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  • Conference paper
    Rood DH, Hall S, Guilderson TP, Finkel RC, Brown TAet al., 2010,

    Challenges and opportunities in high-precision Be-10 measurements at CAMS

    , 11th International Conference on Accelerator Mass Spectrometry, Publisher: ELSEVIER SCIENCE BV, Pages: 730-732, ISSN: 0168-583X
  • Journal article
    Schulte P, Alegret L, Arenillas I, Arz JA, Barton PJ, Bown PR, Bralower TJ, Christeson GL, Claeys P, Cockell CS, Collins GS, Deutsch A, Goldin TJ, Goto K, Grajales-Nishimura JM, Grieve RAF, Gulick SPS, Johnson KR, Kiessling W, Koeberl C, Kring DA, MacLeod KG, Matsui T, Melosh J, Montanari A, Morgan JV, Neal CR, Nichols DJ, Norris RD, Pierazzo E, Ravizza G, Rebolledo-Vieyra M, Reimold WU, Robin E, Salge T, Speijer RP, Sweet AR, Urrutia-Fucugauchi J, Vajda V, Whalen MT, Willumsen PSet al., 2010,

    The Chicxulub Asteroid Impact and Mass Extinction at the Cretaceous-Paleogene Boundary

    , SCIENCE, Vol: 327, Pages: 1214-1218, ISSN: 0036-8075
  • Journal article
    Hieronymus CF, Goes S, 2010,

    Complex cratonic seismic structure from thermal models of the lithosphere: effects of variations in deep radiogenic heating

    , GEOPHYSICAL JOURNAL INTERNATIONAL, Vol: 180, Pages: 999-1012, ISSN: 0956-540X
  • Journal article
    TAGGART S, HAMPSON GJ, JACKSON MD, 2010,

    High-resolution stratigraphic architecture and lithological heterogeneity within marginal aeolian reservoir analogues

    , Sedimentology, ISSN: 0037-0746
  • Journal article
    Capitanio FA, Morra G, Goes S, Weinberg RF, Moresi Let al., 2010,

    India-Asia convergence driven by the subduction of the Greater Indian continent

    , NATURE GEOSCIENCE, Vol: 3, Pages: 136-139, ISSN: 1752-0894
  • Journal article
    Monroy R, Zdravkovic L, Ridley A, 2010,

    Evolution of microstructure in compacted London Clay during wetting and loading

    , GEOTECHNIQUE, Vol: 60, Pages: 105-119, ISSN: 0016-8505
  • Journal article
    Amos CB, Kelson KI, Rood DH, Simpson DT, Rose RSet al., 2010,

    Late quaternary slip rate on the Kern Canyon fault at Soda Spring, Tulare County, California

    , Lithosphere, Vol: 2, Pages: 411-417, ISSN: 1941-8264

    The Kern Canyon fault represents a major tectonic and physiographic boundary in the southern Sierra Nevada of east-central California. Previous investigations of the Kern Canyon fault underscore its importance as a Late Cretaceous and Neogene shear zone in the tectonic development of the southern Sierra Nevada. Study of the late Quaternary history of activity, however, has been confounded by the remote nature of the Kern Canyon fault and deep along-strike exhumation within the northern Kern River drainage, driven by focused fl uvial and glacial erosion. Recent acquisition of airborne lidar (light detection and ranging) topography along the ~140 km length of the Kern Canyon fault provides a comprehensive view of the active surface trace. High-resolution, lidar-derived digital elevation models (DEMs) for the northern Kern Canyon fault enable identifi cation of previously unrecognized offsets of late Quaternary moraines near Soda Spring (36.345°N, 118.408°W). Predominately north-striking fault scarps developed on the Soda Spring moraines display west-side-up displacement and lack a signifi cant sense of strike-slip separation, consistent with detailed mapping and trenching along the entire Kern Canyon fault. Scarp-normal topographic profi ling derived from the lidar DEMs suggests normal displacement of at least 2.8 +0.6/-0.5 m of the Tioga terminal moraine crest. Cosmogenic 10 Be exposure dating of Tioga moraine boulders yields a tight age cluster centered around 18.1 ± 0.5 ka (n = 6), indicating a minimum normal-sense fault slip rate of ~0.1-0.2 mm/yr over this period. Taken together, these results provide the fi rst clear documentation of late Quaternary activity on the Kern Canyon fault and highlight its role in accommodating internal deformation of the southern Sierra Nevada. © 2010 Geological Society of America.
  • Conference paper
    Yan H, Liu J-G, 2010,

