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Title: 3-d structure of the Late Paleozoic suture beneath the Georgia coastal plain: evidence from new COCORP profiling

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6863451

New COCORP data collected on the Georgia coastal plain reveal a broad internally complex zone of basement reflections associated with the Brunswick magnetic low. This feature probably marks the late Paleozoic suture between North American and Africa. Multiple crossings of this feature provide information on its three-dimensional structure as well as its regional trend. The presumed suture consists of prominent bands of both arcuate and planar south-dipping reflections that extend from near the surface to the base of the crust (5-35 km), along with discrete apparently crosscutting northeast-dipping reflections. The dipping reflections in the deep crust extend downward to subhorizontal Moho reflections but do not penetrate through these reflections or offset them, suggesting that Moho is younger than the dipping fabric within the crust. In western Georgia the south-dipping reflections project upward toward metamorphosed and thrust-imbricated eugeoclinal strata exposed in the southernmost Piedmont, suggesting that they represent the downdip extension of that assemblage. The northeast-dipping reflections might represent south-vergent Paleozoic thrusts, Mesozoic normal faults, or both. In western Georgia the suture zone is relatively narrow (about 70 km wide). However, in eastern Georgia complex mid- and lower crustal reflections occur both beneath and to the north of the Brunswick anomaly, implying a broadened zone of crustal deformation.

Research Organization:
Cornell Univ., Ithaca, NY (USA)
OSTI ID:
6863451
Report Number(s):
CONF-8510489-
Journal Information:
Geol. Soc. Am., Abstr. Programs; (United States), Vol. 17; Conference: 98. annual meeting of the Geological Society of America, Orlando, FL, USA, 28 Oct 1985
Country of Publication:
United States
Language:
English