F
Fred Davey
Researcher at GNS Science
Publications - 68
Citations - 3347
Fred Davey is an academic researcher from GNS Science. The author has contributed to research in topics: Crust & Plate tectonics. The author has an hindex of 32, co-authored 67 publications receiving 3188 citations. Previous affiliations of Fred Davey include Wellington Management Company & Pierre-and-Marie-Curie University.
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Seismic reflection measurements behind the Hikurangi convergent margin, southern North Island, New Zealand.
TL;DR: In this article, a 100 km long multichannel seismic reflection profile was recorded across the region of crustal downwarp and the data showed discontinuous coherent reflectors dipping westwards at the east end of the profile, and east dipping reflectors at the west end, from depths of 9 to 15 s two way time.
Summary results from CRP-1, Cape Roberts Project, Antarctica
John B. Anderson,Pietro Armienti,C. Atkins,Peter Barrett,Steven M Bohaty,S. Bryce,M. Claps,M. Curran,Fred Davey,L. De Santis,W. Ehrmann,Fabio Florindo,Christopher R. Fielding,Michael J. Hambrey,M. J. Hannah,David M. Harwood,Stuart Henrys,F. Hoelscher,J.A. Howe,Richard D. Jarrard,R. Kettler,S. Kooyman,Conrad Kopsch,L. Krissek,M. Lavelle,E. Levac,Frank Niessen,Sandra Passchier,Timothy Paulsen,Ross D. Powell,Alex Pyne,G. Rafat,Ian Raine,Andrew P. Roberts,L. Sagnotti,Sonia Sandroni,E. Scholz,J. Simes,John L. Smellie,P. Strong,M. Tabecki,Franco M Talarico,Marco Taviani,K. L. Verosub,Giuliana Villa,P.N. Webb,Gary S. Wilson,Terry J. Wilson,Sherwood W. Wise,Thomas Wonik,Ken J. Woolfe,J.H. Wrenn +51 more
Journal ArticleDOI
Depth variable crustal anisotropy, patterns of crustal weakness, and destructive earthquakes in Canterbury, New Zealand
TL;DR: In this paper, the authors measured surface wave dispersion in the South Island of New Zealand and found a distinct difference in magnitude and azimuth of surface wave anisotropy at different depths within the crust across the region.
Journal ArticleDOI
The Campbell Plateau and its relationship with the Ross Sea, Antarctica
Fred Davey,Robert E. Houtz +1 more
TL;DR: A linear belt of large-amplitude magnetic anomalies trends east-west across the northern Campbell Plateau, apparently crossing the eastern shelf edge obliquely, probably caused by magnetic rocks of pre-Late Cretaceous age as mentioned in this paper.