Geochemists report findings from collected and analyzed helium and carbon isotopic data from springs along a nearly 250-mile segment of Alaska s Denali Fault. The fault s mantle fluid flow rates, they report, fall in the range observed for the world s other major and active strike-slip faults that form plate boundaries.
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Utah State University geochemists Dennis Newell and Coleman Hiett, Alaska-based geochronologist Jeff Benowitz, and University of Alaska Fairbanks Sean Regan report findings from collected and analyzed helium and carbon isotopic data from springs along a nearly 250-mile segment of Alaska's Denali Fault. The fault's mantle fluid flow rates, they report, fall in the range observed for the world's other major and active strike-slip faults that form plate boundaries.