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  • 1
    Keywords: Sedimentary basins. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (104 pages)
    Edition: 1st ed.
    ISBN: 9781634855754
    Series Statement: Geology and Mineralogy Research Developments
    DDC: 551.44000000000005
    Language: English
    Note: Intro -- Contents -- Preface -- Basin Formation on Convergent Margins -- Abstract -- 1. Introduction -- 2. Tectonic Context of Study Area -- 2.1. Existing Dataset and Basin Configuration -- 2.2. Gravity Anomalies of Osaka District -- Conclusion -- Acknowledgments -- References -- Estimations of Subsurface Structures by Gravity Anomaly and Gravity Gradient Tensor -- Abstract -- 1. Introduction -- 2. Edge Emphasis -- 2.1. Various Edge Emphasis Techniques -- 2.2. Applications and Discussion -- 3. Euler Deconvolution -- 3.1. Basic Theories -- 3.2. Applications and Discussion -- 4. Dip Angle Estimation of Fault or Structural Boundary -- 4.1. Basic Theories -- 4.2. Applications and Discussion -- Conclusion -- Acknowledgments -- References -- Subsurface Structure of Osaka Sedimentary Basin and Its Tectonic Evolution -- Abstract -- 1. Introduction -- 2. Seismic Interpretation -- 2.1. Northern Sector -- 2.2. Southern Sector -- 3. Chronology of Ancient Fluvial Basin -- 3.1. Samples -- 3.2. Methods -- 3.3. Results -- 4. Structural Evolution and Temporal Transition of Tectonic Stress -- Conclusion -- Acknowledgments -- References -- Tectonic Implication of Basin Formation on the Basis of Paleogeography Using Stratigraphy and Shallow Subsurface Structure from a Drilling Data Base -- Abstract -- 1. Introduction -- 2. Tectonic Implication on the Basis of Paleogeography from the Pliocene to Quaternary Sediments in Kinki District -- 3. Tectonic Implications on the Basis of Drilling Data during the Quaternary Period in the Osaka Sedimentary Basin -- 3.1. Marine Clay Distribution and Subsurface Structure: Strike and Dip of Marine Clays No. 12, 10, and 9, and the Trend of the Uemachi Flexure -- 3.2. Paleogeography in the Osaka Sedimentary Basin since MIS 5 and the Tectonic Implications -- Conclusion -- Acknowledgments -- References -- About the Authors -- Index.
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  • 2
    Keywords: Earth sciences ; Earth Sciences ; Structural geology ; Sedimentology ; Geophysics ; Engineering geology ; Engineering Geology ; Foundations ; Hydraulics
    Description / Table of Contents: This publication shows the three-dimensional configuration of the gigantic tectonic sag of the Osaka Bay sedimentary basin on the eastern Eurasian margin based on reflection seismic data never before published. The basin has developed relatively quickly since the dawn of the Quaternary. High-resolution subsurface images on the profiles provide highly valuable information about the architecture of active faults, paleoenvironmental changes, and mass balance on the convergent margin. The book presents an excellent case study of a tectonically controlled basin because morphologies and evolutionary processes of such basins show an enormous diversity, reflecting spatiotemporal variation in tectonic stress. Furthermore, this volume provides insight into the general mechanism of sedimentary basin formation. The quantitative analyses contained here will be thought-provoking for industry experts, academics, and graduate and undergraduate students engaged in geologic survey and civil engineering. The contents will be especially useful to professionals in the fields of Quaternary geology, neotectonics, and active fault research
    Type of Medium: Online Resource
    Pages: Online-Ressource (X, 119 p. 80 illus., 59 illus. in color, online resource)
    ISBN: 9789811305771
    Series Statement: Advances in Geological Science
    Language: English
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  • 3
    Keywords: Sedimentary basins. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (127 pages)
    Edition: 1st ed.
