Detrital zircon provenance analysis of the Great Valley Group, California: Evolution of an arc-forearc system
2003; Geological Society of America; Volume: 115; Linguagem: Inglês
10.1130/0016-7606(2003)115 2.0.co;2
ISSN1943-2674
AutoresKathleen D. Surpless, Stephan A. Graham, Joseph L. Wooden, Michael McWilliams,
Tópico(s)Geology and Paleoclimatology Research
ResumoOther| May 01, 2003 Detrital zircon provenance analysis of the Great Valley Group, California: Evolution of an arc-forearc system Kathleen DeGraaff-Surpless; Kathleen DeGraaff-Surpless Search for other works by this author on: GSW Google Scholar Stephan A. Graham; Stephan A. Graham Search for other works by this author on: GSW Google Scholar Joseph L. Wooden; Joseph L. Wooden Search for other works by this author on: GSW Google Scholar Michael O. McWilliams Michael O. McWilliams Search for other works by this author on: GSW Google Scholar Author and Article Information Kathleen DeGraaff-Surpless Stephan A. Graham Joseph L. Wooden Michael O. McWilliams Publisher: Geological Society of America First Online: 01 Jun 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (2003) 115 (5): 639. https://doi.org/10.1130/0016-7606(2003)115 2.0.CO;2 Article history First Online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Kathleen DeGraaff-Surpless, Stephan A. Graham, Joseph L. Wooden, Michael O. McWilliams; Detrital zircon provenance analysis of the Great Valley Group, California: Evolution of an arc-forearc system. GSA Bulletin 2003;; 115 (5): 639. doi: https://doi.org/10.1130/0016-7606(2003)115 2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search (v. 114, no. 12, p. 1564–1580) Figure 2 suggests that the Boxer/Cortina petrofacies boundary is at the base of the Yolo Formation and that the Cortina/Rumsey petrofacies boundary is within the Guinda Formation, when in fact the Rumsey petrofacies extends down to the base of the Guinda Formation and the Cortina petrofacies includes the Venado Formation. This confusion is an artifact of combining a petrofacies column that presents a statistically determined summary of the timing of the petrofacies boundaries for the entire Great Valley with columns that show the timing of stratigraphic units in one location (e.g., Cache Creek). You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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