S
Simon E. Jackson
Researcher at Geological Survey of Canada
Publications - 127
Citations - 21158
Simon E. Jackson is an academic researcher from Geological Survey of Canada. The author has contributed to research in topics: Inductively coupled plasma mass spectrometry & Zircon. The author has an hindex of 42, co-authored 118 publications receiving 18730 citations. Previous affiliations of Simon E. Jackson include Macquarie University & Memorial University of Newfoundland.
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Journal ArticleDOI
Investigating Age Resolution in Laser Ablation Geochronology: Workshop on Data Handling in LA‐ICP‐MSU‐Th‐Pb Geochronology; Vancouver, British Columbia, Canada, 12–13 July 2008
TL;DR: Laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) is an increasingly popular approach for determining the age of mineral grains and the timing of geological events as mentioned in this paper.
Proceedings ArticleDOI
Trace element geochemistry of diamond
Journal ArticleDOI
Sedimentary basin controls on orogenic gold deposits : new constraints from U-Pb detrital zircon and Re-Os sulphide geochronology, Lynn Lake greenstone belt, Canada.
Christopher J.M. Lawley,X.M. Yang,David Selby,David Selby,William J. Davis,S. Zhang,D C Petts,Simon E. Jackson +7 more
TL;DR: In this article, the authors report new U-Pb detrital zircon and Re-Os sulphide (arsenopyrite and pyrite) geochronology and sulphide Pb isotope results for the Paleoproterozoic Lynn Lake greenstone belt (LLGB), Manitoba, Canada.
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Olivine xenocrysts reveal carbonated mid-lithosphere in the northern Slave craton
C. Veglio,Christopher J.M. Lawley,D.G. Pearson,Bruce A. Kjarsgaard,D C Petts,Simon E. Jackson +5 more
TL;DR: In this article , the authors presented new electron microprobe and laser-ablation inductively coupledplasma mass-spectrometry results for a suite of mantle xenoliths (n = 12) and olivine xenocrysts from the Jericho, Muskox, and Voyageur kimberlites (northern Slave craton, Canada).
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Experimental fluid-mediated alteration of zircon under lower greenschist facies conditions
C.J. Kelly,C.J. Kelly,Daniel E. Harlov,Daniel E. Harlov,David A. Schneider,Simon E. Jackson,Renelle Dubosq +6 more
TL;DR: The results from these experiments imply that the surfaces of minimally metamict zircon can be chemically modified by alkali-bearing fluids via ion exchange under lower greenschist pressures and temperatures over relatively short time periods with respect to the geological time scale as mentioned in this paper.