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• Journal article
  Buratti N, Stafford PJ, Bommer JJ, 2010,

  Earthquake accelerogram selection and scalingprocedures for estimating the distribution of structural response

  , Journal of Structural Engineering - ASCE
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• Journal article
  Bal IE, Bommer JJ, Stafford PJ, Crowley H, Pinho Ret al., 2010,

  The influence of geographicalresolution of urban exposure data in an Earthquake Loss Model

  , Earthquake Spectra
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• Journal article
  Walker C, Stafford PJ, 2010,

  The use of modal combination rules with cable-stayedbridges

  , Proceedings of the Institution of Civil Engineers - Bridge Engineering
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• Journal article
  Farrell PE, Piggott MD, Gorman GJ, Ham DA, Wilson CRet al., 2010,

  Automated continuous verification and validation for numerical simulation

  , Geoscientific Model Development Discussions, Vol: 3, Pages: 1587-1623
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• Conference paper
  Southern J, Gorman GJ, Piggott MD, Farrell PE, Bernabeu MO, Pitt-Francis Jet al., 2010,

  Anisotropic mesh adaptivity for cardiac electrophysiology

  , Pages: 929-938-929-938
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• Journal article
  Bell RE, Sutherland R, Barker DHN, Henrys SA, Bannister SC, Wallace LM, Beavan RJet al., 2010,

  Seismic reflection character of the Hikurangi subduction interface, New Zealand, in the regionof repeated Gisborne slow slip events

  , Geophysical Journal International, Vol: 180, Pages: 34-48
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• Journal article
  Wallace LM, Bell RE, Townend J, Ellis S, Bannister S, Henrys S, Sutherland R, Barnes Pet al., 2010,

  Subduction Systems Revealed: Studies of the Hikurangi Margin

  , EOS, Transactions American Geophysical Union, Vol: 91
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• Journal article
  Vinogradov J, Jaafar MZ, Jackson MD, 2010,

  Measurement of Streaming Potential Coupling Coefficient in Sandstones Saturated with Natural and Artificial Brines at High Salinity

  , Journal of Geophysical Research
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• Journal article
  Glover PWJ, Jackson MD, 2010,

  Borehole electrokinetics

  , The Leading Edge, Vol: 29, Pages: 724-728
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• Conference paper
  Kieft RL, Jackson CA-L, Hampson GJ, Larsen Eet al., 2010,

  Sedimentology and sequence stratigraphy of the Hugin Formation, Quadrant 15, Norwegian sector, South Viking Graben

  , 7th Petroleum Geology Conference (PGC), Publisher: GEOLOGICAL SOC PUBLISHING HOUSE, Pages: 157-176, ISSN: 2047-9921
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  • Citations: 23
• Journal article
  Bommer JJ, Stafford PJ, Akkar S, 2010,

  Current empirical ground-motion prediction equations for Europe and their application to Eurocode 8

  , Bulletin of Earthquake Engineering, Vol: 8, Pages: 5-26
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• Journal article
  Mitchell AJ, Ulicny D, Hampson GJ, Allison PA, Gorman GJ, Piggott MD, Wells MR, Pain CCet al., 2010,

  Modelling tidal current-induced bed shear stress and palaeocirculation in an epicontinental seaway: the Bohemian Cretaceous Basin, Central Europe

  , Sedimentology, Vol: 57, Pages: 359-388, ISSN: 0037-0746
  • Publisher Web Link
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• Conference paper
  Foulser-Piggott R, Stafford PJ, 2010,

  Incorporation of the spatial correlation of Arias intensity within Earthquake Loss Estimation

  , 5th International Conference on Recent Advances in Geotechnical Earthquake Engineering and Soil Dynamics
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• Journal article
  Mitchell AJ, Allison PA, Piggott MD, Gorman GJ, Pain CC, Hampson GJet al., 2010,

  Numerical modelling of tsunami propagation with implications for sedimentation in ancient epicontinental seas: the Lower Jurassic Laurasian Seaway

  , Journal of Sedimentary Geology, Vol: 228, Pages: 81-97, ISSN: 0037-0738
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• Conference paper
  Dorra EM, Stafford PJ, Elghazouli AY, 2010,

  Seismic loss assessment for buildings and infrastructure in Greater Cairo

  , 14th European Conference on Earthquake Engineering
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• Journal article
  Leinov E, Vinogradov J, Jackson MD, 2010,

  Salinity Dependence of the Thermoelectric Coupling Coefficient in Brine-Saturated Sandstones

  , Geophysical Research Letters
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• Conference paper
  Yan H, Liu J-G, 2010,

