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书名 Sedimentary Dynamics of Windfield-Source-Basin System(New Concept for Interpretation and Prediction)(精)
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作者 Zaixing Jiang
出版社 科学出版社
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Zaixing Jiang著的《Sedimentary Dynamics of Windfield-Source-Basin System(New Concept for Interpretation and Prediction)(精)》以风场为主线,以源汇为基础,现代观测与盆地资料相结合,全面阐述风场-物源-盆地系统动力学原理及其在古气候、古地理、油气预测中的应用。由传统沉积相、沉积模式的一维属性,源-汇体系的二维属性,提升到了风场-物源-盆地系统的三维性,使得对沉积体系(包括陆相和海相、碎屑岩和碳酸盐)的成因解释更加合理、对未知区沉积体系(储集体)的分布预测更加全面和准确。
目录
1 The Emergence of Windfield-Source-Basin Dynamics
1.1 Depositional System Advances
1.2 The Influence of Windfield on Depositional System
1.2.1 Influence of Windfield on Clastic Depositional System
1.2.2 Effect of the Wind on Carbonate Depositional System
1.3 Multiple Control of the Genesis and Distribution of Depositional Systems
1.4 Research Significance
1.4.1 Significance in Sedimentology
1.4.2 Significance in Paleoclimate
1.4.3 Significance in Hydrocarbon
References
2 Elements and Research Methods of Sedimentary Dynamics of Windfield-Source-Basin System
2.1 Windfield
2.1.1 The Generation of Wind and Three Kinds of Windfield
2.1.2 The Influence of the Wind
2.1.3 Wind Waves
2.1.4 Distribution of Beach Bar Sand Bodies Under the Influence of Wind Force
2.1.5 Research Methodology of Paleo-Windfield—The Recovery of Paleo-Wind Direction
2.1.6 Paleo-Windfield Research Method—Paleo-Wind Strength Recovery
2.2 Source
2.2.1 Formation of Sediment Source
2.2.2 Control of Source on Sedimentation
2.2.3 Source Analytical Method
2.3 Basin
2.3.1 Basic Characteristics of the Basin
2.3.2 The Influence of Paleogeomorphology on Sedimentation and Its Research Method
2.3.3 Influence of Paleo-water Depth on Sediment Deposition and Its Research Method
2.3.4 Influence of Tectonic Activity on Sedimentation
2.4 Windfield-Source-Basin Dynamics
2.4.1 Interactions Between the Elements of the Windfield-Source-Basin System
2.4.2 Classification of the Windfield-Source-Basin System
References
3 Modern Sedimentary System and Windfield-Source-Basin System Dynamics of Qinghai Lake
3.1 Geographical and Geological Background
3.1.1 Geographical Location
3.1.2 Climate of Qinghai Lake
3.1.3 Hydrology of Qinghai Lake
3.1.4 Stratigraphy of Qinghai Lake Basin
3.1.5 Structural Features and Evolution of Qinghai Lake Basin
3.2 Modern Sedimentary System of Qinghai Lake
3.2.1 The Riyue/Bison Mountain–Daotanghe River–Barrier Island Depositional System
3.2.2 Qinghai Nanshan–Alluvial Fan–Fan Delta/Coast Depositional System
3.3 The Distribution of Modern Depositional System and Windfield-Source-Basin Dynamic Model of Qinghai Lake
3.3.1 The Distribution Characteristics of Modern Depositional System
3.3.2 Main Controlling Factors of the Modern Depositional System of Qinghai Lake
3.3.3 Application of the Windfield-Source-Basin Model
References
4 Paleogene Sedimentary System and Sedimentary Dynamics of Windfield-Source-Basin System in the Dongying Sag
4.1 Geology of the Dongying Sag
4.1.1 Tectonic Setting
4.1.2 Stratigraphic Sequence
4.1.3 Characteristics of Tectonic Evolution
4.2 Sequence Stratigraphic Division of Upper Sha-4 Submember in the Dongying Sag
4.2.1 Identification of Sequence Boundaries (SBs)
4.2.2 Division of Sequence in the Typical Wells
4.2.3 Division of Sequence Stratigraphy
4.3 Sedimentary Facies of Upper Sha-4 Submember in the Dongying Sag
4.3.1 Fan-delta
4.3.2 Subaqueous Gravity Flow Deposits
4.3.3 Delta
4.3.4 Clastic Beach Bar
4.3.5 Carbonate Beach Bar
4.3.6 Storm Deposits
4.3.7 Fine Grain Deposits (Semi-Deep Lake-Deep Lake)
4.3.8 Framework of Sedimentary System
4.4 Dynamics of Windfield-Source-Basin System in Upper Sha-4 Submember
4.4.1 Reconstruction of Paleo-Water Depth
4.4.2 Reconstruction of Paleo-Geomorphology
4.4.3 Analysis of Paleo-Provenance
4.4.4 Reconstruction of Paleowind Force
4.4.5 Paleo-Windfield and Sedimentary Environment
4.4.6 Analysis of Factors Controlling Distribution of Beach Bar Sandbodies
4.4.7 Division of Windfield-Source-Basin System
4.5 Significance of Research on Windfield-Source-Basin System and Prospect of Its Application
4.5.1 Significance of Paleo-Climate
4.5.2 Significance for Petroleum Geology
Refere
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