1957
DOI: 10.3133/ofr5733
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Total intensity aeromagnetic profiles of Bethel basin, Alaska

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1978
1978
1978
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“…In conclusion Approximately 10 km north of the north edge of the map on strike with the magnetic high:are a series of aeromagnetic profiles (nos. 5A, 6, 7, and 8) which cross the magnetic high (Dempsey, Meuschke, and Andreasen, 1957)* These profiles, show that the concealed causative rocks of the anomaly become progressively shallower to the.northeast and ultimately crop out at lines 7 and 8 as a restricted area (25 by 10 km) of magnetic schist and metacheirt inferred to be OrdovicianX?) to Devonian(?)…”
Section: Volcanic Rock (Tertiary)mentioning
confidence: 95%
“…In conclusion Approximately 10 km north of the north edge of the map on strike with the magnetic high:are a series of aeromagnetic profiles (nos. 5A, 6, 7, and 8) which cross the magnetic high (Dempsey, Meuschke, and Andreasen, 1957)* These profiles, show that the concealed causative rocks of the anomaly become progressively shallower to the.northeast and ultimately crop out at lines 7 and 8 as a restricted area (25 by 10 km) of magnetic schist and metacheirt inferred to be OrdovicianX?) to Devonian(?)…”
Section: Volcanic Rock (Tertiary)mentioning
confidence: 95%