Link between ridge subduction and gold mineralization in southern Alaska

Peter J. Haeussler; Dwight Bradley; Richard Goldfarb; Lawrence W. Snee; Cliff D. Taylor

doi:10.1130/0091-7613(1995)023<0995:lbrsag>2.3.co;2

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Link between ridge subduction and gold mineralization in southern Alaska

Peter J. Haeussler·Dwight Bradley·Richard Goldfarb·Lawrence W. Snee·Cliff D. Taylor

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Abstract

40 Ar/ 39 Ar geochronology reveals that turbidite-hosted gold deposits in the southern Alaska accretionary prism are the same age as nearby near-trench plutons. These early Tertiary plutons and gold lodes formed above a slab window during subduction of an oceanic spreading center. Ridge subduction is a previously unrecognized tectonic process for the generation of lode gold.

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Geology Article

Source-reported bounding extent: 53.5° to 61.5° latitude; -163° to -135° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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BibTeX RIS

Peter J. Haeussler, Dwight Bradley, Richard Goldfarb, Lawrence W. Snee, Cliff D. Taylor. 1995. Link between ridge subduction and gold mineralization in southern Alaska. https://doi.org/10.1130/0091-7613(1995)023%3C0995%3Albrsag%3E2.3.co%3B2

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