ERRATUM: Spatiotemporally heterogeneous deformation, indirect tectonomagmatic links, and lithospheric evolution during orogenic activity coeval with an arc flare-up, (Geosphere (2022), 18(6), (1752–1782), (10.1130/GES02478.1))

Abstract

ORIGINAL ARTICLE: 2022, v. 18, no. 6, p. 1752–1782, https://doi.org/10.1130/GES02478.1. First published 23 September 2022. ERRATUM PUBLICATION: 2022, v. 18, no. 6, p. 1974–1975, https://doi.org/10.1130/GES02478e.1. First published 4 November 2022. In Figure 5, two field photos of notable outcrops are missing due to a conversion error. The corrected figure follows.[Figure Presented]. Figure 5. Bedrock geology of the Bench Canyon shear zone. Geology and ages are modified from Huber and Rinehart (1965), Peck (1980), Stern et al. (1981), Bateman et al. (1983), Fiske and Tobisch (1994), McNulty (1995), Memeti et al. (2010a), Frazer et al. (2014), Tomek et al. (2017), and Attia et al. (2020). Coordinates are Universal Transverse Mercator (in meters) in North American Datum of 1927, zone 11. New mapping presented herein focused on the central portion of the shear zone and surrounding metamorphic strata, south of the Red Devil Lake granodiorite. Structural measurements are given in dip and dip direction on stereonets. Number of measurements of each type plotted on the stereonets and used to calculate average orientations given in parentheses. All data given in these stereonets are new data collected in the field during mapping.