Sand deposition during the last millennium at Aberffraw, Anglesey, North Wales as determined by OSL dating of quartz

S. D. Bailey; A. G. Wintle; G. A. T. Duller; C. S. Bristow

doi:10.1016/S0277-3791(00)00053-6

Sand deposition during the last millennium at Aberffraw, Anglesey, North Wales as determined by OSL dating of quartz

S. D. Bailey, A. G. Wintle, G. A. T. Duller, C. S. Bristow

Adran Daearyddiaeth a Gwyddorau Daear

Birkbeck, University of London

Allbwn ymchwil: Cyfraniad at gyfnodolyn › Erthygl › adolygiad gan gymheiriaid

94 Dyfyniadau (Scopus)

Crynodeb

Ground-penetrating radar (GPR) was used to identify sediment units at the terminus of a small dune field at Aberffraw. Nine samples were taken from boreholes; sample locations were based on the stratigraphy established by GPR. Quartz grains were dated using a single aliquot regenerative dose protocol that allows for sensitivity changes. Sand deposition at Llyn Coron, Aberffraw, occurred three times in the last 700 years with initial sand movement occurring around 1331 AD, when historical documents record sand being mobilised in a strong storm.

Iaith wreiddiol	Saesneg
Tudalennau (o-i)	701-704
Nifer y tudalennau	4
Cyfnodolyn	Quaternary Science Reviews
Cyfrol	20
Rhif cyhoeddi	5-9
Dynodwyr Gwrthrych Digidol (DOIs)	https://doi.org/10.1016/S0277-3791(00)00053-6
Statws	Cyhoeddwyd - Maw 2001
Digwyddiad	9th International Conference on Luminescence and Electron-Spin Resonance Dating (LED99) - ROME, Yr Eidal Hyd: 06 Medi 1999 → 10 Medi 1999

Mynediad at Ddogfen

10.1016/S0277-3791(00)00053-6

Cysylltiad parhaol

Dolen barhaus

Ffeiliau eraill a chysylltiadau

Dolen i’r cyhoeddiad yn Scopus

Dyfynnu hyn

@article{d09ff19c1502424d9b18b53e0e715432,

title = "Sand deposition during the last millennium at Aberffraw, Anglesey, North Wales as determined by OSL dating of quartz",

abstract = "Ground-penetrating radar (GPR) was used to identify sediment units at the terminus of a small dune field at Aberffraw. Nine samples were taken from boreholes; sample locations were based on the stratigraphy established by GPR. Quartz grains were dated using a single aliquot regenerative dose protocol that allows for sensitivity changes. Sand deposition at Llyn Coron, Aberffraw, occurred three times in the last 700 years with initial sand movement occurring around 1331 AD, when historical documents record sand being mobilised in a strong storm.",

keywords = "OPTICALLY STIMULATED LUMINESCENCE, SEDIMENTS",

author = "Bailey, {S. D.} and Wintle, {A. G.} and Duller, {G. A. T.} and Bristow, {C. S.}",

year = "2001",

month = mar,

doi = "10.1016/S0277-3791(00)00053-6",

language = "English",

volume = "20",

pages = "701--704",

journal = "Quaternary Science Reviews",

issn = "0277-3791",

publisher = "Elsevier",

number = "5-9",

note = "9th International Conference on Luminescence and Electron-Spin Resonance Dating (LED99) ; Conference date: 06-09-1999 Through 10-09-1999",

}

TY - JOUR

T1 - Sand deposition during the last millennium at Aberffraw, Anglesey, North Wales as determined by OSL dating of quartz

AU - Bailey, S. D.

AU - Wintle, A. G.

AU - Duller, G. A. T.

AU - Bristow, C. S.

PY - 2001/3

Y1 - 2001/3

N2 - Ground-penetrating radar (GPR) was used to identify sediment units at the terminus of a small dune field at Aberffraw. Nine samples were taken from boreholes; sample locations were based on the stratigraphy established by GPR. Quartz grains were dated using a single aliquot regenerative dose protocol that allows for sensitivity changes. Sand deposition at Llyn Coron, Aberffraw, occurred three times in the last 700 years with initial sand movement occurring around 1331 AD, when historical documents record sand being mobilised in a strong storm.

AB - Ground-penetrating radar (GPR) was used to identify sediment units at the terminus of a small dune field at Aberffraw. Nine samples were taken from boreholes; sample locations were based on the stratigraphy established by GPR. Quartz grains were dated using a single aliquot regenerative dose protocol that allows for sensitivity changes. Sand deposition at Llyn Coron, Aberffraw, occurred three times in the last 700 years with initial sand movement occurring around 1331 AD, when historical documents record sand being mobilised in a strong storm.

KW - OPTICALLY STIMULATED LUMINESCENCE

KW - SEDIMENTS

UR - http://www.scopus.com/inward/record.url?scp=0035108432&partnerID=8YFLogxK

U2 - 10.1016/S0277-3791(00)00053-6

DO - 10.1016/S0277-3791(00)00053-6

M3 - Article

SN - 0277-3791

VL - 20

SP - 701

EP - 704

JO - Quaternary Science Reviews

JF - Quaternary Science Reviews

IS - 5-9

T2 - 9th International Conference on Luminescence and Electron-Spin Resonance Dating (LED99)

Y2 - 6 September 1999 through 10 September 1999

ER -

Sand deposition during the last millennium at Aberffraw, Anglesey, North Wales as determined by OSL dating of quartz

Crynodeb

Mynediad at Ddogfen

Cysylltiad parhaol

Ffeiliau eraill a chysylltiadau

Ôl bys

Dyfynnu hyn