Deep structure and evolution of the Carolina Trough
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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.
Suggested Citation
Hutchinson, D.R., Grow, J.A., Klitgord, K.D., and Swift, B., 1982, Deep structure and evolution of the Carolina Trough, chap. of Studies in continental margin geology, p. 129-152.
| Publication type | Book chapter |
|---|---|
| Publication Subtype | Book Chapter |
| Title | Deep structure and evolution of the Carolina Trough |
| Year Published | 1982 |
| Language | English |
| Publisher | American Association of Petroleum Geologists |
| Description | 24 p. |
| Larger Work Type | Book |
| Larger Work Subtype | Monograph |
| Larger Work Title | Studies in continental margin geology |
| First page | 129 |
| Last page | 152 |