Zobrazeno 1 - 10
of 96
pro vyhledávání: '"J.D. Peacock"'
Autor:
J.D. Peacock
Publikováno v:
Proceedings of the Geologists' Association. 129:235-240
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::981dc9b5a91d790609d9aa36b265bdd5
https://doi.org/10.1016/j.pgeola.2018.03.007
https://doi.org/10.1016/j.pgeola.2018.03.007
Autor:
J.D. Peacock, James Rose
Publikováno v:
Proceedings of the Geologists' Association. 128:173-179
The concept that Rannoch Moor, the centre of the Younger Dryas (YD), West Highland Icefield, was deglaciated as early as 12.5 cal ka BP is discussed in the light of radiocarbon dates and varve sequences from outlet glaciers of this icefield, and clim
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3ac0a6dc40b869965878803918e01da6
https://doi.org/10.1016/j.pgeola.2017.02.002
https://doi.org/10.1016/j.pgeola.2017.02.002
Publikováno v:
Proceedings of the Geologists' Association. 123:419-437
Offshore boreholes from the outer Firth of Clyde and from the Sea of the Hebrides passed through marine deposits of Holocene, Loch Lomond Stadial (LLS) and Windermere Interstadial (WI) age, but it is likely that older, probably Dimlington Stadial (DS
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3f71d311788be00517f08669e615c6a1
https://doi.org/10.1016/j.pgeola.2012.02.005
https://doi.org/10.1016/j.pgeola.2012.02.005
Publikováno v:
Quaternary Science Reviews. 22:1551-1554
The recent reconstruction by Bowen et al. (2002) of the history of the last British and Irish Ice sheet (BIIS) at the Last Glacial Maximum (LGM) resumes a debate over the extent and behaviour of the last Scottish Ice Sheet (ScIS) that extends back ov
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::95796a1e11d425ba73afe5005848803f
https://doi.org/10.1016/s0277-3791(03)00121-5
https://doi.org/10.1016/s0277-3791(03)00121-5
Autor:
J.D. Peacock
Publikováno v:
Quaternary Science Reviews. 18:1655-1680
Late Devensian raised marine deposits predating the Windermere Interstadial (c. 13–11 ka BP) are found between the Moray Firth and Berwick. The widely distributed, sparsely fossiliferous Errol Clay Formation of the firths of Forth and Tay was laid
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e875311fab7066bf534e83ae37f208b7
https://doi.org/10.1016/s0277-3791(98)00117-6
https://doi.org/10.1016/s0277-3791(98)00117-6
Autor:
Nicholas R. Golledge, Paul Dunlop, Peter U. Clark, M. Armstrong, David E. Smith, J.D. Peacock, Martyn S. Stoker, A.M. McCabe, M.A.E. Browne
Publikováno v:
Journal of the Geological Society. 164:1261-1263
J. D. Peacock, M. Armstrong, M. A. E. Browne, N. R. Golledge & M. S. Stoker write: We are unable to support the view of McCabe et al . (2007) that there were significant readvances of the Scottish Ice-sheet at Lunan Bay and near Perth. The authors pr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::27c57cbf9b451a61e51b17b2fae585e4
https://doi.org/10.1144/0016-76492007-053
https://doi.org/10.1144/0016-76492007-053
Publikováno v:
Kristensen, P, Knudsen, K L, Lykke-Andersen, H, Nørmark, E, Peacock, J D & Sinnott, A 1998, ' Interglacial and glacial climate oscillations in a marine shelf sequence from northern-Denmark a multidisciplinary study ' Quaternary Science Reviews, vol. 17, no. 9-10, pp. 813-837 . https://doi.org/10.1016/S0277-3791(98)00020-1
A 22.5 m long marine shelf sequence in northern Denmark covers the climatic shifts from glacial environments, through interglacial and into early glacial conditions. The interglacial was interrupted by two cool intervals. Also the early glacial succe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::10ea2e7295881bb46e53247c73e854ea
https://doi.org/10.1016/s0277-3791(98)00020-1
https://doi.org/10.1016/s0277-3791(98)00020-1
Autor:
William E. N. Austin, Hans-Peter Plag, K. Rokoengen, D.F. Belknap, K.S. Petersen, R.T.R. Wingfield, John England, James D. Scourse, H. Josenhans, R. J. N. Devoy, D. E. Smith, J.D. Peacock
Publikováno v:
Terra Nova. 8:213-222
Sea levels of the past 20 kyr are largely determined by the response of the Earth to the last ice age. Consequently, sea-level indicators are an important source of information about the interaction between cryosphere and hydrosphere and the solid Ea
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1b8f6983df5eedec2e0aef8c6946f4c5
https://doi.org/10.1111/j.1365-3121.1996.tb00750.x
https://doi.org/10.1111/j.1365-3121.1996.tb00750.x
Autor:
J.D. Peacock
Publikováno v:
Quaternary Science Reviews. 14:1029-1042
Lithological and macrofaunal analysis of vibrocores collected from northwest of the Viking Bank enables the Devensian to Holocene strata to be subdivided into eight informal units, three of which occur widely in the northern North Sea. For the Viking
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::886aeb572ca23b619f5431b8d62b0e1c
https://doi.org/10.1016/0277-3791(95)00041-0
https://doi.org/10.1016/0277-3791(95)00041-0
Autor:
J.D. Peacock
Publikováno v:
Quaternary Science Reviews. 12:263-275
Temperature, salinity and depth limits are given for selected molluscs from boreal and arctic regions of the NE Atlantic and adjacent shelf seas. The significance of the data for palaeoenviromental analysis is briefly discussed.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fc18c2a3edd9e9b2bc6e5de527a7974f
https://doi.org/10.1016/0277-3791(93)90082-w
https://doi.org/10.1016/0277-3791(93)90082-w