  ROBUST SUB-PIXEL DISPARITY ESTIMATION AND ITS REFINEMENT AROUND DEPTH DISCONTINUITY AND FEATURELESS AREAS

  , IEEE International Geoscience and Remote Sensing Symposium, Publisher: IEEE, Pages: 4576-4579
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  • Citations: 3
• Journal article
  Jackson CA-L, Kane KE, Larsen E, 2010,

  Structural evolution of minibasins on the Utsira High, northern North Sea; implications for Jurassic sediment dispersal and reservoir distribution

  , Petroleum Geoscience, Vol: 16, Pages: 105-120

  3D seismic and well data are integrated to determine the tectonostratigraphicevolution of the SW margin of the Utsira High, northern North Sea riftsystem. During the Triassic, a series of minibasins formed due to passive diapirismof the evaporite-bearing, Upper Permian, Zechstein Supergroup. Subsequently,during the Jurassic, a series of secondary minibasins developed as the underlying saltwalls collapsed. These minibasins were a few hundred metres deep, bound bysub-circular to elongate salt-cored structural highs and caused the development ofcomplex subaerial topography and submarine bathymetry on the SW margin of theUtsira High. Salt withdrawal may have been related to: (i) partial dissolution of salt;(ii) differential erosion of the salt walls and adjacent Triassic-filled minibasins; or (iii)salt remigration caused by sub- or supra-salt extension or sediment loading. Thisstudy provides insights into the tectono-stratigraphic evolution of the SW margin ofthe Utsira High and has implications for (i) facies distribution of the ZechsteinSupergroup within the northern North Sea rift system; and (ii) depositional systemdevelopment, and thus reservoir distribution, within the Jurassic sedimentarysuccession.

  • Abstract
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• Conference paper
  Schütz R, Potts DM, Zdravković L, 2009,

  A constitutive model for the behaviour of shotcrete

  , Pages: 49-60

  A constitutive model for the behaviour of shotcrete is presented in this paper. It is formulated within the framework of elasto-plasticity and the smeared crack concept is applied. Two independent yield surfaces govern the mechanical behaviour under compression and tension, which is further controlled by non-linear hardening and softening. The main material parameters are assumed to change with time. Validation of the model has been achieved by fitting the increase in stiffness and strength to published data in the literature. Good agreement is found between predictions of the complete stress-strain curves of shotcrete at different ages and experimental results. The model represents a sophisticated tool for the realistic analysis of tunnels, which are driven according to the principles of the New Austrian Tunnelling Method (NATM).

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• Journal article
  Jackson CA-L, Johnson HD, Zakaria AA, Tongkul F, Crevello PDet al., 2009,

  Sedimentology, stratigraphic occurrence and origin of linked debrites in the West Crocker Fm (Oligo-Miocene), Sabah, NW Borneo

  , Marine and Petroleum Geology, Vol: 26, Pages: 1957-1973

  The West Crocker Fm (Oligocene-Early Miocene), NW Borneo, consists of a large (>20000 km2) submarine fan deposited as part of an accretionary complex. A range of gravity-flow deposits are observed, the most significant of which are mud-poor, massive sandstones interpreted as turbidites and clast-rich, muddy sandstones and sandy mudstones interpreted as debrites. An upward transition from turbidite to debrite is commonly observed, with the contact being either gradational and planar, or sharp and highly erosive. Their repeated vertical relationship and the nature of the contact between them, these intervals are interpreted as being deposited from one flow event which consisted of two distinct flow phases (fully turbulent turbidity current and weakly turbulent to laminar debris flow). The associated bed is called a co-genetic turbidite-debrite, with the upper debrite interval termed a linked debrite. Linked debrites indicates are best developed in the non-channelised parts of the fan system, and are absent to poorly-developed in the proximal channel-levee and distal basin floor environments. Due to outcrop limitations, the genesis of linked debrites within the West Crocker Formation is unclear. Based on clast size and type, it seems likely that a weakly turbulent to laminar debris-flow flow phase was present when the flow event entered the basin. A change in flow behaviour may have led to deposition of a sand-rich unit with ‘turbidite’ characteristics, which was subsequently overlain by a mud-rich unit with ‘debrite’ characteristics. Flow transformation may have been enhanced by the disintegration and incorporation into the flow of muddy clasts derived from the upstream channel floor, channel mouth or from channel levee collapse. Lack of preservation of this debrite in proximal areas may indicate either bypass of this flow phase or that the available outcrops fail to capture the debris flow entry point. Establishing robust sedimentological c

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