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U-Th-Pb and Rb-Sr geochronology of middle Proterozoic granite and augen gneiss, Salmon River Mountains, east-central Idaho

1990; Geological Society of America; Volume: 102; Issue: 1 Linguagem: Inglês

10.1130/0016-7606(1990)102 2.3.co;2

1943-2674

Karl V. Evans, Robert E. Zartman,

Geochemistry and Geologic Mapping

Research Article| January 01, 1990 U-Th-Pb and Rb-Sr geochronology of middle Proterozoic granite and augen gneiss, Salmon River Mountains, east-central Idaho KARL V. EVANS; KARL V. EVANS 1U.S. Geological Survey, Box 25046, MS. 905, Denver Federal Center, Denver, Colorado 80225 Search for other works by this author on: GSW Google Scholar ROBERT E. ZARTMAN ROBERT E. ZARTMAN 2U.S. Geological Survey, Box 25046, M.S. 963, Denver Federal Center, Denver, Colorado 80225 Search for other works by this author on: GSW Google Scholar Author and Article Information KARL V. EVANS 1U.S. Geological Survey, Box 25046, MS. 905, Denver Federal Center, Denver, Colorado 80225 ROBERT E. ZARTMAN 2U.S. Geological Survey, Box 25046, M.S. 963, Denver Federal Center, Denver, Colorado 80225 Publisher: Geological Society of America First Online: 01 Jun 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (1990) 102 (1): 63–73. https://doi.org/10.1130/0016-7606(1990)102 2.3.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 KARL V. EVANS, ROBERT E. ZARTMAN; U-Th-Pb and Rb-Sr geochronology of middle Proterozoic granite and augen gneiss, Salmon River Mountains, east-central Idaho. GSA Bulletin 1990;; 102 (1): 63–73. doi: https://doi.org/10.1130/0016-7606(1990)102 2.3.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 Abstract Coarsely porphyritic granite and augen gneiss in east-central Idaho have been dated by the U-Th-Pb zircon method. When plotted on concordia diagrams, the results give nonlinear data arrays that indicate the presence of at least one component of inherited radiogenic lead, as well as postcrystallization, probably recent, episodic lead-loss.Nevertheless, a systematic relationship between zircon size and convergence of the 207Pb/206Pb ages for the +100- and -100+150-mesh fractions from several samples are interpreted to provide a valid age of about 1,370 m.y. for these plutons. A single sample which is free of inheritance for all size fractions confirms this conclusion. Rb-Sr whole-rock samples are highly enriched in radiogenic strontium but do not define an isochron, probably because the system did not remain closed following crystallization of the plutons.Intrusive contacts of the granitic rocks indicate that deformation and regional metamorphism of the host Yellowjacket Formation occurred prior to 1370 Ma, rather than prior to 1500 Ma as previously suggested by others. This refinement of the geochronology (1) removes the necessity that the Yellowjacket Formation and overlying Proterozoic metasedimentary rocks of central and east-central Idaho be pre-Belt in age; (2) permits the traditional age correlation of the east-central Idaho metasedimentary sequence (Yellowjacket through Lawson Creek Formations) with the Belt Supergroup; and (3) suggests that a re-evaluation is in order for paleogeographic models of central Idaho, especially the proposed topographic high known as the Salmon River Arch. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.