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- W345701811 abstract "Saddlebag Lake pendant provides an important window into the structural development of wallrocks of the Sierra Nevada batholith, and provides constraints on a number of regional tectonic events. Sixteen mappable stratigraphic units crop out within ten major thrust sheets. Stratigraphic cutoffs and estimated 35-degree average ramp angles yield minimum total thrust displacements of 25 km. Adding displacements required by flats, thickness variations among stratigraphic units, internal folds, and internal strains within thrust sheets yields an estimate of 50--60 km of shortening. Although only estimates, these figures indicate that a significant zone of Triassic and Jurassic( ) contractional deformation exists within the pendant, offering little support for extensional tectonic scenarios for Sierran wallrocks that have been proposed. In addition, map and structural relations preclude the existence of intrabatholithic breaks with proposed dextral displacements of up to 210 km, along the eastern edge of the pendant. The authors conclude that this part of the eastern Sierra experienced only the following tectonic events: (1) Antler deformation; (2) Permo-Triassic( ) Golconda thrusting; (3) large-magnitude Late Triassic thrusting during arc volcanism and plutonism; (4) Late Jurassic or Early Cretaceous east-vergent thrusting, folding, and cleavage development. Evidence also exists along the western edge of the pendantmore » for pre-90 Ma dextral shear following the above events. They infer that the latter event may signal development of the Mojave-Snow Lake fault west of Saddlebag Lake pendant.« less" @default.
- W345701811 created "2016-06-24" @default.
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- W345701811 date "1993-04-01" @default.
- W345701811 modified "2023-09-23" @default.
- W345701811 title "Structural development of Saddlebag Lake pendant, eastern Sierra Nevada, California: Implications for crustal evolution" @default.
- W345701811 hasPublicationYear "1993" @default.
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