THE ULTRAMAFIC BODIES OF SOUTHEASTERN PENNSYLVANIA: POSSIBLE DISMEMBERED LAYERED MAFIC INTRUSION
Most PA Piedmont ultramafic bodies are present along regional shear zones and four distinct styles of alteration have been identified: complete serpentinization, blackwall alteration, sheared blackwall alteration, and siliceous alteration. The westernmost bodies of the PA Piedmont exhibit complete serpentinization with textures and relict olivines suggesting an olivine-rich protolith. Bodies present in the eastern PA Piedmont mostly display blackwall alteration: some show orderly concentric zones of alteration, while others show significant shear deformation (unit duplication, strain shadows). When relict cores of the blackwalled bodies are present they reveal unaltered orthopyroxenite and norite lithologies with cumulate textures. Bodies with siliceous alteration show near complete replacement by quartz via contact metamorphism with adjacent granite intrusions. The southeastern Pennsylvania ultramafic bodies may represent a dismembered layered mafic complex from the base of an island arc that was sheared southward along dextral shear zones that widen from a central northern point, sending the dunite based to the west and the less ultramafic (higher stratigraphic units) orthopyroxenite and norite components more easterly.