Strain accumulation and rotation in the Eastern California Shear Zone

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Abstract
Although the Eastern California Shear Zone (ECSZ) (strike ∼N25°W) does not quite coincide with a small circle drawn about the Pacific‐North America pole of rotation, trilateration and GPS measurements demonstrate that the motion within the zone corresponds to right‐lateral simple shear across a vertical plane (strike N33°W±5°) roughly parallel to the tangent to that local small circle (strike ∼N40°W). If the simple shear is released by slip on faults subparallel to the shear zone, the accumulated rotation is also released, leaving no secular rotation. South of the Garlock fault the principal faults (e.g., Calico‐Blackwater fault) strike ∼N40°W, close enough to the strike of the vertical plane across which maximum right‐lateral shear accumulates to almost wholly accommodate that accumulation of both strain and rotation by right‐lateral slip. North of the Garlock fault dip slip as well as strike slip on the principal faults (strike ∼N20°W) is required to accommodate the simple shear accumulation. In both cases the accumulated rotation is released with the shear strain. The Garlock fault, which transects the ECSZ, is not offset by north‐northwest striking faults nor, despite geological evidence for long‐term left‐lateral slip, does it appear at the present time to be accumulating left‐lateral simple shear strain across the fault due to slip at depth. Rather the motion is explained by right‐lateral simple shear across the orthogonal ECSZ. Left‐lateral slip on the Garlock fault will release the shear strain accumulating there but would augment the accumulating rotation, resulting in a secular clockwise rotation rate ∼80 nrad yr−1 (4.6° Myr−1).