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.
Click here for original story, Bubble, bubble, more earthquake trouble? Geoscientists study Alaska’s Denali fault
Source: ScienceDaily