William R. Dickinson, Brian P. Wernicke; Reconciliation of San Andreas slip discrepancy by a combination of interior Basin and Range extension and transrotation near the coast. Geology ; 25 (7): 663–665. doi: https://doi.org/10.1130/0091-7613(1997)025<0663:ROSASD>2.3.CO;2
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Measurements of net translation along the Neogene San Andreas transform boundary between Pacific and North American plates, as indicated by the global correlation of sea-floor magnetic anomalies and by total Neogene displacements along strands of the onshore San Andreas fault system, differ by hundreds of kilometres. The apparent motion discrepancy is reconciled for post–mid-Miocene time if both transrotational deformation along the coastal belt of California and basin-range extension east of the Sierra Nevada are taken into account.