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In this book, you'll find the contribution of magnetometry to geological mapping in the case of the KAPONDA area in the Democratic Republic of Congo.We started with geological formations that were regionally undifferentiated, and by processing magnetometric data (the horizontal gradient on the reduced reduction data at the pole), we delineated these formations and highlighted senestial stalls.Magnetometry is thus an essential tool in geological mapping.
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In this book, you'll find the contribution of magnetometry to geological mapping in the case of the KAPONDA area in the Democratic Republic of Congo.We started with geological formations that were regionally undifferentiated, and by processing magnetometric data (the horizontal gradient on the reduced reduction data at the pole), we delineated these formations and highlighted senestial stalls.Magnetometry is thus an essential tool in geological mapping.