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Record #122658:
- #122658
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MARC recordMagnetic susceptibility as a Quaternary correlation tool: examples from Hudson Strait sediment cores, eastern Canadian Arctic / W.F. Manley, B. MacLean, M.W. Kerwin, John T. Andrews.
| Title: | Magnetic susceptibility as a Quaternary correlation tool: examples from Hudson Strait sediment cores, eastern Canadian Arctic / W.F. Manley, B. MacLean, M.W. Kerwin, John T. Andrews. |
| Author(s): | Manley, W. F. MacLean, B. Kerwin, M. W. Andrews, John T. |
| Date: | 1993. |
| In: | Geological Survey of Canada. Paper. (1993.), Vol. 93-1D (1993) |
| Abstract: | Whole-core, volume magnetic susceptibility (MS) was measured on four sediment cores taken from Hudson Bay and Hatton Basin during 1992 cruise. MS is indicator of sediment density, texture and mineralogy, and can be used to ascertain sediment provenance in relation to Late Quaternary glacial history. Here, it will be used to reconstruct glacial and marine environments at north-east margin of Laurentide ice sheet. |
| Notes: | Geological Survey of Canada. Paper. Vol. 93-1D :137-145 (1993). |
| Keywords: | 551.336 -- Ice ages. 551.79 -- Quaternary. 551.337 -- Chronology of the Pleistocene and recent periods. 550.380 -- Geomagnetic techniques. E7 -- Glaciology: glacial geology and ice ages. (*41) -- Canada. (*3) -- Arctic regions. (*60) -- Arctic Ocean and adjacent waters. (*622) -- Hudson Strait and Ungava Bay. |
| SPRI record no.: | 122658 |
LDR 01625naa#a2200000#a#4500 001 SPRI-122658 005 20231206113648.0 007 ta 008 231206s1993####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-122658 040 ## ‡aUkCU-P‡beng‡eaacr 245 00 ‡aMagnetic susceptibility as a Quaternary correlation tool :‡bexamples from Hudson Strait sediment cores, eastern Canadian Arctic /‡cW.F. Manley, B. MacLean, M.W. Kerwin, John T. Andrews. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1993. 300 ## ‡ap. 137-145 :‡bdiags., tables, map. 500 ## ‡aGeological Survey of Canada. Paper. Vol. 93-1D :137-145 (1993). 520 3# ‡aWhole-core, volume magnetic susceptibility (MS) was measured on four sediment cores taken from Hudson Bay and Hatton Basin during 1992 cruise. MS is indicator of sediment density, texture and mineralogy, and can be used to ascertain sediment provenance in relation to Late Quaternary glacial history. Here, it will be used to reconstruct glacial and marine environments at north-east margin of Laurentide ice sheet. 650 07 ‡a551.336 -- Ice ages.‡2udc 650 07 ‡a551.79 -- Quaternary.‡2udc 650 07 ‡a551.337 -- Chronology of the Pleistocene and recent periods.‡2udc 650 07 ‡a550.380 -- Geomagnetic techniques.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(*41) -- Canada.‡2udc 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*622) -- Hudson Strait and Ungava Bay.‡2udc 700 1# ‡aManley, W. F. 700 1# ‡aMacLean, B. 700 1# ‡aKerwin, M. W. 700 1# ‡aAndrews, John T. 773 0# ‡7nnas ‡tGeological Survey of Canada. Paper. ‡gVol. 93-1D (1993) ‡wSPRI-16499 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231206