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  • 1
    Online Resource
    Online Resource
    Cambridge :Cambridge University Press,
    Keywords: Plate tectonics. ; Electronic books.
    Description / Table of Contents: This book surveys tectonic landforms on solid bodies throughout the Solar System. It discusses the properties and processes that explain the variety of structures observed, and provides methods for mapping and analysing these features. Illustrated with diagrams and spectacular planetary images, this is an essential reference volume.
    Type of Medium: Online Resource
    Pages: 1 online resource (556 pages)
    Edition: 1st ed.
    ISBN: 9780511692093
    Series Statement: Cambridge Planetary Science Series ; v.Series Number 11
    DDC: 551
    Language: English
    Note: Cover -- Half-title -- Series-title -- Title -- Copyright -- Contents -- Contributors -- Preface -- 1 Planetary tectonics: introduction -- Summary -- 1 Introduction -- 2 Terrestrial planets -- 2.1 Mercury -- 2.2 Venus -- 2.3 The Moon -- 2.4 Mars -- 3 Small bodies of the solar system -- 4 Outer planet satellites -- 5 Structural mapping on planetary bodies -- 6 Planetary lithospheres -- 7 Planetary fault populations -- 8 Conclusions -- 2 The tectonics of Mercury -- Summary -- 1 Introduction -- 2 Tectonic features of Mercury -- 2.1 Topographic data -- 2.2 Mapping tectonic features -- 2.3 Lobate scarps -- 2.3.1 Topography of lobate scarps -- 2.3.2 Spatial and temporal distribution of lobate scarps -- 2.3.3 Geometry of lobate scarp thrust faults -- 2.3.4 Displacement-length relationship of lobate scarp thrust faults -- 2.3.5 Influence of buried basins on lobate scarps -- 2.4 High-relief ridges -- 2.5 Wrinkle ridges -- 2.5.1 Topography of wrinkle ridges -- 2.5.2 Spatial distribution of wrinkle ridges on Caloris exterior plains -- 2.6 Wrinkle ridges in the Caloris basin -- 2.7 Caloris basin graben -- 2.8 Summary -- 3. Mechanical and thermal structure of Mercury's crust and lithosphere -- 3.1 Introduction -- 3.2 Thermal structure -- 3.3 Elastic thickness -- 3.4 Fault properties -- 3.5 Summary -- 4. Mechanical and thermal structure of the Caloris basin -- 4.1 Caloris wrinkle ridges and the brittle-ductile transition depth -- 4.2 Strain and depth of faulting of extensional troughs -- 4.3 Caloris loading history -- 4.3.1 Wrinkle ridges -- 4.3.2 Extensional troughs, exterior loading, and lateral crustal flow -- 4.4 Elastic thickness -- 4.5 Stresses -- 4.6 Summary -- 5 Global implications -- 5.1 Fault distribution -- 5.2 Rigidity -- 5.3 Amount of strain and contraction -- 5.4 Sources of stress -- 5.4.1 Contraction -- 5.4.2 Thermal stresses -- 5.4.3 Despinning. , 5.4.4 True polar wander -- 5.4.5 Convection -- 5.4.6 Buoyancy forces -- 5.5 Thermal evolution -- 5.6 Summary -- 6 Conclusions -- Acknowledgments -- References -- 3 Venus tectonics -- Summary -- 1 Introduction -- 2 Tectonic landforms and terrains -- 2.1 Introduction -- 2.2 Plains -- 2.2.1 Distributed deformation -- 2.2.1.1 Wrinkle ridges -- 2.2.1.2 Lineaments and grabens -- 2.2.1.3 Polygonal terrains -- 2.2.2 Concentrated deformation (deformation belts) -- 2.2.2.1 Ridge belt -- 2.2.2.2 Fracture belts -- 2.2.3 Broad-scale vertical deformation -- 2.2.3.1 Stealth ridges -- 2.2.3.2 Regional crustal movements -- 2.3 Volcanic rises -- 2.4 Tessera terrain and crustal plateaus -- 2.4.1 Tessera terrain -- 2.4.2 Crustal plateaus -- 2.4.2.1 Ishtar Terra -- 2.5 Coronae -- 2.6 Chasmata -- 3 Models -- 3.1 Geological models -- 3.2 Geophysical models -- 4 Conclusions -- Acknowledgments -- References -- 4 Lunar tectonics -- Summary -- 1 Introduction -- 2 Tectonic features of Moon -- 2.1 Wrinkle ridges -- 2.1.1 Topography of wrinkle ridges -- 2.1.2 Elevation offsets across wrinkle ridges -- 2.1.3 Subsurface structure at wrinkle ridges -- 2.2 Lunar graben -- 2.2.1 Topography of lunar graben -- 2.2.2 Crater floor graben -- 2.2.3 Rupes Recta normal fault -- 2.3 Lunar scarps -- 2.3.1 Topography of lunar scarps -- 2.4 Wrinkle ridge - lobate scarp transitions -- 2.5 Displacement-length relationships of lunar tectonic features -- 3 Timing of wrinkle-ridge, graben, and lobate scarp formation -- 4 Lunar seismicity -- 4.1 Deep moonquakes -- 4.2 Shallow moonquakes -- 5 Internal structure of the Moon -- 5.1 Seismological constraints -- 5.2 Constraints from gravity and topography -- 6. Basin-localized tectonics and seismicity -- 6.1 Lithospheric structure beneath mare basins -- 6.2 Predictions for tectonic deformation -- 6.3 Basin-localized seismicity. , 7 Global strain from young lobate scarps -- 8 Conclusions and outstanding questions -- Acknowledgments -- References -- 5 Mars tectonics -- Summary -- 1 Introduction -- 2 Global geology, topography and gravity -- 2.1 Physiography -- 2.2 Shape of Mars and crustal structure -- 2.3 Gravity field and lithospheric structure -- 2.4 Core, magnetic field, and true polar wander -- 3 Tectonic features -- 3.1 Extensional structures -- 3.2 Compressional structures -- 3.3 Strike-slip faults -- 4 Tectonic history, orientation and distribution of structures -- 4.1 Alba Patera and Ceraunius Fossae -- 4.2 Structures associated with volcanoes -- 4.3 Tempe Terra -- 4.4 Lunae and Solis Plana -- 4.5 Valles Marineris and Noctis Labyrinthus -- 4.6 Claritas Fossae, Thaumasia, and Sirenum -- 4.7 Western hemisphere tectonic history -- 4.8 Eastern hemisphere -- 4.9 Northern plains -- 5 Tharsis geodynamical models and comparisons to tectonics -- 5.1 Models for the origin of Tharsis -- 5.2 Models for deformation on an elastic spherical shell -- 5.3 Tharsis-induced stress and strain from elastic shell models -- 6 Models and tectonic comparisons: other global-scale features -- 6.1 Models for global isotropic stress and strain -- 6.2 Models for origin of the global dichotomy -- 7 Concluding remarks -- Acknowledgments -- References -- 6 Tectonics of small bodies -- Summary -- 1 Introduction: types of small bodies, their properties, and environments -- 2 Small bodies: characteristics -- 2.1 Asteroids -- 2.2 Comets -- 2.3 Small satellites -- 3 Stress environments of small bodies -- 3.1 Impact environment -- 3.2 Tidal stresses -- 3.3 Thermal stresses -- 4 Observing structures in small bodies: methods and limitations -- 5 Accretional and precursor body structures -- 5.1 Layers in small bodies -- 5.2 Binary objects -- 5.3 Differentiation -- 6 Interior structure from impacts. , 6.1 "Rubble piles" -- 6.2 Porosity -- 6.3 Center of mass - center of figure offsets: significance for structure -- 7 Morphology of surface expressions of structures -- 7.1 Grooves -- 7.2 Troughs -- 7.3 Ridges -- 7.4 Crater shape modification -- 8 Implications of grooves for structure and material properties -- 9 Patterns of linear features and inferred structures -- 9.1 Phobos grooves: impact andor tidal stresses? -- 