Earth:New York-Alabama Lineament
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Revision as of 17:28, 12 June 2021 by imported>Steve Marsio (fixing)
The New York-Alabama Lineament is a magnetic anomaly in the geology of eastern North America running from Alabama to New York. The lineament is defined by discontinuities in aeromagnetic measurements indicating an approximately 220-kilometre (140 mi) displacement of buried geologic structures along this line. The displacement is attributed to the presence of a deeply buried strike-slip fault, possibly dating to the general time of the Grenville orogeny. The lineament was first described in 1978.[1] The fault zone has been associated with the Eastern Tennessee Seismic Zone.[2]
References
- ↑ Steltenpohl, Mark G.; Zeitz, Isidore; Horton, J. Wright Jr.; Daniels, David L. (27 January 2010). "New York–Alabama lineament: A buried right-slip fault bordering the Appalachians and mid-continent North America". Geology 38 (6): 571–574. doi:10.1130/G30978.1.
- ↑ O'Hanlon, Larry (May 28, 2010). "San Andreas-like fault found in eastern U.S.". http://www.nbcnews.com/id/37407341. Retrieved 24 August 2011.
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