By William R. Dickinson
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Extra info for Kinematics of Transrotational Tectonism in the California Transverse Ranges and Its Contribution to Cumulative Slip Along the San Andreas Transform
1990). This rate of shortening, if operative since 4–5 Ma, could account for a significant fraction of the component of Refugio–Santa Cruz shear inferred to have contributed to Hosgri movement. Moreover, the array of west-northwest–east-southeast splay faults, lying due north of the Refugio–Santa Cruz domain within the Santa Maria basin (Fig. 9), trend toward offshore junctures with the Hosgri fault (Steritz and Luyendyk, 1994), and could also account for the transfer of a significant proportion of the calculated shear to strike slip along the latter structure (Hall, 1981).
And Yerkes, R. , 1989, A cross section of the Los Angeles area: Seismically active fold and thrust belt, the 1987 Whittier Narrows earthquake, and earthquake hazard: Journal of Geophysical Research, v. 94, p. 9644–9664. , Gordon, R. , and Argus, D. , 1987, A revised estimate of Pacific–North America motion and implications for western North America plate boundary zone tectonics: Geophysical Research Letters, v. 14, p. 911–914. , Gordon, R. , Argus, D. , 1990, Current plate motions: Geophysical Journal International, v.
Hall, C. , 1981, San Luis Obispo transform fault and Middle Miocene rotation of the western Transverse Ranges, California: Journal of Geophysical Research, v. 86, p. 1015–1031. Hall, C. , 1991, Geology of the Point Sur-Lopez Point region, Coast Ranges, California: A part of the southern California allochthon: Geological Society of America Special Paper 266, 40 p. Hall, C. , and Corbato, C. , 1967, Stratigraphy and structure of Mesozoic and Cenozoic rocks, Nipomo quadrangle, southern Coast Ranges, California: Geological Society of America Bulletin, v.
Kinematics of Transrotational Tectonism in the California Transverse Ranges and Its Contribution to Cumulative Slip Along the San Andreas Transform by William R. Dickinson