Kinematics of the southern Alaska constrained by westward-decreasing post-glacial slip-rates on the Denali fault, Alaska.

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ADS bibcode: 2004AGUFM.G13C..07M
year: 2004
Listed Authors: Meriaux, A.; Sieh, K.; Rubin, C. M.; Ryerson, F. J.; Finkel, R. C.; Meltzner, A.; Taylor, M.
Listed Institutions: Institute of Geophysics and Planetary Physics, Lawrence Livermore National Laboratory, P.O. Box 808, L-206, Livermore, CA 94550 United States; Division of Geologic and Planetary Science, California Institute of Technology, MC 170-25 1200 E. California Blvd, Pasadena, CA 91125 United States; Department of Geological Sciences, Central Washington University, 400 University Way, Ellensburg, WA 98926 United States; Institute of Geophysics and Planetary Physics, Lawrence Livermore National Laboratory, P.O. Box 808, L-206, Livermore, CA 94550 United States; Institute of Geophysics and Planetary Physics, Lawrence Livermore National Laboratory, P.O. Box 808, L-206, Livermore, CA 94550 United States; Division of Geologic and Planetary Science, California Institute of Technology, MC 170-25 1200 E. California Blvd, Pasadena, CA 91125 United States; Division of Geologic and Planetary Science, California Institute of Technology, MC 170-25 1200 E. California Blvd, Pasadena, CA 91125 United States

Kinematics of the southern Alaska constrained by westward-decreasing post-glacial slip-rates on the Denali fault, Alaska.

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