INTEGRATED FIELD GEOLOGY AND AIRBORNE GEOPHYSICAL STUDY OF THE ST. ALBAN’S AREA, NEWFOUNDLAND APPALACHIANS, CANADA: EXPLORATION POTENTIAL
The Day Cove Thrust, an easily recognized magnetic low, separates the volcano-sedimentary sequences of the Ordovician Baie d'Espoir Group (Dunnage Zone) from the Little Passage Gneiss (Gander Zone). Alternating stratigraphic units in the Baie d’Espoir Group are expressed as banded patterns within both the residual magnetic field and the first vertical derivative of the magnetic field. Silurian and Devonian granitoids, which have intruded rocks of both Gander and Dunnage zones, are readily distinguished based upon their magnetic and radiometric expressions. Areas showing magnetic patterns not explained by previous geological mapping, were specifically targeted during bedrock mapping, and included in lithogeochemical and U-Pb geochronological studies as part of this project. New exploration targets from this study having high gold contents (with up to 7 ppm Au in a grab sample at Southeast Brook) are associated with local magnetic lows. These targets are underlain by sandstone and conglomerate, potentially more permeable to mineralizing fluids compared to surrounding shales with higher magnetic signatures.
The study demonstrates how the combination of a detailed airborne geophysical survey, along with bedrock mapping and rock sampling, can refine geological mapping and guide future exploration efforts. An additional airborne geophysical survey was recently completed to the north and northeast of the St. Alban’s map area to continue this work in those areas equally prospective for mineral exploration.