http://www.tandfonline.com/doi/abs/10.1080/00206814.2013.817520
Williams 2013
The Late and Early Cretaceous clastics onlap the Sierra Batholith from W to E. The reconstruction is from seismic and sub surface wells. The western area (not shown on this section) has been post depositionally uplifted and is sub cropped or preserved as a thick deep water marginal marine sequence. Each time slice has the same overall fore-arc form but the details of deposition vary due to onlap position, paleo structure and as Williams highlights in his paper, post depositional incision (the Williams Canyon fill).
I await your scholastic response.
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