Detrital Zircon Geochronology of Basal Cambrian Strata in the Deep Illinois Basin, USA: Evidence for the Paleoproterozoic-Cambrian Tectonic and Sedimentary Evolution of Central Laurentia

AbstractWe present 960 detrital zircon ages from three new, deep boreholes from the Illinois Basin, USA. These zircon age spectra reveal new details of the late Paleoproterozoic through early Cambrian tectonic history of the Illinois Basin, including evidence of the timing of the development of the Reelfoot Rift and breakup of Rodinia. The oldest detrital zircon population is ~1650 Ma, older than any known age for crystalline rocks from other deep drill cores in the basin and conspicuously absent in other Cambrian strata in the region. We interpret this population to have been derived from late Paleoproterozoic crust that exists beneath the Illinois Basin and was exposed during the deposition of Cambrian strata. The principal age peak is ~1375 Ma, characteristic of igneous rocks of the Southern Granite-Rhyolite Province but also present in the St. Francois Mountains of the Eastern Granite-Rhyolite Province (EGRP). A secondary peak of ~1460 Ma detrital zircon reflects the known ages of crystalline rocks th...