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• Conference paper
  Ciesla FJ, Collins GS, Davison TM, O'Brien DPet al., 2009,

  Collisions among porous planetesimals and the water content of planetary embryos

  , 19th Annual VM Goldschmidt Conference, Publisher: Elsevier, Pages: A227-A227, ISSN: 0016-7037
  • Author Web Link
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• Journal article
  Aguera F, Liu JG, 2009,

  Automatic greenhouse delineation from QuickBird and Ikonos satellite images

  , COMPUTERS AND ELECTRONICS IN AGRICULTURE, Vol: 66, Pages: 191-200, ISSN: 0168-1699
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  • Citations: 58
• Journal article
  Amidon WH, Rood DH, Farley KA, 2009,

  Cosmogenic 3He and 21Ne production rates calibrated against 10Be in minerals from the Coso volcanic field

  , Earth and Planetary Science Letters, Vol: 280, Pages: 194-204, ISSN: 0012-821X

  This study calibrates the production rate of cosmogenic ³He in pyroxene, olivine, garnet, zircon and apatite as well as ²¹Ne in quartz and pyroxene against the known production rate of ¹⁰Be in quartz. The Devil's Kitchen rhyolite from the Coso volcanic field in southeastern California (elev. ~ 1300 m) was chosen for this study due to its young age (~ 610 ka) and diverse mineral assemblage. Based on ¹⁰Be, our two rhyolite samples have apparent exposure ages of ~ 49 and 93 ka, indicating substantial erosion after eruption. Combining data from the two samples, we estimate sea level high latitude ³He spallation production rates of 145 ± 11, 141 ± 16, and 144 ± 30 at g^{- 1} a^{- 1} (2σ) for pyroxene, olivine and spessartine garnet respectively. For zircon and apatite, we estimate apparent ³He spallation production rates of 114 ± 8 and 149 ± 28 at g^{- 1} a^{- 1} (2σ) respectively. The rates for zircon and apatite are reported as apparent production rates because we do not explicitly address the redistribution of spallation produced ³He from adjacent minerals. These estimates quantitatively account for production of ³He from both cosmogenic and radiogenic neutron reactions on ⁶Li within the analyzed phases and also implanted from nuclear reactions in neighboring minerals; the high U, Th and Li content of this rhyolite provides a particularly rigorous test of this correction. We estimate ²¹Ne production rates of 17.7 ± 1.6 and 34.1 ± 3.2 at g^{- 1} a^{- 1} (2σ) in quartz and pyroxene (Fe/Mg = 0.7 by mass) respectively. Although high

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  • Citations: 39
• Journal article
  Capitanio FA, Morra G, Goes S, 2009,

  Dynamics of plate bending at the trench and slab-plate coupling

  , GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, Vol: 10, ISSN: 1525-2027
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  • Citations: 98
• Journal article
  Jackson CA-L, Larsen E, 2009,

  Temporal and spatial development of a gravity-driven normal fault array: Middle-Upper Jurassic, South Viking Graben, northern North Sea

  , Journal of Structural Geology, Vol: 31, Pages: 388-402

  Three-dimensional seismic and well data from the South Viking Graben, northern North Sea Basin, is used to investigate the temporal and spatial development of a gravity-driven normal fault array above an evaporite-rich detachment. Two moderate throw (500–900 m), Middle to Upper Jurassic normal faults (the Gudrun and Brynhild Faults) are developed within the study area. Both faults die-out laterally and tip-out upwards at different structural levels within the syn-rift succession. Both faults terminate downwards into Late Permian evaporites (Zechstein Group) and do not offset pre-evaporite basement units. This thin-skinned fault array developed in response to westwards tilting of the hangingwall of the South Viking Graben during Late Jurassic rifting, and consequent westward gliding and extensional break-up of units above the mechanically-weak evaporite horizon. Isochron mapping and well-based correlation of Middle to Upper Jurassic syn-rift units allow constraints to be placed on the temporal evolution of the fault array. Several stages of structural development are observed which document; (i) a period of relatively minor, early (i.e. pre-rift) halokinesis; (ii) variable spatial activity on individual faults within the array; and (iii) the progressive upslope migration of active faulting within the array as a whole. The progressive upslope migration of fault activity is interpreted to reflect progressive “unbuttressing” and extensional faulting of upslope, post-evaporite units. The overall structural style and kinematic evolution identified here shares many characteristics with both ‘rift–raft tectonics’ documented in other rifts developed above an evaporitic sub-stratum and ‘raft tectonics’ described from passive margin basins containing thick mobile salt or shale intervals. This style of fault array evolution differs from that observed in rifts lacking mobile layers at-depth and highlights the importance of these un

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• Journal article
  Fang F, Pain CC, Navon IM, Piggott MD, Gorman GJ, Allison PA, Goddard AJHet al., 2009,

  Reduced-order modelling of an adaptive mesh ocean model

  , INTERNATIONAL JOURNAL FOR NUMERICAL METHODS IN FLUIDS, Vol: 59, Pages: 827-851
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• Journal article
  Boulton SJ, Whittaker AC, 2009,