9.2 Eros grooves: no single pattern -- 9.3 Ida grooves: antipodal effects? -- 9.4 Gaspra structures -- 10 Overview and outstanding questions -- Acknowledgments -- Glossary -- References -- 7 Tectonics of the outer planet satellites -- Summary -- 1 Introduction -- 2 Rheology of ice -- 2.1 Introduction -- 2.2 Elastic deformation -- 2.3 Brittle deformation -- 2.4 Ductile deformation -- 2.5 Viscoelastic behavior -- 2.6 Application to icy satellites -- 2.7 Comparison with silicate behavior -- 3 Global and local stress mechanisms -- 3.1 Background -- 3.1.1 Satellite figures -- 3.1.2 Rigidity and effective elastic thickness -- 3.1.3 Tides -- 3.2 Global stress mechanisms -- 3.2.1 Diurnal tides -- 3.2.2 Nonsynchronous rotation -- 3.2.3 Polar wander -- 3.2.4 Despinning -- 3.2.5 Orbital recession and decay -- 3.2.6 Volume change -- 3.3 Local stress mechanisms -- 3.3.1 Convection -- 3.3.2 Lateral pressure gradients -- 3.3.3 Flexure -- 3.3.4 Impacts -- 4 Io -- 4.1 Tectonic features on Io -- 4.1.1 Fractures -- 4.1.2 Ridges -- 4.1.3 Mountains -- 4.2 Global distribution of mountains and volcanoes -- 5 Active icy satellites -- 5.1 Europa -- 5.1.1 Tectonics of Europa's landforms -- 5.1.1.1 Isolated troughs -- 5.1.1.2 Normal faults -- 5.1.1.3 Ridges -- 5.1.1.4 Bands -- 5.1.1.5 Folds -- 5.1.2 Nonsynchronous rotation of Europa's ice shell -- 5.1.3 Diurnal tidal variations -- 5.1.4 Is Europa currently active? -- 5.2. Enceladus -- 5.3 Triton -- 5.3.1. Ridges. , 5.3.2. Tectonic interactions with cryovolcanic deposits -- 5.3.3. Current activity -- 6 Formerly active icy satellites -- 6.1 Ganymede -- 6.1.1. Dark terrain -- 6.1.2 Bright terrain -- 6.1.3 Implications for Ganymede evolution -- 6.2 Miranda -- 6.3 Ariel -- 6.4 Dione, Tethys, Rhea, and Titania -- 7 Satellites without widespread tectonic activity -- 7.1 Titan -- 7.2 Callisto -- 7.3 Mimas and Iapetus -- 7.4 Other satellites -- 8 Conclusions -- Acknowledgments -- References -- 8 Planetary structural mapping -- Summary -- 1. Introduction -- 2 Mapping and dating structures with spacecraft data -- 2.1 Mapping with visible and infrared images -- 2.2 Mapping with radar images -- 2.3 Mapping with topography -- 3 Structure mapping of planetary bodies -- 3.1 Moon -- 3.2 Mars -- 3.3 Mercury -- 3.4 Venus -- 3.5 Outer planet satellites -- Acknowledgments -- References -- 9 Strength and deformation of planetary lithospheres -- Summary -- 1 Introduction -- 1.1 Flow of rocks: Europa and Ganymede -- 1.2 Mechanisms of deformation -- 1.2.1 Deformation by ionic diffusion coupled with grain boundary sliding -- 1.2.2 Deformation by dislocation processes -- 1.2.3 Deformation by dislocation processes coupled with grain boundary sliding -- 1.2.4 Creep of ice I -- 1.3 Application to Europa and Ganymede -- 2 Strength envelopes: Venus -- 2.1 The strength envelope model -- 2.1.1 Brittle deformation -- 2.1.2 Semi-brittle deformation -- 2.1.3 Plastic flow -- 2.1.4 Water weakening -- 2.1.5 Strength envelope for oceanic lithosphere -- 2.1.6 Strength envelope for continental lithosphere -- 2.1.7 Localization -- 2.1.8 Lithospheric deformation: the global picture -- 2.2 Application to Venus -- 2.2.1 The role of water -- 2.2.2 Strength envelopes for Venus -- 3 Water weakening: Mars -- 3.1 Deformation under hydrous conditions -- 3.1.1 The von Mises criterion and the role of water. , 3.1.2 Comparison of deformation under anhydrous and hydrous conditions.
