1. Ductile Instabilities and Structural Heterogeneity in the Lower Crust.- 1.1. Introduction.- 1.2. Geological Example: Mt. Hay Region, Arunta Block, Central Australia.- 1.3. Structural Heterogeneity and Competency Contrast.- 1.4. Mechanical Instabilities: The Link Between Competency Contrast, Patterns of Deformation, and Heterogeneity.- 1.5. High Strain and the Destruction of the Structures that Record Mechanical Instabilities.- 1.6. Interpretation of Complexly Deformed Rocks: Mt. Hay Region, Australia.- 1.7. Summary.- 1.8. Appendix.- 1.9. References.- 2. Petrological Causes of Seismic Heterogeneity in the Continental Crust.- 2.1. Introduction.- 2.2. Crustal Composition and Compositional Evolution.- 2.3. Rock Properties.- 2.4. Seismic Heterogeneity of Igneous Rocks.- 2.5. Seismic Heterogeneities of Metamorphic Rocks.- 2.6. Anisotropy.- 2.7. Results from Boreholes.- 2.8. Reflectivity.- 2.9. Conclusions.- 2.10. References.- 3. Seismic Modeling of Lower and Mid-Crustal Structure as Exemplified by the Massiccio dei Laghi (Ivrea-Verbano Zone and Serie dei Laghi) Crustal Section, Northwestern Italy.- 3.1. Introduction.- 3.2. Summary of the Regional Geology.- 3.3. Deterministic Forward Seismic Modeling.- 3.4. Discussion.- 3.5. Conclusions.- 3.6. References.- 4. Comparison of Geologic and Seismic Structure of the Uppermost Fast-Spreading Oceanic Crust: Insights From a Crustal Cross-Section at the Hess Deep Rift.- 4.1. Introduction.- 4.2. Tectonic Window at the Hess Deep Rift.- 4.3. Geology of the Uppermost Oceanic Crust at Hess Deep.- 4.4. Interpretation of Upper Crustal Geology and Implications for Processes at the EPR.- 4.5. Physical Properties of Upper Crustal Rock Units.- 4.6. Correlation of Geologic Units and Seismic Layers.- 4.7. Conclusions.- 4.8. References.- 5. A Generic Model for the 1/f-Nature of Seismic Velocity Fluctuations.- 5.1. Introduction.- 5.2. Stochastic Nature of Fault-Induced Seismic Velocity Fluctuations.- 5.3. Generalized Model for 1/f-Scaling of Seismic Velocity Fluctuations.- 5.4. Hyperbolic Scaling in Space.- 5.5. Empirical Evidence: Joint Interpretation of the KTB Lithology and Sonic Logs.- 5.6. Conclusions.- 5.7. References.- 6. Fractures and Physical Heterogeneity in Crustal Rock.- 6.1. Introduction.- 6.2. Power Law Scaling in Crustal Fracture Systems.- 6.3. Physical Analogues for Power-Law Scaling in Crustal Rock.- 6.4. Modeling Power-Law Scaling Crustal Fracture Systems.- 6.5. Discussion: Reservoir Modeling.- 6.6. Conclusions.- 6.7. References.- 7. Statistical Characterization of Spatial Variability in Sedimentary Rock.- 7.1. Introduction.- 7.2. Reproducible Statistical Features of Sedimentary Rock.- 7.3. Statistical Models for Spatial Variability.- 7.4. Comparison with Data.- 7.5. Summary and Conclusions.- 7.6. References.- 8. Multifractal Modeling and Analyses of Crustal Heterogeneity.- 8.1. Introduction.- 8.2. Construction and Properties of Multifractals.- 8.3. Multifractal Analyses of Borehole Logs and Fracture Patterns.- 8.4. Conclusions.- 8.5. Appendix.- 8.6. References.- 9. Seismic Imaging of Lower Crustal Heterogeneity.- 9.1. Introduction.- 9.2. Effects of Acquisition.- 9.3. Effects of Processing.- 9.4. Effects of the Transmission Path.- 9.5. Discussion.- 9.6. Conclusions.- 9.7. References.- 10. The Heterogeneity of the Crust and its Effect on Seismic Wide-Angle Reflection Fields.- 10.1. Introduction.- 10.2. The Evolution of our Perception of the Structure of the Earth’s Crust.- 10.3. Seismic Wide-Angle Reflection Record Sections.- 10.4. Discussion.- 10.5. Conclusions.- 10.6. References.- 11. Heterogeneities of the Uppermost Mantle Inferred From Controlled-Source Seismology.- 11.1. Introduction.- 11.2. Studies of Lithospheric Scattering.- 11.3.Pn/SnWave Propagation.- 11.4. Modeling the Long-RangePn.- 11.5. Discussion and Conclusions.- 11.6. References.- 12. The Nature of Crustal Seismic Heterogeneity: A Case Study From the Grenville Province.- 12.1. Introduction.- 12.2. Geologic Heterogeneit...
Die Inhaltsangabe kann sich auf eine andere Ausgabe dieses Titels beziehen.
