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pro vyhledávání: '"T. Neville George"'
Autor:
T. Neville George
Publikováno v:
Philosophical Transactions of the Royal Society of London. B, Biological Sciences. 282:411-462
The Chadian rocks of Gower comprise the Caswell Bay Oolite beneath and the Caswell Bay Mudstone above. The Oolite is generally a massively bedded ‘pure’ light-grey limestone of shallow-water origin, marking nevertheless not ‘eustatic’ marine
Autor:
T. Neville George
Publikováno v:
Proceedings of the Yorkshire Geological Society. 42:229-262
SUMMARY The six ‘Major Cycles’ of sedimentation formally recognised by Ramsbottom in the British Dinantian succession are based on alternations of rock types and facies, ascribed to ‘regression’ and ‘transgression’ of the sea. Conceptuall
Autor:
T. Neville George
Publikováno v:
Proceedings of the Geologists' Association. 91:155-168
The geomorphic effects of geologically recent (late-Neogene) movements along the Tawe Disturbance are, in a recently proposed hypothesis, to be seen in fault downthrow of several hundred metres between Mynydd Epynt and the Brecon Beacons and in sinis
Autor:
T. Neville George, Emrys J. Howell
Publikováno v:
Annals and Magazine of Natural History. 4:545-561
Autor:
T. Neville George
Publikováno v:
Annals and Magazine of Natural History. 11:423-456
Autor:
T. Neville George
Publikováno v:
Geological Magazine. 64:106-119
In 1844 M'Coy subdivided the genus Spirifer Sowerby into five groups, two of which, Brachythyris and Martinia, were characterized by “the presence of a hinge-line shorter than the width of the shell”. Brachythyris included forms “in which … t
Autor:
T. Neville George
Publikováno v:
Transactions of the Geological Society of Glasgow. 24:32-107
Summary The Midland Valley, though not now a rift valley, had its origin in a rift defined by the Highland Boundary Fault and the Southern Uplands Fault. Its northern margin may be clearly traced from the North Sea to the Atlantic; its southern margi
Autor:
T. Neville George
Publikováno v:
Scottish Journal of Geology. 3:413-448
Synopsis The Eocene basalts of Ulster, transgressing all older rocks in a tectonic context ranging from the Highlands across the Midland Valley to the Southern Uplands, were repeatedly deformed and eroded both before and after the deposition of the O
Autor:
T. Neville George
Publikováno v:
Quarterly Journal of the Geological Society. 98:89-138
I. The General Form of the Towy Drainage Pattern The Towy, like the Teifi, Tawe, and Neath rivers, its sub-parallel neighbours in South Wales, is markedly asymmetrical, and is fed by tributaries most of which flow southwards and enter on the right or
Autor:
T. Neville George
Publikováno v:
Geological Magazine. 67:554-557
It is unusual to discover specimens of Palaeozoic Brachiopoda which clearly display the characters of the delthyrium; in particular, very little is known concerning these features in Carboniferous Protremata. The writer has therefore been fortunate i