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Record #193129:
A multi-dating approach applied to proglacial sediments attributed to the Most Extensive Glaciation of the Swiss Alps / Andreas Dehnert, and 6 others.
Title: | A multi-dating approach applied to proglacial sediments attributed to the Most Extensive Glaciation of the Swiss Alps / Andreas Dehnert, and 6 others. |
Author(s): | Dehnert, Andreas. |
Date: | 2010. |
In: | Boreas. (2010.), Vol. 39(3) (2010) |
Abstract: | Investigates proglacial deltaic "Höhenschotter" deposits from Swiss Plateau, to examine timing of Most Extensive Glaciation (MEG) of Quaternary Switzerland. MEG advance has been previously correlated with Riss Glaciation and MIS 6 (186-127 ka), MIS 12 (474-427 ka), or even earlier stages. Re-evaluates issue, using multi-dating approach applied to "Höhenschotter" deposits in locations outside extent of Last Glacial Maximum. Presents datings from U/Th dating of carbonate precipitated in cavity within gravels, luminescence dating on quartz and feldspar separates from sand layers, and burial dating using cosmogenic nuclides ¹⁰Be and ²⁶Al extracted from quartz pebbles and matrix sand. Suggests correlation with MIS 6. |
Notes: | Boreas. Vol. 39(3) :620-632 (2010). |
Keywords: | 551.33 -- Glacial geology. 551.332.2 -- Drift, glacial. Deposits. 551.336 -- Ice ages. 551.337 -- Chronology of the Pleistocene and recent periods. 550.93 -- Geochronology. 539.163 -- Radionuclides. 551.79 -- Quaternary. E7 -- Glaciology: glacial geology and ice ages. (234.3) -- Alps. (494) -- Switzerland. |
SPRI record no.: | 193129 |
LDR 01947naa#a2200000#a#4500 001 SPRI-193129 005 20240418230314.0 007 ta 008 240418s2010####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-193129 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aDehnert, Andreas. 245 12 ‡aA multi-dating approach applied to proglacial sediments attributed to the Most Extensive Glaciation of the Swiss Alps /‡cAndreas Dehnert, and 6 others. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2010. 300 ## ‡ap. 620-632 :‡bill., diags., tables, map. 500 ## ‡aBoreas. Vol. 39(3) :620-632 (2010). 520 3# ‡aInvestigates proglacial deltaic "Höhenschotter" deposits from Swiss Plateau, to examine timing of Most Extensive Glaciation (MEG) of Quaternary Switzerland. MEG advance has been previously correlated with Riss Glaciation and MIS 6 (186-127 ka), MIS 12 (474-427 ka), or even earlier stages. Re-evaluates issue, using multi-dating approach applied to "Höhenschotter" deposits in locations outside extent of Last Glacial Maximum. Presents datings from U/Th dating of carbonate precipitated in cavity within gravels, luminescence dating on quartz and feldspar separates from sand layers, and burial dating using cosmogenic nuclides ¹⁰Be and ²⁶Al extracted from quartz pebbles and matrix sand. Suggests correlation with MIS 6. 530 ## ‡aAlso issued online ‡uurn:doi:10.1111/j.1502-3885.2010.00146.x‡uhttps://dx.doi.org/10.1111/j.1502-3885.2010.00146.x 650 07 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a551.332.2 -- Drift, glacial. Deposits.‡2udc 650 07 ‡a551.336 -- Ice ages.‡2udc 650 07 ‡a551.337 -- Chronology of the Pleistocene and recent periods.‡2udc 650 07 ‡a550.93 -- Geochronology.‡2udc 650 07 ‡a539.163 -- Radionuclides.‡2udc 650 07 ‡a551.79 -- Quaternary.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(234.3) -- Alps.‡2udc 651 #7 ‡a(494) -- Switzerland.‡2udc 773 0# ‡7nnas ‡tBoreas. ‡gVol. 39(3) (2010) ‡wSPRI-56035 916 ## ‡a2010/09/15 -- RF 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240418 ‡bRF