PETER ROBINSON’S IMPACT ON NEW ENGLAND AND APPALACHIAN GEOLOGY (Invited Presentation)
These principles have been employed in the southern Appalachians (APs) to build several islands of ground truth—detailed (quantitative, reproducible) GM—that laid the foundations for laboratory-driven research in modern petrology, geochemistry, structural geology, geophysics, and geochronology (GC). These islands have revealed major faults, suspect and exotic terranes (TERRs), and modern GC has yielded ages of plutons, faults/TERR boundaries, timing of metamorphism, provenance of TERRs from detrital zircons, which acquitted several that were previously suspect, and timing of orogenies.
These data, coupled with modern data from elsewhere in the AP orogen, have facilitated formulation of new tectonic models throughout the orogen that are internally more consistent with existing data. We now know that Gander terrane extends farther south through southern NE and effects of the Alleghanian orogeny were more widespread here than previously thought. Mid- Paleozoic westward subduction of Avalon beneath NE contrasts with opposite subduction polarity of Carolina subduction in the southern-central APs, requiring a previously unrecognized mid-Paleozoic transform at the NE-central APs junction (credit A. J. Merschat).