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| | The San Andreas Fault System, California - Chapter 8 - References Cited (Site not responding. Last check: 2007-10-15) |
 | | The crust of much of California was formed at an Andean-type continental margin during the Mesozoic and early Cenozoic, and was modified by large strike-slip offsets along the San Andreas fault system during the late Cenozoic. |
 | | Decoupling within the crust, as implied by present upper-crustal tectonic wedging in central California, and decoupling between the crust and mantle, as implied by "subduction" of lithospheric mantle in southern California, indicates that the San Andreas fault system must change with depth in its location and (or) style of deformation. |
 | | Maddock, M.E., 1964, Geology of the Mt. Boarman Quadrangle, Stanislaus County, California: California Division of Mines and Geology Map Sheet 3, scale 1:62,500. |
| education.usgs.gov /california/pp1515/chapter8Ref.html (4573 words) |
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