APPALACHIAN GREAT GRAVITY GRADIENT: GEOLOGICAL EVIDENCE FOR ITS AGE AND ORIGIN
The Martic Thrust/Mine Ridge Region, at the SE edge of the Reading Prong slab, exposes the Cambrian cratonic edge imbricated by the Late Ordovician Taconian orogeny. It is a greatly displaced Early Paleozoic cratonic margin and its presumed gravity gradient cannot be the source of this gravity gradient 100+ km inland. Conceivably the local gradient could result from large displacement of the Moho by the Mesozoic Newark Basin’s border fault but the basin’s tilting and listric fault requirements preclude such interpretations. Absence of regional metamorphic effects excludes a related massive Mesozoic gabbroic intrusion. The GGG in this area is a Mid-Paleozoic feature. Locally, a Mid-Paleozoic very large dextral fault just SE of the GGG places a terrane of NY City Piedmont geology next to this region. This and many other Mid-Paleozoic circum-Rhreic Ocean processes are candidates for this density change to the Appl. Piedmont edge.
The Later-Paleozoic continental collision loaded and tilted that modified cratonic margin, detached its upper surface along the brittle-ductile transition, transported that slab up the ramp, and stranded it on the undisturbed craton just inboard of the GGG