Research Article| June 01, 1989 Sm-Nd and Rb-Sr isotope systematics of scheelites: Possible implications for the age and genesis of vein-hosted gold deposits Keith Bell; Keith Bell 1Department of Earth Sciences, Carleton University, Ottawa-Carleton Geoscience Centre Ottawa, Ontario K1 S 5B6, Canada Search for other works by this author on: GSW Google Scholar C. D. Anglin; C. D. Anglin 2Geological Survey of Canada, Ottawa, Ontario K1 A OE8, Canada Search for other works by this author on: GSW Google Scholar J. M. Franklin J. M. Franklin 2Geological Survey of Canada, Ottawa, Ontario K1 A OE8, Canada Search for other works by this author on: GSW Google Scholar Author and Article Information Keith Bell 1Department of Earth Sciences, Carleton University, Ottawa-Carleton Geoscience Centre Ottawa, Ontario K1 S 5B6, Canada C. D. Anglin 2Geological Survey of Canada, Ottawa, Ontario K1 A OE8, Canada J. M. Franklin 2Geological Survey of Canada, Ottawa, Ontario K1 A OE8, Canada Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1989) 17 (6): 500–504. https://doi.org/10.1130/0091-7613(1989)017<0500:SNARSI>2.3.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Keith Bell, C. D. Anglin, J. M. Franklin; Sm-Nd and Rb-Sr isotope systematics of scheelites: Possible implications for the age and genesis of vein-hosted gold deposits. Geology 1989;; 17 (6): 500–504. doi: https://doi.org/10.1130/0091-7613(1989)017<0500:SNARSI>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 SocietyGeology Search Advanced Search Abstract A positive correlation between present-day 143Nd/144Nd and 147Sm/144Nd ratios from scheelite samples from the Hollinger-McIntyre-Coniaurum gold deposit of Ontario, Canada, corresponds to an age of 2403 ±47 Ma and may date the age of gold mineralization. Initial isotope ratios of scheelites suggest that the fluid responsible for the scheelite and gold mineralization was probably of mantle origin and that it subsequently interacted with continental crust. 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.
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Bell et al. (1989) studied this question.