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Title: Thrust belt geometry in the central Carolina slate belt North Carolina

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6319817

Newly recognized eastward-directed thrust faults and associated folds and cleavage constitute a major structural element in the central Carolina slate belt near Albemarle, North Carolina. At least two northwest-trending imbricate thrusts occur in a 10 km wide zone that trends 30 km along a northeast strike. Reconnaissance mapping suggests the presence of faults with similar style towards the west of this zone. Rocks directly involved in the thrust include the deep water rhythmites of the Tillery Formation that act as surface of detachment, and, also, a mafic rock that previously was mapped as a gabbro sill. Other field evidence documenting the thrusts includes: drag folds with a pronounced axial planar cleavage that parallels the faults; ramp areas with characteristic rootless folds; dragging of an earlier cleavage into fault surfaces; shear zones and kink bands with the same sense of movement as the thrusts. Axial planar cleavage results in part from pressure solution. The intensity of cleavage and the relative overall strain of the rocks increases from west to east across the thrust zone and suggests that thrusting progressed by successive propogation of footwall faults. Systematic and regular changes in the ratio of Bouma sequence intervals ((A+B+C+D)/E) show a marked discontinuity at the faults and suggest relative horizontal displacements of up to 14 km. Reconnaissance work suggests that the thrust may pre-date but are not younger than the regional low grade metamorphism.

Research Organization:
Univ. North Carolina, Wilmington (USA)
OSTI ID:
6319817
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