Zobrazeno 1 - 10 of 40 pro vyhledávání: '"J. D. Peacock"'
1
Pre-Late Devensian high-arctic marine deposits in SW Scotland
Autor: Jeremy D. Everest, J. D. Peacock
Publikováno v: Scottish Journal of Geology. 46:89-92
Synopsis We present new interpretations of Digital Elevation Model (DEM) data and marine fossils collected from three sites on the Rhins of Galloway which, contrary to recent proposals, suggest that the landforms and deposits of the region do not rep
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6b05868731b0a840819b4fdb41b9fe33
https://doi.org/10.1144/0036-9276/01-390
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2
Late Devensian marine deposits (Errol Clay Formation) at the Gallowflat Claypit, eastern Scotland: new evidence for the timing of ice recession in the Tay Estuary
Autor: J. D. Peacock
Publikováno v: Scottish Journal of Geology. 39:1-10
Synopsis The Late Devensian arctic marine deposits (Errol Clay Formation) at the Gallowflat Claypit between Perth and Dundee are correlated with the type succession at nearby Inchcoonans, but include an expanded basal glaciomarine unit with rhythms i
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::a12d8cf0778b6c8f2b243d2fff8f3f26
https://doi.org/10.1144/sjg39010001
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3
A Windermere Interstadial marine sequence: environmental and relative sea level interpretations for the western Forth valley, Scotland
Autor: J. D. Peacock, A. M. Wood, David E. Smith, L. K. Holloway
Publikováno v: Scottish Journal of Geology. 38:41-54
Synopsis Multidisciplinary investigations of a radiocarbon dated isostatically raised, shallow marine sequence have enabled environmental parameters, including estimates of relative sea level and water temperatures, to be reconstructed for the Winder
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::d8bdbc96e63a6e71cc180b84a91776db
https://doi.org/10.1144/sjg38010041
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4
The Bothkennar Gravel Formation (‘buried gravel layer’) of the Forth Estuary
Autor: J. D. Peacock
Publikováno v: Scottish Journal of Geology. 34:1-5
Synopsis The Bothkennar Gravel Formation ‘buried gravel layer’, which is widespread below the Flandrian carse clays (Claret Formation) of the Forth estuary, is interpreted as having been formed chiefly by ice-rafting of sediment from the shore du
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::22b92b7ab24381e965d59558984dc9f2
https://doi.org/10.1144/sjg34010001
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5
Ice-rafted sediments of Loch Lomond Stadial age in western Scotland
Autor: J. D. Peacock
Publikováno v: Scottish Journal of Geology. 33:51-57
Synopsis At two former oil platform sites (Portavadie and Ardyne) in the Clyde estuary, several metres of very poorly sorted gravelly and cobbly silt and sand of the Portavadie Formation were deposited during the Loch Lomond Stadial. The sediments ar
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::ca99a7d6ee20d357bcefbad3b4f89dd8
https://doi.org/10.1144/sjg33010051
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7
The 14C Age of the Icelandic Vedde Ash: Implications for Younger Dryas Marine Reservoir Age Corrections
Autor: Edouard Bard, J. D. Peacock, Dick Kroon, William E. N. Austin, John B Hunt
Publikováno v: Radiocarbon. 37:53-62
Increased marine 14C reservoir ages from the surface water of the North Atlantic are documented for the Younger Dryas period. We use terrestrial and marine AMS 14C dates from the time of deposition of the Icelandic Vedde Ash to examine the marine 14C
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::ff95dd86c1b923eb71775928f8361316
https://doi.org/10.1017/s0033822200014788
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8
Pre-Flandrian slope deformation in the Scottish Highlands: examples from Glen Roy and Glen Gloy
Autor: F. May, J. D. Peacock
Publikováno v: Scottish Journal of Geology. 29:183-189
Synopsis Slope deformation at localities in Glen Roy and Glen Gloy became essentially inactive prior to the formation of glacial lake shorelines (Parallel Roads) that are related to the maximum of Loch Lomond Readvance glaciers (10 500–10 000 BP).
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::f34008b60cf622ea557e6218dfecf471
https://doi.org/10.1144/sjg29020183
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9
Late Devensian and Flandrian palaeoenvironmental changes on the Scottish continental shelf west of the Outer Hebrides
Autor: Rex Harland, J. D. Peacock, I. P. Wilkinson, William E. N. Austin, I. Selby, D. K. Graham
Publikováno v: Journal of Quaternary Science. 7:145-161
Examination of two radiocarbon-dated vibrocores taken from south of St Kilda at a water depth of about 155 m, a short distance within the maximum position of the Late Devensian (Dimlington Stadial) ice sheet, suggests that the St Kilda Basin became f
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::0cf40de48ccf23b4a23ae700a51f95e5
https://doi.org/10.1002/jqs.3390070206
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10
The engineering geology of the Came clay at the National Soft Clay Research Site, Bothkennar
Autor: J. D. Peacock, M. A. Paul, B. F. Wood
Publikováno v: Géotechnique. 42:183-198
It is possible to subdivide the Carse clay deposits above the Bothkennar gravel into bedded, laminated, mottled and weathered faciès. The first is composed of silty clays which retain original sedimentary structures from quiet water tidal deposition
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::f6f802df8979cbf0a46a4251a6ea56e7
https://doi.org/10.1680/geot.1992.42.2.183
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