Published Jun 6, 2023 by Utah State University Understanding the restless fault's mantle-to-crust connections provides critical information for understanding the lithospheric-scale fault's seismic cycle, says Newell, associate professor in USU's Department of Geosciences.
He and colleagues Jeff Benowitz, an Alaska-based geochronologist, Sean Regan of the University of Alaska Fairbanks, and doctoral candidate Coleman Hiett of USU, collected and analyzed helium and carbon isotopic data from springs along a nearly 250-mile segment of the fault and published their findings, "Roadblocks and Speed Limits: Mantle-to-Surface Volatile Flux in the Lithospheric Scale Denali Fault, Alaska," in Geology.
"Active strike-slip faults like Denali have three-dimensional geometries with possible deep conduit connections below the Earth's surface," Newell says. "But we don't know much about how and if these connections are maintained."
To examine these possible deep connections, Newell and Regan sampled 12 springs along the Denali and Totschunda Faults, by way of helicopter and on foot, to the remote, mountainous regions of Alaska's interior.
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