High-pressure amphibolite facies dynamic metamorphism and the Mesozoic tectonic evolution of an ancient continental margin, east- central Alaska

Cynthia Dusel-Bacon; V. L. Hansen; J.A. Scala

doi:10.1111/j.1525-1314.1995.tb00202.x

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High-pressure amphibolite facies dynamic metamorphism and the Mesozoic tectonic evolution of an ancient continental margin, east- central Alaska

Cynthia Dusel-Bacon·V. L. Hansen·J.A. Scala

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Abstract

Ductilely deformed amphibolite facies tectonites comprise two adjacent terranes in east-central Alaska: the northern, structurally higher Taylor Mountain terrane and the southern, structurally lower Lake George subterrane of the Yukon-Tanana terrane. The pressure, temperature, kinematic and age data are interpreted to indicate that the metamorphism of the Taylor Mountain terrane and Lake George subterrane took place during different phases of a latest Palaeozoic through early Mesozoic shortening episode resulting from closure of an ocean basin now represented by klippen of the Seventymile-Slide Mountain terrane. High- to intermediate-pressure metamorphism of the Taylor Mountain terrane took place within a SW-dipping (present-day coordinates) subduction system. High- to intermediate-pressure metamorphism of the Lake George subterrane and the structural contact zone occurred during NW-directed overthrusting of the Taylor Mountain, Seventymile-Slide Mountain and Nisutlin terranes, and imbrication of the continental margin in Jurassic time. -from Authors

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Journal of Metamorphic Geology Article

Source-reported bounding extent: 61.14323525084058° to 66.47820814385636° latitude; -153.10546875° to -140.9765625° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Cynthia Dusel-Bacon, V. L. Hansen, J.A. Scala. 2007-05-05. High-pressure amphibolite facies dynamic metamorphism and the Mesozoic tectonic evolution of an ancient continental margin, east- central Alaska. https://doi.org/10.1111/j.1525-1314.1995.tb00202.x

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