Research Article| August 01, 2000 Sm-Nd dating of the giant Sullivan Pb-Zn-Ag deposit, British Columbia Shao-Yong Jiang; Shao-Yong Jiang 1State Key Laboratory for Mineral Deposits Research, Nanjing University, Nanjing 210093, China Search for other works by this author on: GSW Google Scholar John F. Slack; John F. Slack 2U.S. Geological Survey, National Center, MS 954, Reston, Virginia 20192, USA Search for other works by this author on: GSW Google Scholar Martin R. Palmer Martin R. Palmer 3T.H. Huxley School, Imperial College, Prince Consort Road, London SW7 2BP, UK Search for other works by this author on: GSW Google Scholar Author and Article Information Shao-Yong Jiang 1State Key Laboratory for Mineral Deposits Research, Nanjing University, Nanjing 210093, China John F. Slack 2U.S. Geological Survey, National Center, MS 954, Reston, Virginia 20192, USA Martin R. Palmer 3T.H. Huxley School, Imperial College, Prince Consort Road, London SW7 2BP, UK Publisher: Geological Society of America Received: 11 Jan 2000 Revision Received: 19 May 2000 Accepted: 23 May 2000 First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2000) 28 (8): 751–754. https://doi.org/10.1130/0091-7613(2000)28<751:SDOTGS>2.0.CO;2 Article history Received: 11 Jan 2000 Revision Received: 19 May 2000 Accepted: 23 May 2000 First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Shao-Yong Jiang, John F. Slack, Martin R. Palmer; Sm-Nd dating of the giant Sullivan Pb-Zn-Ag deposit, British Columbia. Geology 2000;; 28 (8): 751–754. doi: https://doi.org/10.1130/0091-7613(2000)28<751:SDOTGS>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 SocietyGeology Search Advanced Search Abstract We report here Sm and Nd isotope data for hydrothermal tourmalinites and sulfide ores from the giant Sullivan Pb-Zn-Ag deposit, which occurs in the lower part of the Mesoproterozoic Purcell (Belt) Supergroup. Whole-rock samples of quartz-tourmaline tourmalinite from the footwall alteration pipe yield a Sm-Nd isochron age of 1470 ± 59 Ma, recording synsedimentary B metasomatism of clastic sediments during early evolution of the Sullivan hydrothermal system. Data for variably altered (chloritized and/or albitized) tourmalinites from the hanging wall of the deposit, which are believed to have formed originally ca. 1470 Ma, define a younger 1076 ± 77 Ma isochron because of resetting of Sm and Nd isotopes during Grenvillian metamorphism. HCl leachates of bedded Pb-Zn ore yield a Sm-Nd isochron age of 1451 ± 46 Ma, which is consistent with syngenetic-exhalative mineralization ca. 1470 Ma; this age could also reflect a slightly younger, epigenetic hydrothermal event. Results obtained for the Sullivan deposit indicate that the Sm-Nd geochronometer has the potential to directly date mineralization and alteration in stratabound sulfide deposits that are not amenable to dating by other isotope methods. 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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