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New York-Alabama Lineament : ウィキペディア英語版 | New York-Alabama Lineament 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 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. The fault zone has been associated with the Eastern Tennessee Seismic Zone. ==References==
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「New York-Alabama Lineament」の詳細全文を読む
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