The Geology of Stratigraphic Sequences
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1 The Geology of Stratigraphic Sequences Bearbeitet von Andrew Miall 2nd ed Buch. xvii, 522 S. Hardcover ISBN Format (B x L): 19,5 x 26 cm Gewicht: 1337 g Weitere Fachgebiete > Geologie, Geographie, Klima, Umwelt > Geologie > Stratigraphie schnell und portofrei erhältlich bei Die Online-Fachbuchhandlung beck-shop.de ist spezialisiert auf Fachbücher, insbesondere Recht, Steuern und Wirtschaft. Im Sortiment finden Sie alle Medien (Bücher, Zeitschriften, CDs, ebooks, etc.) aller Verlage. Ergänzt wird das Programm durch Services wie Neuerscheinungsdienst oder Zusammenstellungen von Büchern zu Sonderpreisen. Der Shop führt mehr als 8 Millionen Produkte.
2 Contents Part I The Emergence of Modern Concepts Historical and Methodological Background Introduction Methods in Geology The Significance of Sequence Stratigraphy DataandArgumentinGeology The Hermeneutic Circle and the Emergence of Sequence Stratigraphy ParadigmsandExemplars TheDevelopmentofDescriptiveStratigraphy The Growth of Modern Concepts Do Stratigraphic Units Have Time Significance? The Development of Modern Chronostratigraphy The Continual Search for a Pulse of the Earth Problems and Research Trends: The Current Status CurrentLiterature Stratigraphic Terminology The Basic Sequence Model Introduction Elements of the Model Accommodation and Supply Stratigraphic Architecture Depositional Systems and Systems Tracts Sequence Models in Clastic and Carbonate Settings Marine Clastic Depositional Systems and Systems Tracts Nonmarine Depositional Systems Carbonate Depositional Systems Sequence Definitions Other Methods for the Stratigraphic Analysis of Cycles of Base-Level Change Introduction FaciesCycles Areas and Volumes of Stratigraphic Units HypsometricCurves ix
3 x Contents 3.5 Backstripping Sea-Level Estimation from Paleoshorelines and Other FixedPoints Documentation of Metre-Scale Cycles Integrated Tectonic-Stratigraphic Analysis Part II The Stratigraphic Framework The Major Types of Stratigraphic Cycle Introduction Sequence Hierarchy The Supercontinent Cycle Cycles with Episodicities of Tens of Millions of Years Cycles with Million-Year Episodicities Cycles with Episodicities of Less Than One Million Years Cycles with Episodicities of Tens to Hundreds of Millions of Years Climate, Sedimentation and Biogenesis The Supercontinent Cycle The Tectonic-Stratigraphic Model The Phanerozoic Record Cycles with Episodicities of Tens of Millions of years Regional to Intercontinental Correlations Tectonostratigraphic Sequences Main Conclusions Cycles with Million-Year Episodicities Continental Margins ClasticPlatformsandMargins Carbonate Cycles of Platforms and Craton Margins Mixed Carbonate-Clastic Successions ForelandBasins ForelandBasinoftheNorthAmericanWesternInterior OtherForelandBasins Arc-RelatedBasins ForearcBasins Backarc Basins CyclothemsandMesothems Conclusions Cycles with Episodicities of Less than One Million Years Introduction Neogene Clastic Cycles of Continental Margins TheGulfCoastBasinoftheUnitedStates Wanganui Basin, North Island, New Zealand Other Examples of Neogene High-Frequency Cycles The Deep-Marine Record Pre-neogene Marine Carbonate and Clastic Cycles Late Paleozoic Cyclothems
4 Contents xi 7.5 Lacustrine Clastic and Chemical Rhythms High-Frequency Cycles in Foreland Basins Main Conclusions Part III Mechanisms Summary of Sequence-Generating Mechanisms Long-Term Eustasy and Epeirogeny Mantle Processes and Dynamic Topography Supercontinent Cycles Cycles with Episodicities of Tens of Millions of Years Eustasy Dynamic Topography and Epeirogeny The Origin of Sloss Sequences Main Conclusions Tectonic Mechanisms Introduction Rifting and Thermal Evolution of Divergent Plate Margins Basic Geophysical Models and Their Implications for Sea-Level Change The Origins of Some Tectonostratigraphic Sequences Tectonism on Convergent Plate Margins and in Collision Zones Magmatic Arcs and Subduction Rates of Uplift and Subsidence on Convergent Margins TectonismVersusEustasyinForelandBasins IntraplateStress The Pattern of Global Stress In-Plane Stress as a Control of Sequence Architecture In-Plane Stress and Regional Histories of Sea-Level Change BasementControl Sediment Supply and the Importance of Big Rivers Environmental Change Main Conclusions Orbital Forcing Introduction TheNatureofMilankovitchProcesses Components of Orbital Forcing BasicClimatology Variations with Time in Orbital Periodicities Isostasy and Geoid Changes Nonglacial Milankovitch Cyclicity The Nature of the Cyclostratigraphic Data Base The Geologic Record The Sensitivity of the Earth to Glaciation The Cenozoic Record Glacioeustasy in the Mesozoic? Late Paleozoic Cyclothems
5 xii Contents 11.4 Distinguishing Between Orbital Forcing and Tectonic Driving Mechanisms Main Conclusions Part IV Chronostratigraphy and Correlation: An Assessment of the Current Status of Global Eustasy The Concept of the Global Cycle Chart FromVailtoHaq TheTwo-ParadigmProblem The Global-Eustasy Paradigm TheComplexityParadigm Defining and Deconstructing Global Eustasy and ComplexityTexts Invisible Colleges and the Advancement of Knowledge The Global-Eustasy Paradigm A Revolution in Trouble? Conclusions Time in Sequence Stratigraphy Introduction Hierarchies of Time and the Completeness of the Stratigraphic Record Main Conclusions Chronostratigraphy, Correlation, and Modern Tests for Global Eustasy Introduction Chronostratigraphic Models andthetestingofcorrelations Chronostratigraphic Meaning of Unconformities A Correlation Experiment TestingforEustasy:TheWayForward Introduction The Dating and Correlation of Stratigraphic Events: Potential Sources of Uncertainty The Value of Quantitative Biostratigraphic Methods Assessment of Relative Biostratigraphic Precision Correlation of Biozones with the Global Stage Framework Assignment of Absolute Ages and the Importance of the Modern Time Scale Modern Tests of the Global-Eustasy Paradigm Cretaceous-Paleogene Sequence Stratigraphy of New Jersey Other Modern High-Resolution Studies of Cretaceous-Paleogene Sequence Stratigraphy Sequence Stratigraphy of the Neogene The Growing Evidence for Glacioeustasy in the Mesozoic and Early Cenozoic Cyclostratigraphy and Astrochronology Historical Background of Cyclostratigraphy The Building of a Time Scale
6 Contents xiii 14.8 Testing Correlations with Carbon Isotope Chemostratigraphy Main Conclusions Future Directions Research Methods RemainingQuestions Future Advances in Cyclostratigraphy? Tectonic Mechanisms of Sequence Generation OrbitalForcing The Codification of Sequence Nomenclature References Author Index Subject Index
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