REEVALUATING THE CHARLOTTE AND CAROLINA TERRANE BOUNDARY: BEDROCK MAPPING,GEOCHEMICAL ANALYSES, AND U/PB AGE-DATING IN THE GREENSBORO 100K
The McLeansville area, along with parts of Greensboro, offers a key setting to study island arc accretion to Laurentia during Appalachian Mountain formation. This is essential for understanding regional rock types, deformation, and mineral resource potential. Field investigations identified major lithologic units and structural fabrics, and samples were collected for laboratory analysis to interpret original geologic processes.
Preliminary results suggest lithologies are inconsistent with established Carolina or Charlotte terrane characteristics. Notable outcrops near the ultramafic body feature amphiboles resembling amphibolite facies rocks of the Charlotte terrane. The dominant felsic unit of the Greensboro Intrusive Suite was confirmed, but scattered mafic rocks suggest additional ultramafic bodies or mafic dikes. Some felsic lithologies have unusual quartz- and feldspar-rich compositions. Evidence of foliation in several outcrops provides critical insights into the extent of deformation in the region.
This work emphasizes the value of field mapping and petrologic analysis in understanding terrane boundaries and tectonic evolution in the southeastern Appalachians, guiding future geologic and economic exploration.