Utility of aeromagnetic studies for mapping of potentially active faults in two forearc basins : Puget Sound, Washington, and Cook Inlet, Alaska

High-resolution aeromagnetic surveys over forearc basins can detect faults and folds in weakly magnetized sediments, thus providing geologic constraints on tectonic evolution and improved understanding of seismic hazards in convergent-margin settings. Puget Sound, Washington, and Cook Inlet, Alaska,...

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Bibliographic Details
Published in:Earth, planets and space Vol. 57; no. 8; pp. 781 - 793
Main Authors: SALTUS, R. W, BLAKELY, R. J, HAEUSSLER, P. J, WELLS, R. E
Format: Conference Proceeding Journal Article
Language:English
Published: Tokyo Terra 01-01-2005
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Summary:High-resolution aeromagnetic surveys over forearc basins can detect faults and folds in weakly magnetized sediments, thus providing geologic constraints on tectonic evolution and improved understanding of seismic hazards in convergent-margin settings. Puget Sound, Washington, and Cook Inlet, Alaska, provide two case histories. In each lowland region, shallow-source magnetic anomalies are related to active folds and/or faults. Mapping these structures is critical for understanding seismic hazards that face the urban regions of Seattle, Washington, and Anchorage, Alaska. Similarities in aeromagnetic anomaly patterns and magnetic stratigraphy between the two regions suggest that we can expect the aeromagnetic method to yield useful structural information that may contribute to earth-hazard and energy resource investigations in other forearc basins.
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ISSN:1343-8832
1880-5981
1880-5981
DOI:10.1186/BF03351857