| | GSA Cordilleran Section Field Trip Guidebook: Independence Dike Swarm |
 | | Dikes correlated with the IDS occur north of the Mt. Morrison quadrangle in the Snow Lake pendant of the central Sierra Nevada, but these dikes likely formed much farther to the south and were translated by Cretaceous dextral faulting to their present location (Lahren et al., 1990; Schweickert and Lahren, 1990). |
 | | Dikes here are shallow-level examples of Independence dikes and resemble dikes exposed in the Ord and Rodman Mountains to the north and west (Dibblee 1964a, 1964b) that cut nearly coeval volcanic rocks of the Upper Sidewinder series (e.g., Schermer and Busby, 1994). |
 | | Dikes in this area mainly strike 320° and are interpreted to have formed during extension orthogonal to the swarm (Karish et al., 1987; Schermer, 1993), based on the observation that the dikes both were injected along and are cut by normal faults in the Upper Sidewinder volcanic series. |
| www.geolab.unc.edu /Petunia/IDS_Web_Site/FTG.html (8405 words) |