The geology of stratigraphic sequences /

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Detalles Bibliográficos
Autor principal: Miall, Andrew D.
Formato: Desconocido
Lenguaje:Español
Publicado: New York : Springer, 2010.
Edición:2nd ed.
Materias:
Aporte de:Registro referencial: Solicitar el recurso aquí
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100 1 |a Miall, Andrew D.  |9 15294 
245 1 4 |a The geology of stratigraphic sequences /   |c Andrew D. Miall 
250 |a 2nd ed. 
260 |a New York :   |b Springer,   |c 2010. 
300 |a 522 p. :   |b il., grafs. ;   |c 27cm. 
500 |a Incluye índice analítico 
505 |a Part 1. The Emergence of Modern Concepts. 1. Historical and Methodological Background -- 1.1. Introduction -- 1.2. Methods in Geology -- 1.2.1. The Significance of Sequence Stratigraphy -- 1.2.2. Data and Argument in Geology -- 1.2.3. The Hermeneutic Circle and the Emergence of Sequence Stratigraphy -- 1.2.4. Paradigms and Exemplars -- 1.3. The Development of Descriptive Stratigraphy -- 1.3.1. The Growth of Modern Concepts -- 1.3.2. Do Stratigraphic Units Have “Time” Significance? -- 1.3.3. The Development of Modern Chronostratigraphy -- 1.4. The Continual Search for a “Pulse of the Earth” -- 1.5. Problems and Research Trends: The Current Status -- 1.6. Current Literature -- 1.7. Stratigraphic Terminology -- 2. The Basic Sequence Model. 2.1. Introduction -- 2.2. Elements of the Model -- 2.2.1. Accommodation and Supply -- 2.2.2. Stratigraphic Architecture -- 2.2.3. Depositional Systems and Systems Tracts -- 2.3. Sequence Models in Clastic and Carbonate Settings -- 2.3.1. Marine Clastic Depositional Systems and Systems Tracts -- 2.3.2. Nonmarine Depositional Systems -- 2.3.3. Carbonate Depositional Systems -- 2.4. Sequence Definitions -- 3. Other Methods for the Stratigraphic Analysis of Cycles of Base-Level Change. 3.1. Introduction -- 3.2. Facies Cycles -- 3.3. Areas and Volumes of Stratigraphic Units -- 3.4. Hypsometric Curves -- x Contents -- 3.5. Backstripping -- 3.6. Sea-Level Estimation from Paleoshorelines and Other Fixed Points -- 3.7. Documentation of Metre-Scale Cycles -- 3.8. Integrated Tectonic-Stratigraphic Analysis -- Part 2. The Stratigraphic Framework. 4. The Major Types of Stratigraphic Cycle. 4.1. Introduction -- 4.2. Sequence Hierarchy -- 4.3. The Supercontinent Cycle -- 4.4. Cycles with Episodicities of Tens of Millions of Years -- 4.5. Cycles with Million-Year Episodicities -- 4.6. Cycles with Episodicities of Less Than One Million Years -- 5. Cycles with Episodicities of Tens to Hundreds of Millions of Years. 5.1. Climate, Sedimentation and Biogenesis -- 5.2. The Supercontinent Cycle -- 5.2.1. The Tectonic-Stratigraphic Model -- 5.2.2. The Phanerozoic Record -- 5.3. Cycles with Episodicities of Tens of Millions of years -- 5.3.1. Regional to Intercontinental Correlations -- 5.3.2. Tectonostratigraphic Sequences -- 5.4. Main Conclusions -- 6. Cycles with Million-Year Episodicities. 6.1. Continental Margins -- 6.1.1. Clastic Platforms and Margins -- 6.1.2. Carbonate Cycles of Platforms and Craton Margins -- 6.1.3. Mixed Carbonate-Clastic Successions -- 6.2. Foreland Basins -- 6.2.1. Foreland Basin of the North American Western Interior -- 6.2.2. Other Foreland Basins -- 6.3. Arc-Related Basins -- 6.3.1. Forearc Basins -- 6.3.2. Backarc Basins -- 6.4. Cyclothems and Mesothems -- 6.5. Conclusions -- 7. Cycles with Episodicities of Less than One Million Years. 7.1. Introduction -- 7.2. Neogene Clastic Cycles of Continental Margins -- 7.2.1. The Gulf Coast Basin of the United States -- 7.2.2. Wanganui Basin, North Island, New Zealand -- 7.2.3. Other Examples of Neogene High-Frequency Cycles -- 7.2.4. The Deep-Marine Record -- 7.3. Pre-neogene Marine Carbonate and Clastic Cycles -- 7.4. Late Paleozoic Cyclothems -- 7.5. Lacustrine Clastic and Chemical Rhythms -- 7.6. High-Frequency Cycles in Foreland Basins -- 7.7. Main Conclusions -- Part 3. Mechanisms. 8. Summary of Sequence-Generating Mechanisms. 