  Quantifying the slip rates, spatial distribution and evolution of active normal faults from geomorphic analysis: Field examples from an oblique-extensional graben, southern Turkey

  , GEOMORPHOLOGY, Vol: 104, Pages: 299-316, ISSN: 0169-555X
  • Author Web Link
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  • Citations: 68
• Journal article
  Slingo J, Bates K, Nikiforakis N, Piggott M, Roberts M, Shaffrey L, Stevens I, Vidale PL, Weller Het al., 2009,

  Developing the next-generation climate system models: challenges and achievements

  , PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, Vol: 367, Pages: 815-831, ISSN: 1364-503X
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  • Citations: 51
• Journal article
  Ham DA, Farrell PE, Gorman GJ, Maddison JR, Wilson CR, Kramer SC, Shipton J, Collins GS, Cotter CJ, Piggott MDet al., 2009,

  Spud 1.0: generalising and automating the user interfaces of scientific computer models

  , Geoscientific Model Development, Vol: 2, Pages: 33-42

  The interfaces by which users specify the scenarios to be simulated by scientific computer models are frequently primitive, under-documented and ad-hoc text files which make using the model in question difficult and error-prone and significantly increase the development cost of the model. In this paper, we present a model-independent system, Spud, which formalises the specification of model input formats in terms of formal grammars. This is combined with an automated graphical user interface which guides users to create valid model inputs based on the grammar provided, and a generic options reading module, libspud, which minimises the development cost of adding model options. Together, this provides a user friendly, well documented, self validating user interface which is applicable to a wide range of scientific models and which minimises the developer input required to maintain and extend the model interface.

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• Journal article
  Latham JP, Mindel J, Xiang J, Guises R, Garcia X, Pain C, Gorman G, Piggott M, Munjiza Aet al., 2009,

  Coupled FEMDEM/Fluids for coastal engineers with special reference to armour stability and breakage

  , Geomechanics and Geoengineering, Vol: 4, Pages: 39-53, ISSN: 1748-6033
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• Conference paper
  Jardine RJ, 2009,

  Administrative report for TC-29, laboratory stress-strain and strength testing of geomaterials

  , Pages: 3771-3773

  TC-29 has been active since the Osaka Conference. This report describes its Terms of Reference, work and achievements. © 2011 IOS Press.

  • Abstract
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• Journal article
  Nishimura S, Martin CJ, Jardine RJ, Fenton CHet al., 2009,

  A new approach for assessing geothermal response to climate change in permafrost regions

  , GEOTECHNIQUE, Vol: 59, Pages: 213-227, ISSN: 0016-8505
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  • Citations: 14
• Conference paper
  Barker DH, Sutherland R, Henrys SA, Bell REet al., 2009,

  TI: Along-strike Transitions in Subduction Characteristics, Hikurangi Margin, New Zealand

  , AGU Fall Meeting
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• Conference paper
  Stafford PJ, 2009,

  Towards vector implementations of hazard analysis and loss estimation

  , Earthquake Engineering by the Beach, Publisher: RELIUS
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• Journal article
  Jaafar MZ, Vinogradov J, Jackson MD, 2009,

  Measurements of Streaming Potential Coupling Coefficient in Sandstones Saturated with High Salinity NaCl Brine

  , Geophysical Research Letters
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• Book chapter
  Marano GC, Sgobba S, Stafford PJ, Greco Ret al., 2009,

  Seismologically consistent stochastic spectra

  , New Trends in Seismic Design of Structures, Editors: Lagaros, Tsompanakis, Papadrakakis, Publisher: Saxe-Cobourg
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• Conference paper
  Gorman GJ, Pain CC, Piggott MD, Umpleby AP, Farrell PE, Maddison JRet al., 2009,

  Interleaved parallel tetrahedral mesh optimisation and dynamic load-balancing

  , Brussels, Belgium, the fourth International Conference on Adaptive Modeling and Simulation
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• Journal article
  Wallace LM, Reyners M, Cochran U, Bannister S, Barnes P, Berryman K, Downes G, Eberhart-Phillips D, Fagereng A, Ellis S, Nicol A, McCaffrey R, Beavan RJ, Henrys S, Sutherland R, Barker DHN, Litchfield N, Townend J, Robinson R, Bell RE, Wilson K, Power Wet al., 2009,

  Characterizing the seismogenic zone of a major plate boundary subduction thrust: Hikurangi Margin, New Zealand

  , Geochemistry, Geophysics, Geosystems, Vol: 10
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• Journal article
  Bell RE, McNeill LC, Bull JM, Henstock TJ, Collier REL, Leeder MRet al., 2009,

  Fault architecture, basin structure and evolution of the Gulf of Corinth Rift

  , Basin Research, Vol: 21, Pages: 824-855
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• Conference paper
  Bell RE, 2009,

  Hikurangi margin tsunami earthquake generated by slip over a subducted seamount

  , Geosciences '09
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