Zobrazeno 1 - 10
of 26
pro vyhledávání: '"Roy A. Livermore"'
Publikováno v:
Earth and Planetary Science Letters. 242:343-353
After isostatic correction for their sedimentary fill, the depths of two small oceanic basins in the southern Scotia Sea suggest that both started to open in mid to late Eocene times. Models of the short magnetic anomaly profiles across the basins pr
Autor:
Alan P. M. Vaughan, Roy A. Livermore
Publikováno v:
Geological Society, London, Special Publications. 246:143-178
A review of evidence for deformation and terrane accretion on the Late Triassic–Early Jurassic margins of Pangea and the mid-Cretaceous margins of the palaeo-Pacific ocean shows that deformation was global and synchronous with probable superplume e
Autor:
Rose L. Winterton, Roy A. Livermore
Publikováno v:
Gondwana Research. 7:287-292
Geographical Information Systems (GIS) provide tools for manipulating and analysing the large thematic datasets associated with Gondwana research. We have used a customised version of Environmental Systems Research Institute's ArcGIS, version 8.2, as
Publikováno v:
Geophysical Journal International. 155:789-804
Earthquake data from the Scotia Arc to early 2002 are reviewed in the light of satellite gravity and other data in order to derive a model for the motion of plates in the Scotia Sea region. Events with magnitude greater than or equal to5, which occur
Publikováno v:
Journal of Petrology. 43:1435-1467
The East Scotia Ridge is an active back-arc spreading centre located to the west of the South Sandwich island arc in the South Atlantic Ocean, consisting of nine main segments, E1 (north) to E9 (south). Major and trace element and Sr–Nd–Pb isotop
Autor:
N.J. Bruguier, Roy A. Livermore
Publikováno v:
Earth and Planetary Science Letters. 191:129-144
Bathymetric and seismic data show that the southernmost segment of the East Scotia Ridge (segment E9) is anomalous in its curved plan form, and in the presence of a large axial volcanic ridge (AVR). Spreading commenced only within the past 1 million
Hydrothermal plumes above the East Scotia Ridge: an isolated high-latitude back-arc spreading centre
Autor:
Peter Morris, Paul A. Tyler, Edward T. Baker, Chris German, Peter J. Statham, I.P. Rouse, Alex P. Cunningham, Roy A. Livermore, N.I. Bruguier, Douglas P. Connelly
Publikováno v:
Earth and Planetary Science Letters. 184:241-250
We have identified first evidence for the presence of submarine hydrothermal activity along the East Scotia Ridge an isolated back-arc spreading centre located at 55–60°S in the Atlantic sector of the Southern Ocean. Using a combination of in situ
Publikováno v:
Journal of Geophysical Research: Solid Earth. 105:8279-8296
The Bouvet triple junction has been proposed to have evolved as a ridge-fault-fault (RFF) type between 20 and 10 Ma, connecting the southernmost Mid-Atlantic Ridge (SMAR) with the Bouvet and Conrad transforms, to the east and west, respectively. We s
Autor:
Jesús Galindo-Zaldívar, Roy A. Livermore, Emma Suriñach, Antonio Barnolas, César Viseras, Luis Somoza, J. C. Balanyá, José Miguel Martínez-Martínez, Andrés Maldonado, Antonio Jabaloy, José Rodríguez-Fernández, Carlos Sanz de Galdeano, Javier Jesús Ramírez Hernández
Publikováno v:
Marine Geophysical Researches. 21:43-68
New swath bathymetric, multichannel seismic and magnetic data reveal the complexity of the intersection between the extinct West Scotia Ridge (WSR) and the Shackleton Fracture Zone (SFZ), a first-order NW-SE trending high-relief ridge cutting across
Publikováno v:
Journal of African Earth Sciences. 29:153-163
The Falkland Islands are one segment of the Permo-Triassic Gondwanian Fold Belt that was displaced during the fragmentation of Gondwana. Palaeomagnetic, structural and palaeocurrent data, reviewed in this paper, provide convincing evidence that the F