A fundamental, and enigmatic, feature of the Northeast Iowa Intrusive Complex is a series of large circular- or horseshoe-shaped magnetic anomalies. Our research group has identified two to three hypotheses of what the geologic source of the anomalies may be. One possible interpretation is that these features are part of a Keweenawan (~1,100 Ma) mafic igneous complex. This has major implications for the regional geologic framework and mineral potential, since it would be the second largest known Midcontinent Rift-related igneous complex. However, the true geologic source can only be known through new drilling, which would give us a chance to directly determine the nature and age of these rocks.
We plan to drill a new borehole through Paleozoic cover to Proterozoic rocks in northeastern Iowa and recover core from the Proterozoic basement sufficient for petrologic and radiometric analyses. Our primary goal is to to test geophysical interpretations of the Proterozoic geology in the area. Our secondary goals are to obtain rarely-available data on the overlying Proterozic section, fluid characteristics, in-situ stress conditions, and thermal conditions at the Proterozoic-Paleozoic unconformity.
Crustal Geophysics and Geochemistry Science Center