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Ocmulgee Fault

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Journal Article
Journal: Geology
Published: 01 May 1991
Geology (1991) 19 (5): 542–544.
Journal Article
Journal: Geology
Published: 01 August 1990
Geology (1990) 18 (8): 708–711.
...Robert J. Hooper; Robert D. Hatcher, Jr. Abstract The Ocmulgee fault is a fundamental boundary within the Piedmont of central Georgia separating North American, Piedmont terrane rocks from exotic rocks of the Avalon (Carolina) terrane. Contrasts in stratigraphy, metamorphic grade, and aeromagnetic...
Journal Article
Published: 01 July 1993
Canadian Journal of Earth Sciences (1993) 30 (7): 1297–1305.
... the western Piedmont décollement zone is coeval with orogen-parallel strike-slip faulting in the high-angle Ocmulgee fault in central Piedmont. These faults shape a shear zone system that probably formed at the boundary of the North American craton, in relation with a transpressional regime of deformation...
Image
Figure 10. Simplified interpretive drawing through the southern Appalachian...
Published: 01 May 2005
fault; OF—Ocmulgee fault. Dipping fault or shear zone is based on dipping reflection zone observed on Georgia lines 13 and 14 (Fig. 1A) .
Journal Article
Journal: GSA Bulletin
Published: 01 May 2005
GSA Bulletin (2005) 117 (5-6): 669–686.
... fault; OF—Ocmulgee fault. Dipping fault or shear zone is based on dipping reflection zone observed on Georgia lines 13 and 14 (Fig. 1A) . ...
FIGURES | View All (15)
Journal Article
Journal: Geosphere
Published: 01 February 2008
Geosphere (2008) 4 (1): 131–144.
..., the Motts Gneiss is sheared into the right-slip Goat Rock fault zone which formed during the late Carboniferous (ca. 288 Ma; Steltenpohl et al., 1992 ). The elongation lineation within both the Goat Rock fault zone and the Motts Gneiss is coaxial. Second, because the Motts Gneiss is similar in its...
FIGURES | View All (5)
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1967
AAPG Bulletin (1967) 51 (12): 2400–2429.
... Cretaceous deposits in the region are the nonmarine sand and clay beds of the Potomac Group. There is a conspicuous thickening of the Eocene north of the James River, a fact which made Cederstrom (1945c) postulate the presence of a fault. However, more work must be done before the existence of this fault...
FIGURES | View All (8)