Synthesis of late Paleozoic and Mesozoic eolian deposits of the ...

pp. 71-74
46 °
41 °
36 °
31'=
117 ° 112 ° 107 ° 102 °
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+ 0 100 200 300 Km + ~ . . . . . . . + ~\ ,,,,J,. / +
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Fig. 33. Generalized Late Jurassic tectonic elements that influenced sedimentation of Morrison-age eolian deposits. Boundaries are approximate and varied through time.