Zobrazeno 1 - 7
of 7
pro vyhledávání: '"R. H. Maddock"'
Autor:
R. P. Barnes, G. S. Kimbell, M. C. Akhurst, Antoni E. Milodowski, R. A. Chadwick, D. Millward, R. H. Maddock, M. G. Norton
Publikováno v:
Proceedings of the Yorkshire Geological Society. 52:139-158
SUMMARY The Lake District Boundary Fault Zone (LDBFZ) lies at the boundary between the Permo-Triassic East Irish Sea Basin and the Lower Palaeozoic Lake District Block. It divides northwards, within west Cumbria, into a network of fault strands that
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::62d313c8706d20823a61fb2359675bc7
https://doi.org/10.1144/pygs.52.2.139
https://doi.org/10.1144/pygs.52.2.139
Publikováno v:
Quarterly Journal of Engineering Geology. 24:363-374
Attempts were made to obtain absolute ages constraining the most recent episode of fault activity in the North Somerset Coastal Fault Belt as part of the seismic hazard assessment for the proposed Hinkley Point ‘C’ power station. Radiometric (ura
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::69d30513114ddc4d2d2caf0eef7ce16d
https://doi.org/10.1144/gsl.qjeg.1991.024.04.04
https://doi.org/10.1144/gsl.qjeg.1991.024.04.04
Autor:
R. H. Maddock
Publikováno v:
Journal of the Geological Society. 149:249-250
The papers in this thematic set arise from a meeting jointly organized by the Tectonic Studies Group and the Stratigraphy Committee of the Geological Society and held at Burlington House on 28 November 1990. About 80 people heard oral presentations o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8fdbd25298520abf8893642280cb4c24
https://doi.org/10.1144/gsjgs.149.2.0249
https://doi.org/10.1144/gsjgs.149.2.0249
Publikováno v:
Pure and Applied Geophysics PAGEOPH. 124:3-30
Fault rocks formed in phyllosilicate-bearing rocks formed over a wide range of environmental conditions within the Earth's crust are characterised by similar structural and microstructural features. The most striking of these are (a) P foliation, def
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3c0216d31a9500f9918840850d2e79f4
https://doi.org/10.1007/bf00875717
https://doi.org/10.1007/bf00875717
Publikováno v:
Scopus-Elsevier
The palaeomagnetic properties and magnetic fabric of clay-rich fault gouge in a prominent fault at Porth-y-pistyll on the northern coast of Anglesey, North Wales, have been investigated in an attempt to constrain the age of last movement on this faul
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8037f68657a48092f35dfc79c2b3412e
http://www.scopus.com/inward/record.url?eid=2-s2.0-0026464697&partnerID=MN8TOARS
http://www.scopus.com/inward/record.url?eid=2-s2.0-0026464697&partnerID=MN8TOARS
Autor:
M. P. Bates, Richard D. Law, John Wheeler, Geoffrey E. Lloyd, Colin C. Ferguson, S. M. Agar, Ernest H. Rutter, David J. Prior, A. Welbon, K. H. Brodie, Rob J. Knipe, R. H. Maddock, S.H. White, T. H. Bell, N. T. Grant
Publikováno v:
Geology. 15:829
Accurate rock-specimen orientations are a fundamental link between hand-speciman or thin-section features and larger geologic structures. Without field orientation, observations made using petrological or electron microscopes are devalued and may be
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5bea9fd9a131ba51af364450475e8eb0
https://doi.org/10.1130/0091-7613(1987)15<829:oosedf>2.0.co
https://doi.org/10.1130/0091-7613(1987)15<829:oosedf>2.0.co
Autor:
R. H. Maddock
Publikováno v:
Geology. 11:105
A petrographic and electron-microprobe study of fault-generated pseudotachylytes from the Outer Hebrides Thrust Zone, Scotland, demonstrates that the textures have resulted from the primary crystallization of a clast-laden melt rather than the devitr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::deba8524c2d33eb0e43ecf0ea8382591
https://doi.org/10.1130/0091-7613(1983)11<105:moofpd>2.0.co
https://doi.org/10.1130/0091-7613(1983)11<105:moofpd>2.0.co