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- W1489779749 abstract "Aeromagnetic data over the Lake Clark Fault reveal a north-trending band of magnetic anomalies that are right-laterally offset about 26 km across the fault. The magnetic anomalies correlate spatially with a belt of dated 34-39-Ma granitic plutons. Thus, the Lake Clark Fault has had ~26 km of right-lateral offset in the past 34-39 Ma. The Castle Mountain Fault, which lies along the strike of the Lake Clark Fault to the east-northeast, must have had a similar or, possibly, greater amount of offset. We infer the presence of an additional right-lateral strike-slip fault about 35 km northwest of the Lake Clark Fault, herein named the 'Telequana Fault,' on the basis of 11 km of right-lateral offset of a north-trending band of magnetic anomalies." @default.
- W1489779749 created "2016-06-24" @default.
- W1489779749 creator A5061346924 @default.
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- W1489779749 date "2005-01-01" @default.
- W1489779749 modified "2023-09-27" @default.
- W1489779749 title "26 km of offset on the Lake Clark fault since late Eocene time" @default.
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- W1489779749 doi "https://doi.org/10.3133/pp1709a" @default.
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