Research Paper GEOSPHERE The Tahoe-Sierra frontal fault zone, Emerald Bay area, Lake Tahoe, California: History, displacements, and rates 1 2 1 3 4 4 GEOSPHERE, v. 15, no. 3 R.A. Schweickert , J.G. Moore , M.M. Lahren , W. Kortemeier , C. Kitts , and T. Adamek 1Department of Geological Sciences, MS 172, University of Nevada, Reno, Nevada 89557, USA 2U.S. Geological Survey, MS 910, Menlo Park, California 94025, USA https://doi.org/10.1130/GES02022.1 3Western Nevada College, 2201 West College Parkway, Carson City, Nevada 89703, USA 4Robotic Systems Laboratory, Santa Clara University, 500 El Camino Real, Santa Clara, California 95053, USA 18 figures; 3 tables; 1 set of supplemental files CORRESPONDENCE:
[email protected] ABSTRACT zones along the eastern edge of the Sierra Nevada microplate. The Lake Tahoe basin (Figs. 1A and 1B), a complex half-graben, is part of the Walker Lane belt, CITATION: Schweickert, R.A., Moore, J.G., Lahren, M.M., Kortemeier, W., Kitts, C., and Adamek, T., 2019, The location and geometry of the boundary between the Sierra Nevada possibly an incipient plate boundary, and a region of dextral transtensional de- The Tahoe-Sierra frontal fault zone, Emerald Bay area, microplate and the transtensional Walker Lane belt of the Basin and Range formation between the internally unfaulted Sierra Nevada and the extensional Lake Tahoe, California: History, displacements, and Province in the Lake Tahoe area have been debated. Two options are that Basin and Range Province to the east. Numerous studies in the Walker Lane belt rates: Geosphere, v. 15, no. 3, p. 783–819, https://doi .org /10.1130 /GES02022.1.