Zobrazeno 1 - 10
of 45
pro vyhledávání: '"N. H. Woodcock"'
Autor:
N. H. Woodcock, N. J. Soper
Publikováno v:
The Geology of England and Wales ISBN: 9781862393882
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8457db93431381fdd403e99d6c218fc0
https://doi.org/10.1144/goewp.6
https://doi.org/10.1144/goewp.6
Autor:
N. H. Woodcock
Publikováno v:
A Revised Correlation Ordovician Rocks ISBN: 9781862396920
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::23161669225fde8891c5943d578659c7
https://doi.org/10.1144/sr24.3
https://doi.org/10.1144/sr24.3
Autor:
N. H. Woodcock, J. C. Pauley
Publikováno v:
Geological Journal. 24:113-120
Two formations are named in the presumed Precambrian sedimentary rocks of the Old Radnor Inlier. The Strinds Formation comprises fine- to medium-grained sandstones and pebbly sandstones. Grain-size, texture, clast types, and lithological invariance s
Autor:
N. H. Woodcock, N. J. Soper
Publikováno v:
Geological Magazine. 140:627-647
Illite crystallinity data from the Silurian slate belts of England and Wales indicate anchizone to low epizone metamorphism during the Acadian deformation in late Early Devonian time. This metamorphic grade implies a substantial overburden, now erode
Publikováno v:
Geological Society, London, Special Publications. 160:189-211
Autor:
R. P. Barnes, N. H. Woodcock
Publikováno v:
Geological Society, London, Special Publications. 160:89-107
Publikováno v:
Geological Society, London, Special Publications. 103:197-208
This work reviews the correlation of the British and Irish Cambrian with the current (though incomplete) international standard for the Cambrian. Since the earlier edition of 1972, the basal and upper limits of the Cambrian system has been internatio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2d4f8e8381edfa9b822d7277383f8ced
https://doi.org/10.1144/sr25
https://doi.org/10.1144/sr25
Autor:
M. A. Awan, N. H. Woodcock
Publikováno v:
Geological Journal. 28:179-189
New mapping has better defined the well known arc in Acadian (late Caledonian) structures centred in the Berwyn Hills. This arc, convex to the north-west and about 20 km across, is defined by the strikes of bedding and cleavage and the trends of fold
Publikováno v:
Geological Magazine. 129:367-372