of magnetic basement (Fig. 11, Plate 3) range from ~20-400 m for the shallow sill sources and > 5000 m for the broad anomalies.
Figure 24. Close-up of crystalline basement map over the northern boundary between the Mauritanide belt (high frequency anomalies on west) and Archean BIF’s and Jurassic dikes (east) (box 24, Fig. 17, Plates 1 and 2). High frequency generally east-trending anomalies associated with the Mauritanide belt clearly truncate more northerly (NNW, NNE) trending anomalies of the Archean BIF’s and Jurassic dikes (Fig. 24). The anomalies within the Mauritanide belt most likely relate to slivers of ophiolite and or deformed BIF. Calculated depths to the top of magnetic basement (Fig. 11, Plate 3) range from ~100-900 m.
Figure 25. Close-up of crystalline basement map over Archean gneiss domes or BIF (linear and circular NNW trending highs) and greenstone belts (high amplitude lows) (box 25, Fig. 17, Plates 1 and 2). North-northwest trending bands of circular and linear magnetic highs embedded in high amplitude magnetic lows can be observed in the southern portion of the exposed Archean basement (Fig. 25). The sources of the highs are BIF’s (Fig. 1). The BIF’s are low in potassium (Fig. 12), Thorium (Fig. 13) and with moderate concentrations of Uranium (Fig. 14) so appear blue on the ternary radiometric map (Fig. 15, Plate 4). Linear anomalies related to younger (Cretaceous?) dikes cross these anomalies. Calculated depths to the top of magnetic basement (Fig. 11, Plate 1) range from ~150-700 m.