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Record #201265:
Chronology of glaciation and deglaciation during the Loch Lomond (Younger Dryas) stade in the Scottish Highlands: implications of recalibrated ¹⁰Be exposure ages / Colin K. Ballantyne.
Title: | Chronology of glaciation and deglaciation during the Loch Lomond (Younger Dryas) stade in the Scottish Highlands: implications of recalibrated ¹⁰Be exposure ages / Colin K. Ballantyne. |
Author(s): | Ballantyne, Colin K. |
Date: | 2012. |
In: | Boreas. (2012.), Vol. 41(4) (2012) |
Abstract: | Describes recalibration of 33 ¹⁰Be exposure ages for boulders on moraines or deglacial sites in Scottish highlands using locally derived ¹⁰Be production rate and assuming rock surface erosion rates of zero to 1 mm ka⁻¹, which produces exposure ages 130-980 years older than originally reported. Uses filtered results to generate aggregate probability density distributions for timing of moraine deposition and deglaciation. |
Notes: | Boreas. Vol. 41(4) :513-526 (2012). |
Keywords: | 551.33 -- Glacial geology. 550.93 -- Geochronology. 54.027 -- Isotope analysis. 546.45 -- Beryllium. 551.583.3 -- Climatic changes, Quaternary. 551.332.52 -- Moraines, terminal and recessional. 551.324.63 -- Land ice, advance and retreat. 551.4 -- Geomorphology. E7 -- Glaciology: glacial geology and ice ages. (411) -- Scotland. |
SPRI record no.: | 201265 |
LDR 01711naa#a2200000#a#4500 001 SPRI-201265 005 20240329104257.0 007 ta 008 240329s2012####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-201265 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aBallantyne, Colin K. 245 10 ‡aChronology of glaciation and deglaciation during the Loch Lomond (Younger Dryas) stade in the Scottish Highlands :‡bimplications of recalibrated ¹⁰Be exposure ages /‡cColin K. Ballantyne. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2012. 300 ## ‡ap. 513-526 :‡bill., diags., tables, maps. 500 ## ‡aBoreas. Vol. 41(4) :513-526 (2012). 520 3# ‡aDescribes recalibration of 33 ¹⁰Be exposure ages for boulders on moraines or deglacial sites in Scottish highlands using locally derived ¹⁰Be production rate and assuming rock surface erosion rates of zero to 1 mm ka⁻¹, which produces exposure ages 130-980 years older than originally reported. Uses filtered results to generate aggregate probability density distributions for timing of moraine deposition and deglaciation. 530 ## ‡aAlso issued online ‡uurn:doi:10.1111/j.1502-3885.2012.00253.x‡uhttps://dx.doi.org/10.1111/j.1502-3885.2012.00253.x 650 07 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a550.93 -- Geochronology.‡2udc 650 07 ‡a54.027 -- Isotope analysis.‡2udc 650 07 ‡a546.45 -- Beryllium.‡2udc 650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc 650 07 ‡a551.332.52 -- Moraines, terminal and recessional.‡2udc 650 07 ‡a551.324.63 -- Land ice, advance and retreat.‡2udc 650 07 ‡a551.4 -- Geomorphology.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(411) -- Scotland.‡2udc 773 0# ‡7nnas ‡tBoreas. ‡gVol. 41(4) (2012) ‡wSPRI-56035 916 ## ‡a2012/11/08 -- JR 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240329 ‡bJR