Publications
197 results found
Cheadle MJ, McGeary S, Warner MR, et al., 1987, Extensional structures on the western UK continental shelf: a review of evidence from deep seismic profiling., Continental extensional tectonics, Pages: 445-465
BIRPS deep seismic reflection data show the existence of a wide variety of sedimentary basins, most of which originated during Palaeozoic-Mesozoic crustal extension. Symmetrical interior- fracture basins are numerous, but more complex basins are also common and show the importance of fault reactivation and the influence of pre-existing structures on basin development. The relatively small amount of extension which has affected this region suggests that the highly reflective lower crust is more likely to be due to lithological variation formed by mafic igneous intrusion and underplating during crustal extension than to-extensional ductile fabrics within the lower crust.-from Authors Bullard Lab., Dept. of Earth Sci., Univ. of Cambridge, Madingley Rd., Cambridge CB3 0EX, UK.
WARNER MR, 1985, DEEP REFLECTIONS FROM THE UPPER MANTLE, Publisher: BLACKWELL SCIENCE LTD, Pages: 338-338, ISSN: 0016-8009
JONES RH, WARNER MR, 1985, WHY IS THE OUTER ISLES THRUST REFLECTIVE, Publisher: BLACKWELL SCIENCE LTD, Pages: 338-338, ISSN: 0016-8009
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- Citations: 1
MCGEARY S, WARNER MR, 1985, SEISMIC PROFILING THE CONTINENTAL LITHOSPHERE, NATURE, Vol: 317, Pages: 795-797, ISSN: 0028-0836
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- Citations: 105
Hall J, Brewer JA, Matthews DH, et al., 1984, Crustal structure across the Caledonides from the ‘WINCH’ seismic reflection profile: Influences on the evolution of the Midland Valley of Scotland, Transactions of the Royal Society of Edinburgh: Earth Sciences, Vol: 75, Pages: 97-109, ISSN: 0263-5933
The Western Isles-North Channel (‘WINCH’) deep seismic reflection profile runs through the North Channel across the extension of the Midland Valley into the Firth of Clyde. A variety of shallow Carboniferous and younger sedimentary basins dominates the upper crustal structure. The deep structure includes a reflective lower crust, bounded downwards by the Moho, and dipping ‘thrusts-. No margins to the Midland Valley are observed equivalent to the bounding faults on land. Thrusts below both the Highlands and the Southern Uplands have a variety of dip directions indicative of zig-zag crustal shortening of 100 km in the Highlands and 60 km in the Southern Uplands. The Moho varies only a little in depth, despite the gross crustal deformation in the Caledonides. Isostatic recovery of the Moho on unlocking of collided crustal blocks may explain the formation of some sedimentary basins. © 1984, Royal Society of Edinburgh. All rights reserved.
BARTON P, MATTHEWS D, HALL J, et al., 1984, MOHO BENEATH THE NORTH-SEA COMPARED ON NORMAL INCIDENCE AND WIDE-ANGLE SEISMIC RECORDS, NATURE, Vol: 308, Pages: 55-56, ISSN: 0028-0836
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- Citations: 36
WARNER MR, MATTHEWS DH, 1984, ACQUISITION AND PROCESSING DEEP SEISMIC-REFLECTION LINES WINCH AND SWAT, Publisher: BLACKWELL SCIENCE LTD, Pages: 300-300, ISSN: 0016-8009
HALL J, POWELL DW, WARNER MR, et al., 1984, SEISMOLOGICAL EVIDENCE FOR SHALLOW CRYSTALLINE BASEMENT IN SOUTHERN UPLANDS, SCOTLAND - REPLY, NATURE, Vol: 309, Pages: 89-90, ISSN: 0028-0836
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- Citations: 2
BREWER JA, MATTHEWS DH, WARNER MR, et al., 1983, BIRPS DEEP SEISMIC-REFLECTION STUDIES OF THE BRITISH-CALEDONIDES, NATURE, Vol: 305, Pages: 206-210, ISSN: 0028-0836
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- Citations: 156
HALL J, POWELL DW, WARNER MR, et al., 1983, SEISMOLOGICAL EVIDENCE FOR SHALLOW CRYSTALLINE BASEMENT IN THE SOUTHERN UPLANDS OF SCOTLAND, NATURE, Vol: 305, Pages: 418-420, ISSN: 0028-0836
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- Citations: 31
WARNER MR, HIPKIN RG, BROWITT CWA, 1982, SOUTHERN UPLANDS SEISMIC REFRACTION PROFILE - PRELIMINARY-RESULTS, Publisher: BLACKWELL SCIENCE LTD, Pages: 279-279, ISSN: 0016-8009
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- Citations: 1
Edwards SF, Warner M, Warner M, 1979, A dislocation theory of crystal melting and of glasses, Philosophical Magazine A: Physics of Condensed Matter, Structure, Defects and Mechanical Properties, Vol: 40, Pages: 257-278, ISSN: 0141-8610
The dislocation theory of the liquid state is refined by an accurate assessment of the interaction energy between dislocations. This shows a screening phenomenon which gives a first-order transition rather than the second-order transition of simpler theories. Within this framework, a theory of glass is constructed in which the dislocation network is taken to have a long relaxation time and can be frozen in, whilst other effects such as vibrations attain thermal equilibrium. Such an idealization permits a calculation of glass thermodynamics. © 1979 Taylor & Francis Group, LLC.
WARNER MR, 1979, LONGITUDINAL STRUCTURE OF PI2 MICROPULSATIONS, Publisher: WILEY-BLACKWELL, Pages: 298-298, ISSN: 0016-8009
WARNER MR, 1979, PI2 PULSATIONS OBSERVED ON A LATITUDINAL ARRAY, Publisher: WILEY-BLACKWELL, Pages: 298-298, ISSN: 0016-8009
WARNER MR, ORR D, 1979, TIME OF FLIGHT CALCULATIONS FOR HIGH-LATITUDE GEOMAGNETIC-PULSATIONS, PLANETARY AND SPACE SCIENCE, Vol: 27, Pages: 679-689, ISSN: 0032-0633
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- Citations: 92
WARNER MR, ORR D, 1977, LONG PERIOD CONTINUOUS PULSATIONS AT HIGH LATITUDES, Publisher: BLACKWELL SCIENCE LTD, Pages: 299-299, ISSN: 0016-8009
WARNER MR, ORR D, 1977, TIME OF FLIGHT CALCULATIONS OF HIGH LATITUDE GEOMAGNETIC PULSATIONS, Publisher: AMER GEOPHYSICAL UNION, Pages: 722-722, ISSN: 0002-8606
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