"Primarily aimed at the researcher, this book provides an excellent introductory overview to the subject, which should be read by any Earth Scientist wishing to gain an insight into the characterisation and imaging of crustal and upper mantle heterogeneity. It should be an essential part of any reference collection." (Richard England, University of Leicester, UK in The Eggs, #6, December 2003) "In summary, this well-written volume provides a glimpse into the highly specialized but critically important field of studying small-scale heterogeneity in structures an dprocesses related to deformation, igneous intrusion, and sedimentation. The presentation of material achieves an excellent balance between a theoretical and an observational approach so that any reader will be able to gain entry into this burgeoning field." (John H. McBride, Brigham Young University, USA in Eos, 85: 15, April 2004)
Most of our knowledge about the physical structure and the chemical composition of the Earth's deep interior is inferred from seismic data. The interpretation of seismic waves generally follows the assumption that the Earth's physical structure is grossly layered and that fluctuations of the physical parameters within individual layers are smooth in structure and small in magnitude. While this view greatly facilitates the analytic and interpretative procedure, it is clearly at odds with evidence from outcrops and boreholes, which indicates that compositional, structural and petrophysical heterogeneity in the Earth prevails over a wide range of scales. This book is the first to unify three different views of crustal and upper mantle heterogeneity. It brings together the geological view, which is derived from the analysis of crustal exposures and deep boreholes; the stochastic view, which attempts to find order and structure in these seemingly chaotic data; and the seismological view, which considers the end product of the complex interaction of seismic energy with the heterogeneous structure at depth. John Goff and Klaus Holliger have compiled chapters that explore and quantify the relationship between geological and petrophysical heterogeneity and its seismic response, and use seismic data to probe the fabric of the Earth's interior. Geologists, geostaticians, and geophysicists alike will benefit from the integrative perspective presented in Heterogeneity in the Crust and Upper Mantle: Nature, Scaling, and Seismic Properties, making this text an unparalleled reference for professionals and students in Earth science fields.
„Über diesen Titel“ kann sich auf eine andere Ausgabe dieses Titels beziehen.
Anbieter: Romtrade Corp., STERLING HEIGHTS, MI, USA
Zustand: New. This is a Brand-new US Edition. This Item may be shipped from US or any other country as we have multiple locations worldwide. Artikel-Nr. ABNR-86593
Anbieter: Anybook.com, Lincoln, Vereinigtes Königreich
Zustand: Good. This is an ex-library book and may have the usual library/used-book markings inside.This book has hardback covers. In good all round condition. Please note the Image in this listing is a stock photo and may not match the covers of the actual item,950grams, ISBN:9780306474477. Artikel-Nr. 5585348
Anzahl: 1 verfügbar
Anbieter: Antiquariat Bookfarm, Löbnitz, Deutschland
Hardcover. XIX, 349 S. Ehem. Bibliotheksexemplar mit Signatur und Stempel. GUTER Zustand, ein paar Gebrauchsspuren. Ex-library with stamp and library-signature. GOOD condition, some traces of use. w10666 9780306474477 Sprache: Englisch Gewicht in Gramm: 550. Artikel-Nr. 2432513
Anzahl: 1 verfügbar
Anbieter: Majestic Books, Hounslow, Vereinigtes Königreich
Zustand: Used. pp. xix + 349 Illus., Maps. Artikel-Nr. 5773714
Anzahl: 1 verfügbar
Anbieter: Biblios, Frankfurt am main, HESSE, Deutschland
Zustand: Used. pp. xix + 349. Artikel-Nr. 183122759
Anzahl: 1 verfügbar
Anbieter: AHA-BUCH GmbH, Einbeck, Deutschland
Buch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - Most of our knowledge about the physical structure and the chemical composition of the Earth's deep interior is inferred from seismic data. The interpretation of seismic waves generally follows the assumption that the Earth's physical structure is grossly layered and that fluctuations of the physical parameters within individual layers are smooth in structure and small in magnitude. While this view greatly facilitates the analytic and interpretative procedure, it is clearly at odds with evidence from outcrops and boreholes, which indicates that compositional, structural and petrophysical heterogeneity in the Earth prevails over a wide range of scales. This book is the first to unify three different views of crustal and upper mantle heterogeneity. It brings together the geological view, which is derived from the analysis of crustal exposures and deep boreholes; the stochastic view, which attempts to find order and structure in these seemingly chaotic data; and the seismological view, which considers the end product of the complex interaction of seismic energy with the heterogeneous structure at depth. John Goff and Klaus Holliger have compiled chapters that explore and quantify the relationship between geological and petrophysical heterogeneity and its seismic response, and use seismic data to probe the fabric of the Earth's interior. Geologists, geostaticians, and geophysicists alike will benefit from the integrative perspective presented in Heterogeneity in the Crust and Upper Mantle: Nature, Scaling, and Seismic Properties, making this text an unparalleled reference for professionals and students in Earth science fields. Artikel-Nr. 9780306474477
Anzahl: 1 verfügbar
Anbieter: Revaluation Books, Exeter, Vereinigtes Königreich
Hardcover. Zustand: Brand New. 1st edition. 349 pages. 9.75x6.50x1.00 inches. In Stock. Artikel-Nr. x-0306474476
Anzahl: 2 verfügbar