Detailed mapping of the Greenville 1[degree] x 2[degree] quadrangle has outlined the Paris Mountain thrust sheet, dominated by sillimanite-mica schist, biotite gneiss, and amphibolite. It overlies footwall biotite gneiss and sillimanite-mica schist of the Six Mile thrust sheet. Structural analysis of regional foliation patterns (i.e., warpings of the dominant metamorphic schistosity) indicates pervasive, broad, upright-inclined macroscopic folding of the Inner Piedmont rocks with half wavelengths of 9--15 km. These folds plunge northeast and east at shallow-moderate angles (4[degree]--44[degree]), post-dating emplacement of the Paris Mountain allochthon. At exposures near Enoree Church, folds of this generation have developed after an episode of tight, overturned folding of schistosity. The age of the macroscopic folding episode (Taconic , Alleghanian ) is unknown.
'/%3e%3c/defs%3e%3cpath fill='%23012169' d='M0 0h10080v5040H0z'/%3e%3cpath stroke='%23fff' stroke-width='.6' d='m0 0 6 3m0-3L0 3' clip-path='url(%23b)' transform='scale(840)'/%3e%3cpath stroke='%23e4002b' stroke-width='.4' d='m0 0 6 3m0-3L0 3' clip-path='url(%23c)' transform='scale(840)'/%3e%3cpath stroke='%23fff' stroke-width='840' d='M2520 0v2520M0 1260h5040'/%3e%3cpath stroke='%23e4002b' stroke-width='504' d='M2520 0v2520M0 1260h5040'/%3e%3cg fill='%23fff'%3e%3cuse xlink:href='%23d' x='2520' y='3780'/%3e%3cuse xlink:href='%23a' x='7560' y='4200'/%3e%3cuse xlink:href='%23a' x='6300' y='2205'/%3e%3cuse xlink:href='%23a' x='7560' y='840'/%3e%3cuse xlink:href='%23a' x='8680' y='1869'/%3e%3cuse xlink:href='%23e' x='8064' y='2730'/%3e%3c/g%3e%3c/svg%3e)
