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  • 1
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Spektrum, Akad.-Verl.
    Call number: 9/M 10.0228
    Type of Medium: Monograph available for loan
    Pages: XXV, 735 S. , Ill., graph. Darst., Kt.
    Edition: 5. Aufl.
    ISBN: 9783827418128
    Uniform Title: Understanding earth
    Classification:
    Geology
    Language: German
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    New York : W. H. Freeman
    Call number: 4/M 08.0160
    Description / Table of Contents: The fifth edition of "Understanding Earth" continues the book's enduring goal, to help students understand what physical geology teaches us about the world and what it brings to our lives. Two new co-authors have introduced a wealth of recent data and applications to keep the science on the cutting edge. Students will enjoy coming to learn how we know what we know, and how that knowledge impacts our lives as citizens and consumers.
    Type of Medium: Monograph available for loan
    Pages: Getr. Zählung , Ill, Kt. , 28 cm
    Edition: 5th ed.
    ISBN: 0-7167-6682-5 , 978-0-7167-6682-7
    Classification:
    A..
    Language: English
    Note: Meet the Authors ... vi --- Preface ... xiii --- The Modern Theory and Practice of Geology --- The Earth System ... 1 --- The Scientific Method ... 2 --- Earth's Shape and Surface ... 3 --- The Geologic Record ... 4 --- Peeling the Onion: Discovery of a Layered Earth ... 6 --- Earth as a System of Interacting Components ... 10 --- An Overview of Geologic Time ... 14 --- Plate Tectonics: The Unifying Theory ... 18 --- The Discovery of Plate Tectonics ... 19 --- The Mosaic of Plates ... 22 --- Rates and History of Plate Motions ... 30 --- The Grand Reconstruction ... 35 --- Mantle Convection: The Engine of Plate Tectonics ... 37 --- The Theory of Plate Tectonics and the Scientific Method ... 42 --- Basic Geologic Processes --- Earth Materials: Minerals and Rocks ... 44 --- What Are Minerals? ... 45 --- The Atomic Structure of Matter ... 46 --- Chemical Reactions ... 47 --- Chemical Bonds ... 49 --- The Atomic Structure of Minerals ... 49 --- Rock-Forming Minerals ... 52 --- Physical Properties of Minerals ... 56 --- What Are Rocks? ... 62 --- Igneous Rocks ... 63 --- Sedimentary Rocks ... 64 --- Metamorphic Rocks ... 66 --- The Rock Cycle: Interactions Between the Plate Tectonic and Climate Systems ... 66 --- Minerals Occur in Rocks as Valuable Resources ... 68 --- Earth Issues: Sulfide Minerals React to Form Acid Waters on Earth and Mars ... 57 --- Igneous Rocks: Solids from Melts ... 76 --- How Do Igneous Rocks Differ from One Another? ... 78 --- How Do Magmas Form? ... 83 --- Where Do Magmas Form? ... 85 --- Magmatic Differentiation ... 85 --- Forms of Magmatic Intrusions ... 88 --- Igneous Activity and Plate Tectonics ... 91 --- Sedimentation: Rocks Formed by Surface Processes ... 100 --- Sedimentary Rocks Are Produced by Surface Processes in the Rock Cycle ... 102 --- Sedimentary Basins: The Sinks for Sediments ... 106 --- Sedimentary Environments ... 108 --- Sedimentary Structures ... 111 --- Burial and Diagenesis: From Sediment to Rock ... 114 --- Classification of Siliciclastic Sediments and Sedimentary Rocks ... 116 --- Classification of Chemical and Biological Sediments and Sedimentary Rocks ... 119 --- Earth Policy: Darwin's Coral Reefs and Atolls ... 124 --- Metamorphism: Modification of Rocks by Temperature and Pressure ... 130 --- Metamorphism and the Earth System ... 132 --- Causes of Metamorphism ... 133 --- Types of Metamorphism ... 134 --- Metamorphic Textures ... 136 --- Regional Metamorphism and Metamorphic Grade ... 141 --- Plate Tectonics and Metamorphism ... 144 --- Deformation: Modification of Rocks by Folding and Fracturing ... 150 --- Mapping Geologic Structure ... 152 --- How Rocks Deform ... 154 --- Basic Deformation Structures ... 