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  • 2
    Keywords: Underground storage Technological innovations ; Energy storage Technological innovations ; Geological carbon sequestration Technological innovations ; Gas reservoirs Forecasting ; Energy security Forecasting ; Stockage souterrain - Innovations ; Énergie - Stockage - Innovations ; Piégeage du carbone géologique - Innovations ; Réservoirs de gaz naturel (Géologie) - Prévision ; Sécurité énergétique - Prévision ; Case studies ; Case studies ; Études de cas
    Description / Table of Contents: "The secure storage of energy and carbon dioxide in subsurface geological formations plays a crucial role in transitioning to a low-carbon energy system. The suitability and security of subsurface storage sites rely on the geological and hydraulic properties of the reservoir and confining units. Additionally, their ability to withstand varying thermal, mechanical, hydraulic, biological and chemical conditions during storage operations is essential. Each subsurface storage technology has distinct geological requirements and faces specific economic, logistical, public and scientific challenges. As a result, certain sites can be better suited than others for specific low-carbon energy applications. This Special Publication provides a summary of the state of the art in subsurface energy and carbon dioxide storage. It includes 20 case studies that offer insights into site selection, characterization of reservoir processes, the role of caprocks and fault seals, as well as monitoring and risk assessment needs for subsurface storage operations"--Publisher's description
    Type of Medium: Book
    Pages: vii, 514 Seiten , Illustrationen, Karten, Diagramme , 26 cm
    ISBN: 9781786205766 , 1786205769
    Series Statement: Geological Society special publication no. 528
    Language: English
    Note: Includes bibliographical references and index , Sections: Overarching topics -- Site selection and characterization -- Reservoir processes -- Caprocks and fault seals -- Monitoring and risk assessment -- New subsurface storage concepts.
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  • 3
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 341 (1989), S. 424-426 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The inferred strike-slip faults deform moderately cratered plains of presumed volcanic origin south-east of Valles Marineris in Coprates8 (Fig. 1). Wrinkle ridges of north-south strike also deform plains materials throughout the area (Fig. 2). The strike-slip faults are defined by a series of ...
    Type of Medium: Electronic Resource
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  • 4
    Publication Date: 2011-05-01
    Description: Previous theoretical work has suggested that porous sedimentary rocks subjected to sufficiently high strain rates may not form deformation band damage zones (DBDZs). This hypothesis is evaluated by an examination of faults within the porous Navajo Sandstone at the Upheaval Dome impact structure in Canyonlands National Park, southeastern Utah, where high strain-rate conditions are known to have occurred. We found no evidence for DBDZ formation along the accessible fault planes at Upheaval Dome. Instead, a layer of pulverized quartz grains within the Navajo Sandstone occurs adjacent to the fault planes. Similar material has been observed in association with dynamic rupture in crystalline and sedimentary rocks along the San Andreas fault in southern California and in metamorphic rocks along the Bosman fault in South Africa. Measured grain sizes obtained from the pulverized material collected at Upheaval Dome are consistent with strain rates of [~]1-3 x 103 s-1. Pulverized sedimentary rocks along the San Andreas fault imply strain rates of [~]10-2 to 101 s-1. Strain rates along the faults at Upheaval Dome are well above the average values associated with intraplate tectonics but are consistent with, or faster than, seismic slip rates along faults such as the San Andreas fault. Our results support the hypothesized rate dependence of deformation in porous rocks.
    Print ISSN: 0016-7606
    Electronic ISSN: 1943-2674
    Topics: Geosciences
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