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3D geological models attempt to integrate all sources of geological and geophys ical data into a single
comprehensive model whose purpose is to help identify future poss ible mineral exploration targets. These
models are normally built based on sparse surface outcrops, a few boreholes and sometimes airborne
geophysical surveys to fill the gap. However, often the resulting geophysical models appear inadequate
because of a lack of phys ical property measurements, problems in contact definition and source depth
estimat ion caused by the interference of signals from overlapping sources, non-vertical geological contacts,
and the inherent non-uniqueness of unconstrained geophysical models. A combination of algorithms
involving edge mapping and strike and dip determination of geological contacts by means of using both
geophysical and topographic data represents a first step toward the construction of a set of constraints that
can be utilized for the actual 3D geologica l model. However all these algorithms and models need to be
tested on areas where we…TOBECONT’D…
William Morris
Wallbridge
Earth science
McMaster University
Globalink Research Award
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