156 --- Styles of Continental Deformation ... 163 --- Unraveling Geologic History ... 165 --- Earth and Planets Through Geologic Time --- Clocks in Rocks: Timing the Geologic Record ... 168 --- Reconstructing Geologic History from the Stratigraphic Record ... 170 --- Geologic Time Scale: Relative Ages ... 178 --- Measuring Absolute Time with Radioactive Clocks ... 180 --- Geologic Time Scale: Absolute Ages ... 183 --- Timing the Earth System ... 184 --- Earth Issues: The Grand Canyon Sequence and Regional Correlation of Strata ... 176 --- Early History of the Terrestrial Planets ... 188 --- Origin of the Solar System ... 190 --- Early Earth: Formation of a Layered Planet ... 192 --- Diversity of the Planets ... 195 --- What's in a Face? The Age and Complexion of Planetary Surfaces ... 197 --- Mars Rocks! ... 204 --- Exploring the Solar System and Beyond ... 210 --- Evolution of the Continents ... 214 --- The Tectonics of North America ... 216 --- Tectonic Provinces Around the World ... 221 --- How Continents Grow ... 224 --- How Continents Are Modified ... 226 --- The Formation of Cratons ... 235 --- The Deep Structure of Continents ... 236 --- Geobiology: Life Interacts with the Earth ... 240 --- The Biosphere as a System ... 242 --- Microbes: Nature's Tiny Chemists ... 246 --- Geobiological Events in Earth's History ... 254 --- Astrobiology: The Search for Extraterrestrial Life ... 265 --- Earth Issues: The Mother of all Mass Extinctions: Whodunit? ... 264 --- Internal Geosystems --- Volcanoes ... 270 --- Volcanoes as Geosystems ... 272 --- Lavas and Other Volcanic Deposits ... 273 --- Eruptive Styles and Landforms ... 277 --- Geosystem Interactions ... 282 --- The Global Pattern of Volcanism ... 284 --- Volcanism and Human Affairs ... 288 --- Earth Policy: Mount St. Helens: Dangerous but Predictable ... 292 --- Earthquakes ... 296 --- What Is an Earthquake? ... 298 --- Studying Earthquakes ... 301 --- Earthquakes and Patterns of Faulting ... 309 --- Earthquake Destructiveness ... 313 --- Can Earthquakes Be Predicted? ... 320 --- Earth Issues: The Great Indian Ocean Tsunami of 2004 ... 312 --- Earth Issues: Seven Steps to Earthquake Safety ... 319 --- Exploring: Earth's Interior ... 324 --- Exploring the Interior with Seismic Waves ... 325 --- Layering and Composition of the Interior ... 328 --- Earth's Internal Heat and Temperature ... 332 --- The Three-Dimensional Structure of the Mantle ... 338 --- Earth's Magnetic Field and the Geodynamo ... 337 --- Earth Issues: The Uplift of Scandinavia: Nature's Experiment with Isostasy ... 331 --- Earth Issues: The Geoid: Shape of Planet Earth ... 338 --- Surficial Geosystems --- The Climate System ... 346 --- Components of the Climate System ... 348 --- The Greenhouse Effect ... 352 --- Climate Variability ... 355 --- The Carbon Cycle ... 362 --- Twentieth-Century Warming: Human Fingerprints of Global Change ... 366 --- Earth Issues: Vostok and GRIP: Ice-Core Drilling in Antarctica and Greenland ... 358 --- Earth Issues: El Nino: The Wayward Child ... 360 --- Weathering, Erosion, and Mass Wasting: Interface Between Climate and Tectonics ... 370 --- Weathering, Erosion, Mass Wasting, and the Rock Cycle ... 372 --- Controls on Weathering ... 372 --- Chemical Weathering ... 373 --- Physical Weathering ... 378 --- Soil: The Residue of Weathering ... 381 --- Mass Wasting ... 384 --- Classification of Mass Movements ... 388 --- Understanding the Origins of Mass Movements ... 395 --- The Hydrologic Cycle and Groundwater ... 400 --- Flows and Reservoirs ... 402 --- Hydrology and Climate ... 404 --- The Hydrology of Runoff ... 406 --- Groundwater ... 408 --- Water Resources from Major Aquifers ... 415 --- Erosion by Groundwater ... 417 --- Water Quality ... 418 --- Water Deep in the Crust ... 421 --- Earth Issues: Water Is a Precious Resource: Who Should Get It? ... 404 --- Earth Issues: When Do Groundwaters Become Nonrenewable Resources? ... 