USGS · 70186707
Deep structure and evolution of the Carolina Trough
Abstract
Multichannel seismic-reflection data together with two-dimensional gravity and magnetic models suggest that the crustal structure off North Carolina consists of normal continental crust landward of the Brunswick magnetic anomaly (BMA), rift-stage crust in the 80-km-wide zone between the BMA and the East Coast magnetic anomaly (ECMA), and normal oceanic crust seaward of the ECMA.
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D. R. Hutchinson, J. A. Grow, Kim D. Klitgord, B.A. Swift. 1982. Deep structure and evolution of the Carolina Trough. https://pubs.usgs.gov/publication/70186707
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