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  • 1
    Keywords: Faults (Geology) ; Aufsatzsammlung ; Störung ; Deformation ; Strukturgeologie ; Verwerfung ; Faltung ; Tektonik ; Rifting ; Störungstektonik ; Rift ; Abschiebung ; Aufsatzsammlung ; Störung ; Deformation ; Strukturgeologie ; Verwerfung ; Faltung ; Tektonik ; Rifting ; Störungstektonik ; Rift ; Abschiebung ; Aufsatzsammlung
    Description / Table of Contents: Normal faults are the primary structures that accommodate extension of the brittle crust. This volume provides an up-to-date overview of current research into the geometry and growth of normal faults. The 23 research papers present the findings of outcrop and subsurface studies of the geometrical evolution of faults from a number of basins worldwide, complemented by analogue and numerical modelling studies of fundamental aspects of fault kinematics. The topics addressed include how fault length changes with displacement, how faults interact with one another, the controls of previous structure on fault evolution and the nature and origin of fault-related folding. This volume will be of interest to those wishing to develop a better understanding of the structural geological aspects of faulting, from postgraduate students to those working in industry
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (vi, 540 Seiten) , Illustrationen, Diagramme, Karten
    Series Statement: Geological Society special publication no. 439
    DDC: 551.872
    Language: English
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  • 2
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (vii, 504 Seiten) , Illustrationen
    ISBN: 9781786205209
    Series Statement: Cross-border themes in petroleum geology / edited by S. Patruno (University of Nicosia, Cyprus), S.G. Archer (Harbour Energy, UK), D. Chiarella (Royal Holloway, University of London, UK), J.A. Howell (University of Aberdeen, UK), C.A-L. Jackson (University of Manchester, UK) and H. Kombrink (North Sea Core, UK) 1
    Language: English
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  • 3
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (viii, 320 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 9781786204585
    Series Statement: Cross-border themes in petroleum geology / edited by S. Patruno (University of Nicosia, Cyprus), S.G. Archer (Harbour Energy, UK), D. Chiarella (Royal Holloway, University of London, UK), J.A. Howell (University of Aberdeen, UK), C.A-L. Jackson (University of Manchester, UK) and H. Kombrink (North Sea Core, UK) 2
    Language: English
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  • 4
    ISSN: 1524-475X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Medicine
    Notes: Activated protein C (APC) is a serine protease that plays a central role in physiological anticoagulation, and has more recently been shown to be a potent anti-inflammatory mediator. Using cultured human cells, we show here that APC up-regulates the angiogenic promoters matrix metalloproteinase-2 in skin fibroblasts and umbilical vein endothelial cells, vascular endothelial growth factor in keratinocytes and fibroblasts, and monocyte chemoattractant protein-1 in fibroblasts. In the chick embryo chorioallantoic membrane assay, APC promoted the granulation/remodeling phases of wound healing by markedly stimulating angiogenesis as well as promoting reepithelialization. In a full-thickness rat skin-healing model, a single topical application of APC enhanced wound healing compared to saline control. APC-treated wounds had markedly more blood vessels on day 7 and a significantly lower infiltration of neutrophils at days 4 and 7. The broad spectrum matrix metallo-proteinas, GM6001, prevented the ability of APC to promote wound healing. In summary, our results show that APC promotes cutaneous wound healing via a complex mechanism involving stimulation of angiogenesis and inhibition of inflammation. These unique properties of APC make it an attractive therapeutic agent to promote the healing of chronic wounds.
    Type of Medium: Electronic Resource
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  • 5
    ISSN: 1365-3121
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Seismic-stratigraphic analysis of the Cretaceous to succession of the Uer Terrace, North Sea seabed Basin, Norway, demonstrates that the Upper Oligocene succession has undergone large-scale mobilization of mudstone-dominated units due to the upward migration of water and associated hydrocarbons into the interval, which is in some way linked to a period of gas expulsion from adjacent deep basins. Seismic-stratigraphic analysis of units overlying the mobilized zones indicates they created positive seafloor topography during the Late Miocene implying gaseous fluids were expelled at the seabed. Loading by the overlying Pliocene succession caused the mobilized mud masses to deflate and resulted in the formation of low-relief, fault-bounded craters. The results of this study have implications for understanding the location and timing of fluid flow in sedimentary basins.