416 --- Stream Transport: From Mountains to Oceans ... 426 --- Stream Valleys, Channels, and Floodplains ... 428 --- Drainage Networks ... 432 --- Where Do Channels Begin? How Running Water Erodes Solid Rock ... 435 --- How Stream Waters Flow and Transport Sediment ... 437 --- Deltas: The Mouths of Rivers ... 440 --- Streams as Geosystems ... 443 --- Earth Issues: The Development of Cities on Floodplains ... 432 --- Winds and Deserts ... 452 --- Wind as a Flow of Air ... 454 --- Wind as a Transport Agent ... 455 --- Wind as an Agent of Erosion ... 458 --- Wind as a Depositional Agent ... 460 --- The Desert Environment ... 464 --- Earth Issues: Martian Dust Storms and Dust Devils ... 457 --- Coastlines and Ocean Basins ... 472 --- Basic Differences Between Ocean Basins and Continents ... 474 --- Coastal Processes ... 474 --- Shorelines ... 485 --- Sea Level Change as a Measure of Global Warming ... 488 --- Continental Margins ... 491 --- The Deep Oceans ... 494 --- Ocean Sedimentation ... 500 --- Earth Policy: The Great New Orleans Flood ... 480 --- Earth Issues: Preserving Our Beaches ... 490 --- Glaciers: The Work of Ice ... 504 --- Ice as a Rock ... 506
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  • 3
    facet.materialart.12
    New York, Basingstoke : Freeman
    Call number: 9781464138744
    Type of Medium: 12
    Pages: 1 Online-Ressource (755 Seiten) , Illustrationen, Diagramme, Karten
    Edition: 7th edition
    ISBN: 978-1-4641-3874-4 , 1-4641-3874-5
    Language: English
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  • 4
    Monograph available for loan
    Monograph available for loan
    New York : Macmillan Learning
    Call number: AWI G1-21-94626
    Type of Medium: Monograph available for loan
    Pages: Getrennte Zählungen , Illustrationen, Karten
    Edition: Eighth edition
    ISBN: 9781319055325 , 9781319325398 , 1319325394
    Former Title: Understanding earth [5th edition]
    Language: English
    Note: Contents About the Authors Preface Chapter 1 The Earth System The Scientific Method Hypothesis and Theory Scientific Models Importance of Scientific Collaboration Geology as a Science Earth's Shape and Surface Peeling the Onion: Discovery of a Layered Earth Earth's Density The Mantle and Core The Crust The Inner Core Chemical Composition of Earth's Major Layers Earth as a System of Interacting Components The Climate System The Plate Tectonic System The Geodynamo Interactions Among Geosystems Support Life An Overview of Geologic Time The Origin of Earth and Its Global Geosystems The Evolution of Life Chapter 2 Plate Tectonics: The Unifying Theory The Discovery of Plate Tectonics Continental Drift Seafloor Spreading The Great Synthesis: 1963-1968 The Plates and Their Boundaries Divergent Boundaries Convergent Boundaries Transform Faults Combinations of Plate Boundaries Rates and History of Plate Movements The Seafloor as a Magnetic Tape Recorder Deep-Sea Drilling Measurements of Plate Movements by Geodesy The Grand Reconstruction Seafloor isochrons Reconstructing the History of Plate Movements The Breakup of Pangaea The Assembly of Pangaea by Continental Drift Implications of the Grand Reconstruction Mantle Convection:The Engine of Plate Tectonics Where Do the Plate-Driving Forces Originate? How Deep Does Plate Recycling Occur? What Is the Nature of Rising Convection Currents? Chapter 3 Earth Materials: Minerals and Rocks What Are Minerals? The Structure of Matter The Structure of Atoms Atomic Number and Atomic Mass Chemical Reactions Chemical Bonds The Formation of Minerals The Atomic Structure of Minerals The Crystallization of Minerals How Do Minerals Form? Classes of Rock-Forming Minerals Silicates Carbonates Oxides Sulfides Sulfates Physical Properties of Minerals Hardness Cleavage Fracture Luster Color Density Crystal Habit What Are Rocks? Properties of Rocks Igneous Rocks Sedimentary Rocks Metamorphic Rocks