Franciscan Complex Calera limestones: accreted remnants of Farallon Plate oceanic plateaus

@article{Tarduno1985FranciscanCC,
  title={Franciscan Complex Calera limestones: accreted remnants of Farallon Plate oceanic plateaus},
  author={John A. Tarduno and Michael O. Mcwilliams and Michel G. Debiche and William V. Sliter and M. Clark Blake},
  journal={Nature},
  year={1985},
  volume={317},
  pages={345-347}
}
The Calera Limestone, part of the Franciscan Complex of northern California, may have formed in a palaeoenvironment similar to Hess and Shatsky Rises of the present north-west Pacific1. We report here new palaeomagnetic results, palaeontological data and recent plate-motion models that reinforce this assertion. The Calera Limestone may have formed on Farallon Plate plateaus, north of the Pacific–Farallon spreading centre as a counterpart to Hess or Shatsky Rises. In one model2, the plateaus… 
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