    ENHANCED ROBUST PHASE CORRELATION BASED SUB-PIXEL FEATURE MATCHINIG FOR TARGET MOTION ESTIMATION

    , 2010 ISPRS Technical Commission III Symposium on Photogrammetry Computer Vision and Image Analysis, Pages: 76-79

    This paper presents an enhanced robust phase correlation (ERPC) algorithm for sub-pixel feature matching and its application intarget motion estimation for aerial video surveillance. The ERPC can cope with very large motion measurement on the one hand andimprove the sub-pixel accuracy by entirely avoiding the ill-posed problem of 2D phase unwrapping in 2D fitting technique of phasecorrelation on the other. The key advantage of EPRC is its robustness and sub-pixel accuracy which are essential for precise targetspeed measurement. Furthermore, EPRC is solely applied to the certain parts (not to the whole scene) of a scene where the movingtargets are detected, which greatly improves robustness and computing speed of the EPRC based target motion estimation. Finally,we introduce our robust camera compensation and moving target detection scheme. With this simple scheme, we are able toefficiently estimate the motions of multiple targets at sub-pixel accuracy.
  • Journal article
    Weller H, Ringler T, Piggott M, Wood Net al., 2010,

    CHALLENGES FACING ADAPTIVE MESH MODELING OF THE ATMOSPHERE AND OCEAN

    , BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY, Vol: 91, Pages: 105-+, ISSN: 0003-0007
  • 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
  • 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
  • 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
  • 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
  • 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
  • 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
  • Journal article
    Garcia X, Pavlidis D, Gorman GJ, Gomes JLMA, Piggott MD, Aristodemou E, Mindel J, Latham JP, Pain CC, ApSimon Het al., 2010,

    A two-phase adaptive finite element method for solid–fluidcoupling in complex geometries

    , International Journal for Numerical Methods in Fluids

    In this paper we present a method to solve the Navier–Stokes equations in complex geometries, suchas porous sands, using a finite-element solver but without the complexity of meshing the porous space.The method is based on treating the solid boundaries as a second fluid and solving a set of equationssimilar to those used for multi-fluid flow. When combined with anisotropic mesh adaptivity, it is possibleto resolve complex geometries starting with an arbitrary coarse mesh. The approach is validated bycomparing simulation results with available data in three test cases. In the first we simulate the flow pasta cylinder. The second test case compares the pressure drop in flow through random packs of sphereswith the Ergun equation. In the last case simulation results are compared with experimental data on theflow past a simplified vehicle model (Ahmed body) at high Reynolds number using large-eddy simulation(LES). Results are in good agreement with all three reference models.
  • Conference paper
    Henrys SA, Sutherland R, Seward A, Hendersen M, Stern TA, Savage MK, Townend J, Mochizuki K, Sato H, Iwasaki T, Bassett D, Bell REet al., 2010,

    The 2009-2010 SAHKE Experiment: Acquisition and preliminary results across the interseismically locked southern Hikurangi margin, New Zealand

    , American Geophysical Union Fall Meeting
  • Conference paper
    Barker DH, Wallace LM, Bell RE, Henrys SAet al., 2010,

    Drilling at the northern Hikurangi subduction margin, New Zealand: The key to unlock the secrets of slip slip events

    , American Geophysical Union Fall Meeting
  • 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
  • Journal article
    Glover PWJ, Jackson MD, 2010,

    Borehole electrokinetics

    , The Leading Edge, Vol: 29, Pages: 724-728

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