The Rock Cycle: Interactions Between the Plate Tectonic and Climate Systems Concentrations of Valuable Mineral Resources Hydrothermal Deposits Igneous Deposits Sedimentary Deposits Mineral Evolution Chapter 4 Igneous Rocks: Solids from Melts How Do Igneous Rocks Differ from One Another? Texture Chemical and Mineral Composition How Do Magmas Form? How Do Rocks Melt? The Formation of Magma Chambers Where Do Magmas Form? Magmatic Differentiation Fractional Crystallization: Laboratory and Field Observations Granite from Basalt: Complexities of Magmatic Differentiation Forms of Igneous Intrusions Plutons Sills and Dikes Veins Igneous Processes and Plate Tectonics Spreading Centers as Magma Factories Subduction Zones as Magma Factories Mantle Plumes as Magma Factories Chapter 5 Volcanoes Volcanoes as Geosystems Lavas and Other Volcanic Deposits Types of Lava Textures of Volcanic Rocks Pyroclastic Deposits Eruptive Styles and Landforms Central Eruptions Fissure Eruptions Interactions of Volcanoes with Other Geosystems Volcanism and the Hydrosphere Volcanism and the Atmosphere The Global Pattern of Volcanism Volcanism at Spreading Centers Volcanism in Subduction Zones Intraplate Volcanism: The Mantle Plume Hypothesis 2018 Eruption of Kilauea Volcano, Hawaii Volcanism and Human Affairs Volcanic Hazards Reducing the Risks of Volcanic Hazards Natural Resources from Volcanoes Chapter 6 Sedimentation: Rocks Formed by Surface Processes Surface Processes of the Rock Cycle Weathering and Erosion: The Source of Sediments Transportation and Deposition: The Downhill Journey to Sedimentary Basins Oceans as Chemical Mixing Vats Sedimentary Basins:The Sinks for Sediments Rift Basins and Thermal Subsidence Basins Flexural Basins Sedimentary Environments Continental Sedimentary Environments Shoreline Sedimentary Environments Marine Sedimentary Environments Siliciclastic versus Chemical and Biological Sedimentary Environments Sedimentary Structures Cross-Bedding Graded Bedding Ripples Bioturbation Structures Bedding Sequences Burial and Diagenesis: From Sediment to Rock Burial Diagenesis Classification of SiliciclasticSediments and Sedimentary Rocks Coarse-Grained Siliciclastics: Gravel and Conglomerate Medium-Grained Siliciclastics: Sand and Sandstone Fine-Grained Siliciclastics Classification of Chemical and Biological Sediments and Sedimentary Rocks Carbonate Sediments and Rocks Evaporite Sediments and Rocks: Products of Evaporation Other Biological and Chemical Sediments Chapter 7 Metamorphism: Alteration of Rocks by Temperature and Pressure Causes of Metamorphism The Role of Temperature The Role of Pressure The Role of Fluids Types of Metamorphism Regional Metamorphism Contact Metamorphism Seafloor Metamorphism Other Types of Metamorphism MetamorphicTextures Foliation and Cleavage Foliated Rocks Granoblastic Rocks Porphyroblasts Regional Metamorphism and Metamorphic Grade Mineral Isograds: Mapping Zones of Change Metamorphic Grade and Parent Rock Composition Metamorphic Fades PlateTectonics and Metamorphism Metamorphic Pressure-Temperature Paths Ocean-Continent Convergence Continent-Continent Collision Exhumation: A Link Between the Plate Tectonic and Climate Systems Chapter 8 Deformation: Modification of Rocks by Folding and Fracturing PlateTectonic Forces Mapping Geologic Structure Measuring Strike and Dip Geologic Maps Geologic Cross Sections How Rocks Deform Brittle and Ductile Behavior of Rocks in the Laboratory Brittle and Ductile Behavior of Rocks in Earth's Crust Basic Deformation Structures Faults Folds Circular Structures Joints Deformation Textures Styles of Continental Deformation Tensional Tectonics Compressive Tectonics Shearing Tectonics Unraveling Geologic History Chapter 9 Clocks in Rocks: liming the Geologic Record Reconstructing Geologic History From the Stratigraphic Record Principles of Stratigraphy Fossils as Recorders of Geologic Time Unconformities: Gaps in the Geologic Record Cross-Cutting Relationships The Geologic Time Scale: Relative Ages Intervals of Geologic Time Interval Boundaries Mark Mass Extinctions Ages of Petroleum Source Rocks Measuring Absolute Time with Isotopic Clocks Discovery of Radioactivity Radioactive Isotopes: The Clocks in Rocks Isotopic Dating Methods The Geologic Time Scale: Absolute Ages Eons: The Longest Intervals of Geologic Time Perspectives on Geologic Time Recent Advances in Timing the Earth System Sequence Stratigraphy ,Chemical Stratigraphy Paleomagnetic Stratigraphy Clocking the Climate System Chapter 10 Earthquakes What Is an Earthquake? The Elastic Rebound Theory Fault Rupture During Earthquakes Foreshocks and Aftershocks How Do We Study Earthquakes? Seismographs Seismic Waves Locating the Focus Measuring the Size of an Earthquake Determining Fault Mechanisms GPS Measurements and "Silent" Earthquakes Earthquakes and Patterns of Faulting The Big Picture: Earthquakes and Plate Tectonics Regional Fault Systems Earthquake Hazards and Risks How Earthquakes Cause Damage Reducing Earthquake Risk Can Earthquakes Be Predicted? Long-Term Forecasting Short-Term Prediction Medium-Term Forecasting Chapter 11 Exploring Earth's Interior Exploring Earth's Interior with Seismic Waves Basic Types of Waves Paths of Seismic Waves Through Earth Seismic Exploration of Near-Surface Layering Layering and Composition of Earth's Interior The Crust The Mantle The Core-Mantle Boundary The Core Earth's Internal Temperature Heat Flow Through Earth's Interior Temperatures Inside Earth Visualizing Earth'sThree-Dimensional Structure Seismic Tomography Earth's Gravitational Field Earth's Magnetic Field and the Geodynamo The Dipole Field Complexity of the Magnetic Field Paleomagnetism The Magnetic Field and the Biosphere Chapter 12 The Climate System What Is Climate? Components of the Climate
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 5
    Monograph available for loan
    Monograph available for loan
    Berlin Heidelberg : Springer Spektrum
    Call number: 9/M 18.91614
    Description / Table of Contents: Teil I Moderne Theorien und Methoden der Geologie -- 1 System Erde -- 2 Plattentektonik - die alles erklärende Theorie -- Teil II Grundlegende Prozesse -- 3 Die Baustoffe der Erde: Minerale und Gesteine -- 4 Magmatische Gesteine: Gesteine aus Schmelzen -- 5 Sedimente und Sedimentgesteine -- 6 Metamorphe Gesteine -- 7 Störungen, Falten und andere Zeugen der Gesteinsdeformation -- Teil III Der Faktor Zeit -- 8 Zeitmessung im System Erde -- 9 Die Entwicklung der terrestrischen Planeten -- 10 Die Entwicklung der Kontinente -- 11 Geobiologie.-Teil IV Endogene Geosysteme -- 12 Vulkanismus -- 13 Erdbeben -- 14 Die Erforschung des Erdinneren -- Teil V Exogene Geosysteme -- 15 System Klima -- 16 Verwitterung, Erosion und Massenbewegungen -- 17 Der Kreislauf des Wassers und das Grundwasser -- 18 Der Transport zum Ozean -- 19 Wind und Wüsten -- 20 Das Meer -- 21 Gletscher: Die Tätigkeit des Eises -- 22 Landschaftsentwicklung -- Teil VI Geowissenschaften und Gesellschaft -- 23 Mensch und Umwelt -- 24 Übungsaufgaben aus der geologischen Praxis -- Glossar
    Description / Table of Contents: Dieses bewährte Lehrbuch erläutert die grundlegenden Prozesse durch leicht verständliche Texte. Bestechende Fotos führen die Studenten gleichsam an den Ort des Geschehens. Didaktisch hervorragende Zeichnungen verdeutlichen die geologischen Vorgänge in Gegenwart und Vergangenheit. Vulkanismus an Plattengrenzen, Sedimentation in Flussdeltas oder Dünenbildung in Sandwüsten sind damit nur einige Beispiele der vielfältigen Vorgänge, die unsere Erde gestaltet haben und noch immer gestalten. In vielen Fällen können wir sie auch unmittelbar beobachten und mit diesem Lehrbuch verstehen. Auf diese Weise wird der geologische Prüfungsstoff in diesem Lehrbuch zu einer weltweiten Exkursion. Die Neuauflage wurde an vielen