Why is Denali (6,194 m) so big? Caught inside the tectonic wake of a migrating restraining bend

نویسندگان

چکیده

Abstract Topography along strike‐slip fault restraining bends is theoretically self‐limited by erosion, block translation and the expected abandonment of bends. However, Denali (6,194 m) Foraker (5,304 are located within a bend dextral Fault system. We reveal role evolution in mountain building with physical experiments scaled to simulate Alaska Mount McKinley (MMRB). Despite natural complexity MMRB, first‐order patterns (of separation rates, uplift lateral migration) from geologic data align experiments. Thermochronology, seismicity, slip rate show that persistence single strand through ~6 Ma MMRB facilitated simultaneous advection crust migration eastern vertex bend.

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ژورنال

عنوان ژورنال: Terra Nova

سال: 2021

ISSN: ['0954-4879', '1365-3121']

DOI: https://doi.org/10.1111/ter.12571