9. Long-Term Eustasy and Epeirogeny. 9.1. Mantle Processes and Dynamic Topography -- 9.2. Supercontinent Cycles -- 9.3. Cycles with Episodicities of Tens of Millions of Years -- 9.3.1. Eustasy -- 9.3.2. Dynamic Topography and Epeirogeny -- 9.3.3. The Origin of Sloss Sequences -- 9.4. Main Conclusions -- 10. Tectonic Mechanisms. 10.1. Introduction -- 10.2. Rifting and Thermal Evolution of Divergent Plate Margins -- 10.2.1. Basic Geophysical Models and Their Implications for Sea-Level Change -- 10.2.2. The Origins of Some Tectonostratigraphic Sequences -- 10.3. Tectonism on Convergent Plate Margins and in Collision Zones -- 10.3.1. Magmatic Arcs and Subduction -- 10.3.2. Rates of Uplift and Subsidence on Convergent Margins -- 10.3.3. Tectonism Versus Eustasy in Foreland Basins -- 10.4. Intraplate Stress -- 10.4.1. The Pattern of Global Stress -- 10.4.2. In-Plane Stress as a Control of Sequence Architecture -- 10.4.3. In-Plane Stress and Regional Histories of Sea-Level Change -- 10.5. Basement Control -- 10.6. Sediment Supply and the Importance of Big Rivers -- 10.7. Environmental Change -- 10.8. Main Conclusions -- 11. Orbital Forcing. 11.1. Introduction -- 11.2. The Nature of Milankovitch Processes -- 11.2.1. Components of Orbital Forcing -- 11.2.2. Basic Climatology -- 11.2.3. Variations with Time in Orbital Periodicities -- 11.2.4. Isostasy and Geoid Changes -- 11.2.5. Nonglacial Milankovitch Cyclicity -- 11.2.6. The Nature of the Cyclostratigraphic Data Base -- 11.3. The Geologic Record -- 11.3.1. The Sensitivity of the Earth to Glaciation -- 11.3.2. The Cenozoic Record -- 11.3.3. Glacioeustasy in the Mesozoic? -- 11.3.4. Late Paleozoic Cyclothem -- 11.4. Distinguishing Between Orbital Forcing and Tectonic Driving Mechanisms -- 11.5. Main Conclusions -- Part 4. Chronostratigraphy and Correlation: An Assessment of the Current Status of “Global Eustasy”. 12. The Concept of the Global Cycle Chart. 12.1. From Vail to Haq -- 12.2. The Two-Paradigm Problem -- 12.2.1. The Global-Eustasy Paradigm -- 12.2.2. The Complexity Paradigm -- 12.3. Defining and Deconstructing Global Eustasy and Complexity Texts -- 12.4. Invisible Colleges and the Advancement of Knowledge -- 12.5. The Global-Eustasy Paradigm — A Revolution in Trouble? -- 13. Time in Sequence Stratigraphy. 13.1. Introduction -- 13.2. Hierarchies of Time and the Completeness of the Stratigraphic Record -- 13.3. Main Conclusions -- 14. Chronostratigraphy, Correlation, and Modern Tests for Global Eustasy. 14.1. Introduction -- 14.2. Chronostratigraphic Models and the Testing of Correlations -- 14.3. Chronostratigraphic Meaning of Unconformities -- 14.4. A Correlation Experiment -- 14.5. Testing for Eustasy: The Way Forward -- 14.5.1 Introduction -- 14.5.2. The Dating and Correlation of Stratigraphic Events: Potential Sources of Uncertainty -- 14.5.3. The Value of Quantitative Biostratigraphic Methods -- 14.5.4. Assessment of Relative Biostratigraphic Precision -- 14.5.5. Correlation of Biozones with the Global Stage Framework -- 14.5.6. Assignment of Absolute Ages and the Importance of the Modern Time Scale -- 14.6. Modern Tests of the Global-Eustasy Paradigm -- 14.6.1. Cretaceous-Paleogene Sequence Stratigraphy of New Jersey -- 14.6.2. Other Modern High-Resolution Studies of Cretaceous-Paleogene Sequence Stratigraphy -- 14.6.3. Sequence Stratigraphy of the Neogene -- 14.6.4. The Growing Evidence for Glacioeustasy in the Mesozoic and Early Cenozoic -- 14.7. Cyclostratigraphy and Astrochronology -- 14.7.1. Historical Background of Cyclostratigraphy -- 14.7.2. The Building of a Time Scale -- 14.8. Testing Correlations with Carbon Isotope Chemostratigraphy -- 14.9. Main Conclusions -- 15. Future Directions. 15.1. Research Methods -- 15.2. Remaining Questions -- 15.2.1. Future Advances in Cyclostratigraphy? -- 15.2.2. Tectonic Mechanisms of Sequence Generation -- 15.2.3. Orbital Forcing -- 15.2.4. The Codification of Sequence Nomenclature. 
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