    ISBN: 9789811305771
    Series Statement: Advances in Geological Science Series
    DDC: 552.5
    Language: English
    Note: Intro -- Preface -- Acknowledgements -- Contents -- 1 Tectonic Context of the Study Area -- 1.1 Plate Tectonic Framework of the Eastern Eurasian Margin -- 1.1.1 Chronicle of Plate Motions Since 100 Ma -- 1.1.2 Present-Day Configuration -- 1.2 Tectonic Epochs of Southwest Japan-Previous Studies -- 1.2.1 Paleomagnetism -- 1.2.2 Reflection Seismic Survey -- 1.3 Recent Crustal Movements Revealed by Geodetic Observation -- 1.4 Spatiotemporal Overview of the Osaka Sedimentary Basin -- 1.4.1 Paleogeography -- 1.4.2 Active Faults on Land -- 1.4.3 Geophysical Studies -- References -- 2 Basic Knowledge-Stratigraphy of the Osaka Group -- 2.1 Overview of Sedimentary Basins -- 2.2 Chronology -- 2.2.1 Biostratigraphy -- 2.2.2 Magnetostratigraphy -- 2.2.3 Tephrochronology -- 2.3 Paleoenvironment -- 2.4 Deep Boring Survey -- 2.4.1 Onshore Data -- 2.4.2 Offshore Data -- 2.5 Tectonic Movements Deduced from Burial History -- 2.5.1 Isotope Stage Boundaries -- 2.5.2 Subsurface Datum Levels -- 2.5.3 Differential Subsidence of Northern Osaka Basin -- References -- 3 Reflection Seismic Data -- 3.1 Dataset -- 3.2 Correlation Between Subsurface Datum Planes and Seismic Horizons -- 3.3 Systematic Descriptions -- 3.3.1 Data Acquired by Geological Survey of Japan, AIST -- 3.3.2 Data Acquired by Hydrographic and Oceanographic Department, JCG -- 3.3.3 Data Acquired by Hyogo Prefecture -- 3.3.4 Data Acquired by Osaka Soil Test Laboratory, GRI -- 3.3.5 Auxiliary Data -- 3.4 Results -- 3.4.1 Structural Architecture -- 3.4.2 Basin Accommodation -- References -- 4 Discussion-Origin and Evolution of the Osaka Basin -- 4.1 Comparison Between Proximal and Peripheral Parts of the Basin -- 4.2 Marine-Land Connectivity of Major Structural Trends -- 4.2.1 Awaji-Rokko Fault System and Osaka Bay Fault -- 4.2.2 N-S Warping Zones -- 4.2.3 Median Tectonic Line. , 4.2.4 Broad Contractional Horsts off the Eastern Coast of Awaji Island -- 4.3 Evolutionary Process of the Osaka Basin-A Tectonic Model -- 4.3.1 A Synthesis of the Plio-Pleistocene Tectonic Events -- 4.3.2 Structural Framework of the Present Osaka Basin -- References.
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  • 4
    Online Resource
    Online Resource
    New York :Nova Science Publishers, Incorporated,
    Keywords: Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (96 pages)
    Edition: 1st ed.
    ISBN: 9781536146769
    Series Statement: Geology and Mineralogy Research Developments Series
    Language: English
    Note: Intro -- Contents -- Preface -- Acknowledgments -- Chapter 1 -- Tectonic Overview of the Study Area -- Abstract -- 1. Introduction -- 2. Longstanding Activity on the Median Tectonic Line Since the Late Mesozoic -- 3. Arc Bending Related to the Japan Sea Backarc Spreading in the Miocene -- 4. Development of Extensional Structure in Kyushu Since the Pliocene -- 5. Geophysical Properties of Central Kyushu -- 5.1. Gravity Anomaly and Crustal Structure -- 5.2. Seismicity and Stress-Strain State -- Conclusion -- References -- Chapter 2 -- Geological Background -- Abstract -- 1. Introduction -- 2. Stratigraphy of Land-Exposed Strata -- 3. Structural Features -- 4. Correlation between Land and Marine Sequences -- Conclusion -- References -- Chapter 3 -- Seismic Interpretation -- Abstract -- 1. Introduction -- 2. Survey and Processing Specifications -- 3. Systematic Descriptions -- 3.1. Beppu Bay (Line A) -- 3.2. Beppu Bay (Line B) -- 3.3. Beppu Bay (Line C) -- 3.4. Beppu Bay (Line D) -- 3.5. Beppu Bay (Line E) -- 3.6. Beppu Bay (Line F) -- 3.7. Beppu Bay (Line G) -- 3.8. Beppu Bay (Line H) -- 3.9. Beppu Bay (Line I) -- 3.10. Beppu City (Beppu Coast Line) -- 3.11. Oita Plain (Ono River Line) -- 3.12. Oita Plain (Oita Coast Line) -- 3.13. Oita Plain (2016-A Line) -- 3.14. Oita Plain (Oita River Line) -- 4. Age Control of Seismic Horizons -- 5. Three-Dimensional Architecture of the Studied Basin -- Conclusion -- References -- Chapter 4 -- Fault-Controlled Processes of Basin Evolution -- Abstract -- 1. Introduction -- 2. Hypothesis of the Temporal Migration of an Arc-Bisecting Fault -- 3. Tectonic Context of Recent Contractional/Extensional Episodes -- 4. Remaining Problems and Further Recommended Exploration -- 4.1. Active Faulting under the Effect of Continued Crustal Collision. , 4.2. Recent Seismic Events and Active Segments of the Arc-Bisecting Fault -- Conclusion -- References -- About the Authors -- Index -- Blank Page.
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