The Slate Islands Impact Structure: Structural Interpretation and Age Constraints

Computer Science

Scientific paper

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Craters: Impact, Slate Islands, Terrace Zone, Uplift: Central

Scientific paper

The ~7-km-wide Slate Islands group, located in northern Lake Superior ~10 km south of Terrace Bay, Ontario, represents the heavily eroded central portion of a complex impact crater. Bathymetric data suggest an original crater diameter of ~32 km. Macroscopic and microscopic shock metamorphic features are common expressions within the Archean-to-Proterozoic igneous, metamorphic, and sedimentary target complex. Field studies conducted over the last two years reveal that the islands preserve not only the uplifted basement of the central structure, as previously recognized, but also allogenic breccia deposits of the original peripheral trough. Allogenic breccias are particularly prevalent along the eastern and northern island exposures. Heterogeneous melt bodies are located within heavily brecciated units of the central uplift. The intensely deformed structural trough and rim zone are evident on the N-S GLIMPCE reflection seismic line traversing the crater ~7 km to the west of the crater center. Currently available age constraints are weak but the apparent lack of post-Jacobsville clasts in the preserved breccia units suggests a Late Proterozoic-Early Paleozoic (800-500 Ma) age. Isotopic analyses of melt rocks, essential for refining the production age of this impact crater are currently underway.

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