U-Pb SHRIMP ages of detrital granulite-facies rutiles: further constraints on provenance of Jurassic sandstones on the Norwegian margin

Electron microprobe analyses of 128 detrital rutile grains from two Jurassic sandstone samples (Hettangian and Bajocian-Bathonian in age) from hydrocarbon exploration wells on the Norwegian margin confirm that more than 85 % of the rutiles were derived from metapelitic rocks. Zr-in-rutile geothermom...

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Bibliographic Details
Published in:Geological Magazine
Main Authors: Meinhold, Guido, Morton, Andrew, Fanning, Christopher, Whitham, A G
Format: Article in Journal/Newspaper
Language:unknown
Published: Cambridge University Press
Subjects:
Keywords: clastic sediment
electron probe analysis
granulite facies
high temperature
hydrocarbon exploration
Jurassic
metamorphism
metapelite
metasedimentary rock
provenance
rutile
sandstone
SHRIMP dating
uranium-lead dating
Atlantic Ocean
North Sea
geothermometry
Norwegian margin
sediment provenance
U-Pb geochronology
Greenland
East Greenland
Online Access:http://hdl.handle.net/1885/50560
https://doi.org/10.1017/S0016756810000877
https://openresearch-repository.anu.edu.au/bitstream/1885/50560/5/u4027924xPUB206_2011.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/50560/7/01_Meinhold_U-Pb_SHRIMP_ages_of_detrital_2010.pdf.jpg
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Summary:Electron microprobe analyses of 128 detrital rutile grains from two Jurassic sandstone samples (Hettangian and Bajocian-Bathonian in age) from hydrocarbon exploration wells on the Norwegian margin confirm that more than 85 % of the rutiles were derived from metapelitic rocks. Zr-in-rutile geothermometry confirms that about 83 % of the rutile was formed under high-grade metamorphism (>750 C). Sixty-two rutile grains, including 60 of the identified high-temperature rutile population, were also analysed for U-Pb geochronology using SHRIMP. The206Pb-238U rutile ages range from approximately 485-292 Ma, with a major cluster between 450 and 380 Ma. These data suggest that the detrital rutile was predominantly derived from a felsic source that experienced granulite-facies metamorphism about 450-380 Ma ago. This conclusion is consistent with derivation from high-grade Caledonian metasedimentary rocks, probably the Krummedal sequence in central East Greenland, as previously suggested by an earlier provenance study using conventional heavy mineral analysis, garnet geochemistry and detrital zircon age dating. The present study underscores the importance of rutile geochemistry and geochronology in quantitative single-mineral provenance analysis of clastic sedimentary rocks.

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