T143 Plate Tectonics, Arc-Trench Systems, Cordilleran Tectonics, Sedimentary Basins, Sandstone Provenance, and Geoarchaeology I: A Celebration of William R. Dickinson's Career
Monday, 26 September 2016
1:30 PM - 5:30 PM
Mile High Ballroom 2B
BILL DICKINSON, "HERO OF PLATE TECTONICS", PT 2: THE ARIZONA YEARS
Paper number: T143-3
Program: Technical Sessions
Time: 1:50 PM – 2:05 PM
Authors
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Raymond Ingersoll Presenting AuthorUniv California - Los Angeles Dept Earth, Planetary & Space Sciences, Los Angeles, CA
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Richard A. SchweickertUniversity of Nevada, Reno, Reno, NV
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Stephan A. GrahamStanford University, Stanford, CA
Abstract
Bill quickly saw the power of detrital zircon as a provenance tool and published several papers (primarily with Gehrels, but also including students) concerned with maximum depositional ages of strata, fertility of zircon in source rocks, and most of all, paleogeographic reconstructions of North America’s drainage patterns for the late Paleozoic and early Mesozoic. The Colorado Plateau became his new playground! These efforts overlapped with his grand syntheses of the California margin (1981), sinistral Nacimiento fault (1983), sedimentation associated with core complexes (1991), forearc basins (1995), Coast Range ophiolite (1996), transrotation and volcanism in coastal California (1996, 1997), circum-Pacific Holocene shore lines (2001), Basin and Range (2002), Cordillera (2004), San Gregorio-Hosgri fault (2005), Great Basin (2006, 2011), temper sands in Oceana pottery (2006), Cordilleran continental margin (2008) and provenance of Colorado Plateau strata (with Gehrels, 2008-2011 and later).
During Bill’s “retirement,” he received the Penrose Medal, the Sloss Award, the Twenhofel Medal, the Rip Rap Award and Stanford Distinguished Alumnus Award. He also became a member of the National Academy of Sciences and served as President of GSA. His bootprints will remain prominent in the Anthropocene record!
Geological Society of America Abstracts with Programs. Vol. 48, No. 7
doi: 10.1130/abs/2016AM-282996
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