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Holocene and Latest Pleistocene Oblique Dextral Faulting on the Southern Inyo Mountains Fault, Owens Lake Basin, California

¹ Desert Research Institute
2215 Raggio Parkway
Reno, Nevada 89512
sbacon{at}dri.edu
 (S.N.B.)

² U.S. Geological Survey
3000 East Line Street
Bishop, California 93514
ajayko{at}usgs.gov
 (A.S.J.)

³ U.S. Geological Survey
MS 926A National Center
Reston, Virginia 20192
mcgeehin{at}usgs.gov
 (J.P.M.)

The Inyo Mountains fault (IMF) is a more or less continuous range-front fault system, with discontinuous late Quaternary activity, at the western base of the Inyo Mountains in Owens Valley, California. The southern section of the IMF trends N20°–40° W for at least 12 km at the base of and within the range front near Keeler in Owens Lake basin. The southern IMF cuts across a relict early Pliocene alluvial fan complex, which has formed shutter ridges and northeast-facing scarps, and which has dextrally offset, well-developed drainages indicating long-term activity. Numerous fault scarps along the mapped trace are northeast-facing, mountain-side down, and developed in both bedrock and younger alluvium, indicating latest Quaternary activity. Latest Quaternary multiple- and single-event scarps that cut alluvium range in height from 0.5 to 3.0 m. The penultimate event on the southern IMF is bracketed between 13,310 and 10,590 cal years B.P., based on radiocarbon dates from faulted alluvium and fissure-fill stratigraphy exposed in a natural wash cut. Evidence of the most recent event is found at many sites along the mapped fault, and, in particular, is seen in an 0.5-m northeast-facing scarp and several right-stepping en echelon 0.5-m-deep depressions that pond fine sediment on a younger than 13,310 cal years B.P. alluvial fan. A channel that crosses transverse to this scarp is dextrally offset 2.3 ± 0.8 m, providing a poorly constrained oblique slip rate of 0.1–0.3 m/k.y. The identified tectonic geomorphology and sense of displacement demonstrate that the southern IMF accommodates predominately dextral slip and should be integrated into kinematic fault models of strain distribution in Owens Valley.

This article has been cited by other articles:

				A.S. Jayko and S.N. Bacon Late Quaternary MIS 6-8 shoreline features of pluvial Owens Lake, Owens Valley, eastern California Geological Society of America Special Papers, January 1, 2008; 439(0): 185 - 206. [Abstract] [Full Text] [PDF]

				S. N. Bacon and S. K. Pezzopane A 25,000-year record of earthquakes on the Owens Valley fault near Lone Pine, California: Implications for recurrence intervals, slip rates, and segmentation models Geological Society of America Bulletin, July 1, 2007; 119(7-8): 823 - 847. [Abstract] [Full Text] [PDF]