Stellen ergänzt und aktualisiert. Dies gilt vor allem für die Kapitel Geobiologie, Klimasystem sowie Mensch und Umwelt, die wegen ihrer Bedeutung für den zu erwartenden Klimawandel wesentlich erweitert wurden. Die Visualisierung von Sachverhalten ist noch erheblich verbessert worden. Ein umfangreiches Glossar mit deutschen und englischen Begriffen ergänzt dieses bewährte Lehrbuch. Stimmen zum Buch: 〉〉Die Autoren haben das Kunststück fertig gebracht, die trockenen Fakten so bunt zu präsentieren, dass das Studium unserer Erde zum Abenteuer wird.Auf den ersten Blick überzeugt zunächst das ansprechende Layout. Das Buch ist durchgängig farbig gestaltet und enthält eine Vielzahl von exzellenten Fotos und didaktisch sehr gut aufbereiteten Zeichnungen. (..) Mehr als bisher sind in der Neuauflage die Systeme der Erde grundlegendes Thema des Buches. In etlichen Exkursen werden diese genauer durchleuchtet. Andere Exkurse widmen sich wirtschaftlichen und politischen Themen, wobei deutlich wird, welche Bedeutung die Geologie für die Zukunft der Menschheit hat. Das beste Lehrbuch der Allgemeinen Geologie, umfassend, aktuell, leicht verständlich. Sehr verständlich und anschaulich, ohne dabei den wissenschaftlichen Anspruch aufzugeben. Unbedingt empfehlenswert. Ein ganz hervorragend aufgebautes Lehrbuch für alle Studierende der Geologie, Geowissenschaften sowie angrenzender Disziplinen wie z.B. Bodenkunde oder Hydrologie. Aufgrund des klaren Aufbaus und der verständlichen Erläuterungen mit Hilfe von ansprechenden Bildern und Grafiken, aber auch für geologisch interessierte Laien wärmstens zu empfehlen.Ein "Klassiker" der Geologie und als umfassende Einführung sehr gut geeignet. 〈〈 Prof. Dr. Alexander Siegmund, Pädagogische Hochschule He ...
    Type of Medium: Monograph available for loan
    Pages: XXX, 769 Seiten , 578 Illustrationen
    Edition: 7. Auflage
    ISBN: 978-3-662-48341-1
    Classification:
    Geology
    Language: German
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  • 6
    Electronic Resource
    Electronic Resource
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Earth and Planetary Sciences 27 (1999), S. 313-358 
    ISSN: 0084-6597
    Source: Annual Reviews Electronic Back Volume Collection 1932-2001ff
    Topics: Geosciences , Physics
    Notes: Abstract Stromatolites are attached, lithified sedimentary growth structures, accretionary away from a point or limited surface of initiation. Though the accretion process is commonly regarded to result from the sediment trapping or precipitation-inducing activities of microbial mats, little evidence of this process is preserved in most Precambrian stromatolites. The successful study and interpretation of stromatolites requires a process-based approach, oriented toward deconvolving the replacement textures of ancient stromatolites. The effects of diagenetic recrystallization first must be accounted for, followed by analysis of lamination textures and deduction of possible accretion mechanisms. Accretion hypotheses can be tested using numerical simulations based on modern stromatolite growth processes. Application of this approach has shown that stromatolites were originally formed largely through in situ precipitation of laminae during Archean and older Proterozoic times, but that younger Proterozoic stromatolites grew largely through the accretion of carbonate sediments, most likely through the physical process of microbial trapping and binding. This trend most likely reflects long-term evolution of the earth's environment rather than microbial communities.
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Microbialites are organosedimentary structures that can be constructed by a variety of metabolically distinct taxa. Consequently, microbialite structures abound in the fossil record, although the exact nature of the biogeochemical processes that produced them is often unknown. One such ...
