Results
- Showing results for:
- Reset all filters
Search results
-
Journal articleBuratti N, Stafford PJ, Bommer JJ, 2010, , Journal of Structural Engineering - ASCE
-
Journal articleBal IE, Bommer JJ, Stafford PJ, et al., 2010,
The influence of geographicalresolution of urban exposure data in an Earthquake Loss Model
, Earthquake Spectra -
Journal articleWalker C, Stafford PJ, 2010,
The use of modal combination rules with cable-stayedbridges
, Proceedings of the Institution of Civil Engineers - Bridge Engineering -
Journal articleFarrell PE, Piggott MD, Gorman GJ, et al., 2010, , Geoscientific Model Development Discussions, Vol: 3, Pages: 1587-1623
-
Conference paperSouthern J, Gorman GJ, Piggott MD, et al., 2010, , Pages: 929-938-929-938
-
Journal articleBell RE, Sutherland R, Barker DHN, et al., 2010, , Geophysical Journal International, Vol: 180, Pages: 34-48
-
Journal articleWallace LM, Bell RE, Townend J, et al., 2010, , EOS, Transactions American Geophysical Union, Vol: 91
-
Journal articleVinogradov J, Jaafar MZ, Jackson MD, 2010, , Journal of Geophysical Research
-
Journal articleGlover PWJ, Jackson MD, 2010, , The Leading Edge, Vol: 29, Pages: 724-728
-
Conference paperKieft RL, Jackson CA-L, Hampson GJ, et al., 2010, , 7th Petroleum Geology Conference (PGC), Publisher: GEOLOGICAL SOC PUBLISHING HOUSE, Pages: 157-176, ISSN: 2047-9921
- Cite
- Citations: 23
-
Journal articleBommer JJ, Stafford PJ, Akkar S, 2010, , Bulletin of Earthquake Engineering, Vol: 8, Pages: 5-26
-
Journal articleMitchell AJ, Ulicny D, Hampson GJ, et al., 2010, , Sedimentology, Vol: 57, Pages: 359-388, ISSN: 0037-0746
-
Conference paperFoulser-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 -
Journal articleMitchell AJ, Allison PA, Piggott MD, et al., 2010, , Journal of Sedimentary Geology, Vol: 228, Pages: 81-97, ISSN: 0037-0738
-
Conference paperDorra EM, Stafford PJ, Elghazouli AY, 2010,
Seismic loss assessment for buildings and infrastructure in Greater Cairo
, 14th European Conference on Earthquake Engineering -
Journal articleLeinov E, Vinogradov J, Jackson MD, 2010, , Geophysical Research Letters
-
Conference paperYan H, Liu J-G, 2010, , IEEE International Geoscience and Remote Sensing Symposium, Publisher: IEEE, Pages: 4576-4579
- Cite
- Citations: 3
-
Journal articleJackson CA-L, Kane KE, Larsen E, 2010, , 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.
-
Conference paperSchütz R, Potts DM, Zdravkovi膰 L, 2009,
A constitutive model for the behaviour of shotcrete
, Pages: 49-60A 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).
-
Journal articleJackson CA-L, Johnson HD, Zakaria AA, et al., 2009, , 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
This data is extracted from the Web of Science and reproduced under a licence from Thomson Reuters. You may not copy or re-distribute this data in whole or in part without the written consent of the Science business of Thomson Reuters.