Middle Devensian ice-proximal gravels at Howe of Byth, Grampian region

A. M. Hall; G. Duller; J. Jarvis; A. G. Wintle

doi:10.1144/sjg31010061

Middle Devensian ice-proximal gravels at Howe of Byth, Grampian region

A. M. Hall
, G. Duller
, J. Jarvis
, A. G. Wintle

Adran Daearyddiaeth a Gwyddorau Daear

University of St Andrews

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

13 Dyfyniadau (Scopus)

Crynodeb

These ice-proximal glaciofluvial gravels have given luminescence ages of 45 ± 4 and 37 ± 4 ka BP. The gravels were laid down by meltwater draining from an ice margin in the Moray Firth and provide the first firm evidence of extensive glaciation in NE Scotland during the Mid Devensian. -from Authors

Iaith wreiddiol	Saesneg
Tudalennau (o-i)	61-64
Nifer y tudalennau	4
Cyfnodolyn	Scottish Journal of Geology
Cyfrol	31
Rhif cyhoeddi	1
Dynodwyr Gwrthrych Digidol (DOIs)	https://doi.org/10.1144/sjg31010061
Statws	Cyhoeddwyd - 1995

Mynediad at Ddogfen

10.1144/sjg31010061

Cysylltiad parhaol

Dolen barhaus

Ffeiliau eraill a chysylltiadau

Dolen i’r cyhoeddiad yn Scopus

Dyfynnu hyn

@article{b38c4a65f62d439c8942f641fc42433e,

title = "Middle Devensian ice-proximal gravels at Howe of Byth, Grampian region",

abstract = "These ice-proximal glaciofluvial gravels have given luminescence ages of 45 ± 4 and 37 ± 4 ka BP. The gravels were laid down by meltwater draining from an ice margin in the Moray Firth and provide the first firm evidence of extensive glaciation in NE Scotland during the Mid Devensian. -from Authors",

author = "Hall, \{A. M.\} and G. Duller and J. Jarvis and Wintle, \{A. G.\}",

year = "1995",

doi = "10.1144/sjg31010061",

language = "English",

volume = "31",

pages = "61--64",

journal = "Scottish Journal of Geology",

issn = "0036-9276",

publisher = "The Geological Society of London",

number = "1",

}

TY - JOUR

T1 - Middle Devensian ice-proximal gravels at Howe of Byth, Grampian region

AU - Hall, A. M.

AU - Duller, G.

AU - Jarvis, J.

AU - Wintle, A. G.

PY - 1995

Y1 - 1995

N2 - These ice-proximal glaciofluvial gravels have given luminescence ages of 45 ± 4 and 37 ± 4 ka BP. The gravels were laid down by meltwater draining from an ice margin in the Moray Firth and provide the first firm evidence of extensive glaciation in NE Scotland during the Mid Devensian. -from Authors

AB - These ice-proximal glaciofluvial gravels have given luminescence ages of 45 ± 4 and 37 ± 4 ka BP. The gravels were laid down by meltwater draining from an ice margin in the Moray Firth and provide the first firm evidence of extensive glaciation in NE Scotland during the Mid Devensian. -from Authors

UR - https://www.scopus.com/pages/publications/0029541742

U2 - 10.1144/sjg31010061

DO - 10.1144/sjg31010061

M3 - Article

AN - SCOPUS:0029541742

SN - 0036-9276

VL - 31

SP - 61

EP - 64

JO - Scottish Journal of Geology

JF - Scottish Journal of Geology

IS - 1

ER -

Middle Devensian ice-proximal gravels at Howe of Byth, Grampian region

Crynodeb

Mynediad at Ddogfen

Cysylltiad parhaol

Ffeiliau eraill a chysylltiadau

Ôl bys

Dyfynnu hyn