ANALYSIS OF A REGIONAL MIDDLE PALEOZOIC UNCONFORMITY ALONG THE DISTALSOUTHEASTERN LAURENTIAN MARGIN, SOUTHERNMOST APPALACHIANS - IMPLICATIONS FOR TECTONIC EVOLUTION
Jf. Tull, ANALYSIS OF A REGIONAL MIDDLE PALEOZOIC UNCONFORMITY ALONG THE DISTALSOUTHEASTERN LAURENTIAN MARGIN, SOUTHERNMOST APPALACHIANS - IMPLICATIONS FOR TECTONIC EVOLUTION, Geological Society of America bulletin, 110(9), 1998, pp. 1149-1162
The highly allochthonous Talladega belt in the southernmost Appalachia
n orogen of Alabama and Georgia represents the most completely preserv
ed outboard fragment of the early Paleozoic Laurentian continental mar
gin in this part of the orogen. Palinspastic restoration indicates tha
t this Alleghanian thrust sheet was originally located at or near this
continental margin. The Talladega belt is within a structural recess
(Alabama recess) in the orogen, which is interpreted to have originate
d as a continental promontory during the opening and initial closing o
f the Iapetus ocean. Because continental promontories protrude oceanwa
rd along a continental margin, any significant early deformation of th
is margin should be recorded within this thrust sheet. Regional geolog
ic mapping has revealed a middle Paleozoic regional unconformity withi
n this belt, and distortion of this unconformity by late Paleozoic reg
ional folding provides for examination of subcrop geometries below the
unconformity over a large area (similar to 640 km(2)). Retrodeformati
on of the late Paleozoic folds indicates that only very mild deformati
on predated the unconformity. The origin of this early deformation is
unclear. Possibilities include very mild contractional deformation dur
ing the Taconic orogeny, or folding associated,vith wrench or extensio
nal faulting during Silurian(?)-Devonian Acadian successor-basin forma
tion. If the latter is the case, then no vestiges of Taconic deformati
on can be found in this outboard fragment of the margin, implying that
a major continental promontory at the southwesternmost Laurentian mar
gin may have escaped any significant effects of this orogeny.