Zobrazeno 1 - 10
of 15
pro vyhledávání: '"B. W. Glover"'
Publikováno v:
Petroleum Geoscience. 5:293-301
Nd-Sr data indicate that two isotopically distinct terrains supplied sediment to the Upper Carboniferous basins of Britain. One terrain was relatively depleted in radiogenic Nd, and included large areas of old continental crust; the other was less de
Publikováno v:
Journal of the Geological Society. 154:735-745
Sediments of the Halesowen and Salop Formations (Westphalian D-Stephanian) in the West Midlands were deposited on the southern margin of the Pennine Basin during a period of relative tectonic quiescence during the Variscan Orogeny. The clastic framew
Publikováno v:
Journal of the Geological Society. 153:901-906
New Nd and Sr data indicate that two isotopically distinct terrains supplied sediment to the Silesian Pennine Basin. The sources consisted of a northerly-derived fluvial system, which was responsible for much of the detritus during Namurian times, an
Autor:
B. W. Glover, T. McKie
Publikováno v:
Geological Society, London, Special Publications. 103:257-269
Publikováno v:
Geological Society, London, Special Publications. 82:251-265
Publikováno v:
Journal of the Geological Society. 151:971-986
Metasedimentary rocks of the Neoproterozoic Grampian and Appin groups exposed in the Glen Roy district (Monadhliath Mountains, Scotland) were strongly folded during an initial progressive tectonothermal event of the Caledonian orogeny. The attitude a
Publikováno v:
Journal of the Geological Society. 151:697-713
The presence of strata of Westphalian A to possibly Stephanian age in south Staffordshire, located at the southern margin of the Pennine Basin, provides a rare control on the timing of late Carboniferous deformation in Central England. During Westpha
Autor:
B. W. Glover, A. M. O'beirne
Publikováno v:
Sedimentology. 41:115-132
Studies, spanning a 3 year period, of Westphalian C strata exposed in an active quarry have enabled three dimensional reconstruction of a lacustrine delta complex. The sequence exhibits a complex history of lake infilling by sediment introduced by in
Publikováno v:
Journal of the Geological Society. 150:737-750
The Westphalian C Etruria Formation of Tansey Green, South Staffordshire, comprises three facies associations deposited during a period of extensional faulting. Subsequent to upper delta plain deposition during Westphalian A and B times, the lower Et
Autor:
B. W. Glover
Publikováno v:
Scottish Journal of Geology. 29:29-43
Synopsis The Neoproterozoic metasedimentary rocks between Spean Bridge and Rubha Cuil-cheanna in the Central Highlands of Scotland form part of the Grampian and Appin Groups of the Caledonides. The oldest strata, the Fort William Formation comprise a