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  • 8
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: A major palaeokarst erosion surface is developed within the middle Proterozoic Elu Basin, northwestern Canada. This palaeokarst is named the sub-Kanuyak unconformity and truncates the Parry Bay Formation, a sequence of shallow-marine dolostones that were deposited within a north-facing carbonate platform under a semi-arid climate.The sub-Kanuyak unconformity exhibits up to 90 m of local relief, and also formed under semi-arid conditions when Parry Bay dolostones were subaerially exposed during a relative sea-level drop of about 180 m. Caves and various karren developed within the meteoric vadose and phreatic zones. Their geometry, size and orientation were largely controlled by northwest- and northeast-trending antecedent joints, bedding, and lithology. Near-surface caves later collapsed forming valleys, and intervening towers or walls, and plains. Minor terra rossa formed on top of highs. Karstification was most pronounced in southern parts of Bathurst Inlet but decreased northward, probably reflecting varying lengths of exposure time along a north-dipping slope.The Kanuyak Formation is up to 65 m thick, and partially covers the underlying palaeokarst. It consists of six lithofacies: (i) breccia formed during collapse of caves, as reworked collapse breccia and regolith; (ii) conglomerate representing gravel-dominated braided-fluvial deposits; (iii) sandstone deposited as braided-fluvial and storm-dominated lacustrine deposits; (iv) interbedded sandstone, siltstone and mudstone of sheet flood origin; (v) dolostones formed from dolocretes and quiet-water lacustrine deposits; and (vi) red-beds representing intertidal-marine mudflat deposits. Rivers flowed toward the northwest and northeast within karst valleys and caves; lakes were also situated within valleys; marine mudflat sediments completely cover the palaeokarst to the north.A regional correlation of the sub-Kanuyak unconformity with the intra-Greenhorn Lakes disconformity within the Coppermine homocline suggests that similar styles of karstification occurred over an extensive region. The Elu Basin palaeokarst, however, was developed more landward, and was exposed for a longer period of time than the Coppermine homocline palaeokarst.
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  • 9
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Ltd
    Sedimentology 51 (2004), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The precipitation of calcite and aragonite as encrustations directly on the seafloor was an important platform-building process during deposition of the 2560–2520 Ma Campbellrand-Malmani carbonate platform, South Africa. Aragonite fans and fibrous coatings are common in unrestricted, shallow subtidal to intertidal facies. They are also present in restricted facies, but are absent from deep subtidal facies. Decimetre-thick fibrous calcite encrustations are present to abundant in all depositional environments except the deepest slope and basinal facies. The proportion of the rock composed of carbonate that precipitated as encrustations or in primary voids ranges from 0% to 〉 65% depending on the facies. Subtidal facies commonly contain 20–35%in situ precipitated carbonate, demonstrating that Neoarchaean sea water was supersaturated with respect to aragonite, carbonate crystal growth rates were rapid compared with sediment influx rates, and the dynamics of carbonate precipitation were different from those in younger carbonate platforms. The abundance of aragonite pseudomorphs suggests that sea-water pH was neutral to alkaline, whereas the paucity of micrite suggests the presence of inhibitors to calcite and aragonite nucleation in the mixed zone of the oceans.
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  • 10
    ISSN: 1365-3121
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The Late Neoproterozoic Buah Formation (Nafun Group, Oman) is a carbonate unit outcropping in the Jabal Akhdar and Huqf areas. It is composed mostly of shallow-water carbonates deposited on a distally steepened carbonate ramp. Correlation of two δ13C isotope shifts shows that in the Jabal Akhdar ramp differentiation into fast and slow subsiding areas was followed by lateral progradation. In the Huqf area, however, a uniform scenario of upward shallowing of the facies and lateral progradation is demonstrated by chemostratigraphic timelines cross-cutting the facies belts. The chemostratigraphic profiles show that the Buah Formation was deposited during sea-level highstand conditions and that ramp differentiation was due to synsedimentary tectonics. High-resolution correlation of δ13C profiles from the same lithostratigraphic unit (whether Precambrian or Phanerozoic in age) lacking biostratigraphic data can shed light on carbonate systems dynamics, tectonic vs. eustatic controls on depositional sequences and basin subsidence.
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