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Coyle, David A. (1989) A method of sampling clast-rich laminated diamictons for magnetic analyses. Canadian Journal of Earth Sciences, 26 (8) 1654-1656 doi:10.1139/e89-141

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Reference TypeJournal (article/letter/editorial)
TitleA method of sampling clast-rich laminated diamictons for magnetic analyses
JournalCanadian Journal of Earth Sciences
AuthorsCoyle, David A.Author
Year1989 (August 1)Volume26
Issue8
PublisherCanadian Science Publishing
DOIdoi:10.1139/e89-141Search in ResearchGate
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Mindat Ref. ID480610Long-form Identifiermindat:1:5:480610:7
GUID0
Full ReferenceCoyle, David A. (1989) A method of sampling clast-rich laminated diamictons for magnetic analyses. Canadian Journal of Earth Sciences, 26 (8) 1654-1656 doi:10.1139/e89-141
Plain TextCoyle, David A. (1989) A method of sampling clast-rich laminated diamictons for magnetic analyses. Canadian Journal of Earth Sciences, 26 (8) 1654-1656 doi:10.1139/e89-141
In(1989, August) Canadian Journal of Earth Sciences Vol. 26 (8) Canadian Science Publishing
Abstract/Notes The sampling of nonlithified diamictons for magnetic analyses (anisotropy of magnetic susceptibility and paleomagnetic remanence) has been restricted to samples that are either massive, clay-rich sediments, or fine-grained ones with very low pebble contents. A new method was developed that produced standard-sized 2 × 2 × 2 cm cubes of sediment from a laminated, clay-poor diamicton from southern Denmark. The sampling procedure did not affect the sample or its magnetic characteristics in any observable manner.


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