Zobrazeno 1 - 7
of 7
pro vyhledávání: '"R. G. Davy"'
Autor:
D. Barker, Michael Warner, Rebecca Bell, R. G. Davy, Stuart Henrys, Nathan L. Bangs, Joanna Morgan, Laura Frahm, Ryuta Arai
Full-waveform inversion (FWI) can resolve subsurface physical properties to high resolutions, yet high-performance computing resources have only recently made it practical to invert for high frequencies. A benefit of high-frequency FWI is that recove
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9974acf4a20bd09655c61b3f89e7050e
http://hdl.handle.net/10044/1/91974
http://hdl.handle.net/10044/1/91974
Publikováno v:
Geophysical Journal International. 218:45-56
SUMMARY We present a new approach to estimate 3-D seismic velocities along a target interface. This approach uses an artificial neural network trained with user-supplied geological and geophysical input features derived from both a 3-D seismic reflec
Autor:
Martin Weeks, Gabriella Castiello, J. Collier, Frank Kruger, Lidong Bie, Marjorie Wilson, Jeroen van Hunen, Anna Bird, B. Chichester, Jon D Blundy, Andy Clegg, Nicholas Harmon, R. G. Davy, Richie Robertson, Henning Kirk, Joan L. Latchman, Andreas Rietbrock, T. Henstock, Timothy J. Henstock, Catherine A. Rychert, Stephen Hicks, Colin G. Macpherson, Ben Pitcairn, Ben Roche, Mike Kendall, Dan Posse, Sophie Butcher, Jamie J. Wilkinson, Chen Chen, Jenny S. Collier, Benjamin Maunder, Jon P. Davidson, Saskia Goes, Caroline Harkin, Stephen Tait, George F. Cooper, Erik Labahn, Robert Allen
Publikováno v:
Journal of geophysical research / Solid earth, 125 (6)
We present a high‐resolution 2‐D P‐wave velocity model from a 225‐km‐long active seismic profile, collected over ~60–75 Ma central Atlantic crust. The profile crosses five ridge segments separated by a transform and three nontransform off
Autor:
R. G. Davy, Joanna Morgan, Gaël Lymer, Timothy J. Reston, Jonathan M. Bull, Gaye Bayrakci, Dale S. Sawyer, Dirk Klaeschen, Derren Cresswell, Timothy A. Minshull
Publikováno v:
Geophysical Journal International, 212 (1). pp. 244-263.
Continental hyperextension during magma-poor rifting at the Deep Galicia Margin is characterised by a complex pattern of faulting, thin continental fault blocks, and the serpentinisation, with local exhumation, of mantle peridotites along the S-refle
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::78a235669eaad091beb804fc3d406da4
https://eprints.soton.ac.uk/414348/
https://eprints.soton.ac.uk/414348/
Autor:
Cord Papenberg, Dirk Klaeschen, Timothy A. Minshull, Julia K. Morgan, Marta Pérez-Gussinyé, Gaye Bayrakci, Jonathan M. Bull, Timothy J. Reston, R. G. Davy, Dale S. Sawyer, Donna J. Shillington, César R. Ranero
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
Bayrakci, G. ... et al.-- 5 pages, 3 figures, supplementary information https://dx.doi.org/10.1038/ngeo2671
Water and carbon are transferred from the ocean to the mantle in a process that alters mantle peridotite to create serpentinite and suppo
Water and carbon are transferred from the ocean to the mantle in a process that alters mantle peridotite to create serpentinite and suppo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::42961d5d5dc8178b55d76bcef1429a00
https://eprints.soton.ac.uk/388558/
https://eprints.soton.ac.uk/388558/
Autor:
R G, Davy
Publikováno v:
Nursing mirror and midwives journal. 144(4)
Autor:
R G, Davy, D C, White
Publikováno v:
Anaesthesia. 28(1)