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 1471-0528
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Medicine
    Notes: Investigation of the pathophysiology of pre-eclampsia (characterised by insufficient invasion of the intrauterine vasculature by cytotrophoblasts) has been hampered by the absence of a suitable animal model, and ethical constraints in clinical studies. We have developed a novel in vitro human cell co-culture system allowing direct assessment of cytotrophoblast invasion of a decidual endothelial cell monolayer from the abluminal side, as occurs in vivo. This model will facilitate detection, at the cellular level, of abnormal endothelial cell–trophoblast functional interactions in pre-eclampsia and other pregnancy disorders with abnormal placentation.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Annals of the New York Academy of Sciences 667 (1992), S. 0 
    ISSN: 1749-6632
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Natural Sciences in General
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Ltd
    Aquaculture research 35 (2004), S. 0 
    ISSN: 1365-2109
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: This study was conducted to help provide a framework for Australian regulation of shrimp farm siting and discharges. Monitoring of farm water usage, and intake and discharge water quality was conducted at three commercial intensive shrimp farms, chosen to represent different operating environments, latitudes, cultured species and management styles. Weekly samples were taken over 3 years, for 3–12 months at each farm, to investigate intake and discharge concentrations and loads of total suspended solids (TSS), total nitrogen (TN) and total phosphorus (TP). Mean water exchange was 1.4 ML ha−1 day−1 (about 10% day−1) at the first farm studied and 0.5 ML ha−1 day−1 (about 3.6% day−1) at the others. Farm mean discharge concentration varied as follows: TSS, from 36.9 to 119 mg L−1; TN, from 2.1 to 3.1 mg L−1 and TP, from 0.22 to 0.28 mg L−1. Farm mean intake concentrations were from 11% to 91% of equivalent mean discharge concentration (for TN at Farm B and TSS at Farm C respectively). Mean net discharge loads, related to area of production ponds at each farm, varied as follows: TSS, from 4.8 to 85.7 kg ha−1 day−1; TN, from 1 to 1.8 kg ha−1 day−1 and TP, from 0.11 to 0.22 kg ha−1 day−1. The highest net loads of TSS, TN and TP were all from the farm with the highest water exchange rate, located on a coastal river, and studied during a year of high rainfall with associated poor water quality. These results can be used to help predict likely discharge characteristics for new shrimp farms, and provide a benchmark against which to evaluate future improvements in shrimp farm environmental management.
    Type of Medium: Electronic Resource
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  • 9
    Publication Date: 2021-07-01
    Description: In regions experiencing multiple phases of extension, rift‐related strain can vary along and across the basin during and between each phase, and the location of maximum extension can differ between the rift phase. Despite having a general understanding of multiphase rift kinematics, it remains unclear why the rift axis migrates between extension episodes. The role pre‐existing structures play in influencing fault and basin geometries during later rifting events is also poorly understood. We study the Stord Basin, northern North Sea, a location characterised by strain migration between two rift episodes. To reveal and quantify the rift kinematics, we interpreted a dense grid of 2D seismic reflection profiles, produced time‐structure and isochore (thickness) maps, collected quantitative fault kinematic data and calculated the amount of extension (β‐factor). Our results show that the locations of basin‐bounding fault systems were controlled by pre‐existing crustal‐scale shear zones. Within the basin, Permo‐Triassic Rift Phase 1 (RP1) faults mainly developed orthogonal to the E‐W extension direction. Rift faults control the locus of syn‐RP1 deposition, whilst during the inter‐rift stage, areas of clastic wedge progradation are more important in controlling sediment thickness trends. The calculated amount of RP1 extension (β‐factor) for the Stord Basin is up to β = 1.55 (±10%, 55% extension). During the subsequent Middle Jurassic‐Early Cretaceous Rift Phase 2 (RP2), however, strain localised to the west along the present axis of the South Viking Graben, with the Stord Basin being almost completely abandoned. Rift axis migration during RP2 is interpreted to be related to changes in lithospheric strength profile, possibly related to the ultraslow extension (〈1 mm/year during RP1), the long period of tectonic quiescence (ca. 50 myr) between RP1 and RP2 and possible underplating. Our results highlight the very heterogeneous nature of temporal and lateral strain migration during and between extension phases within a single rift basin.
    Description: Norges Forskningsråd http://dx.doi.org/10.13039/501100005416
    Keywords: 551.8 ; crustal extension ; multirifted basin ; Northern North Sea ; seismic interpretation ; tectonics and sedimentation
    Type: article
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  • 10
    Publication Date: 2022-05-25
    Description: Author Posting. © The Oceanography Society, 2012. This article is posted here by permission of The Oceanography Society for personal use, not for redistribution. The definitive version was published in Oceanography 25, No. 2 (2012): 108–123, doi:10.5670/oceanog.2012.46.
    Description: Nonlinear internal waves are found in many parts of the world ocean. Their widespread distribution is a result of their origin in the barotropic tide and in the variety of ways they can be generated, including by lee waves, tidal beams, resonance, plumes, and the transformation of the internal tide. The differing generation mechanisms and diversity of generation locations and conditions all combine to produce waves that range in scale from a few tens of meters to kilometers, but with all properly described by solitary wave theory. The ability of oceanic nonlinear internal waves to persist for days after generation and the key role internal waves play in connecting large-scale tides to smaller-scale turbulence make them important for understanding the ocean environment.
    Description: Christopher Jackson gratefully acknowledges the support of the Office of Naval Research through contract N0001409C0224.
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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