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
References

5 Depositional Systems and Windfield-Source-Basin System Dynamics of the West Sag，Liaohe Depression，Bohai Bay Basin
5．1 Geologic Setting
5．1．1 Tectonic Divisions
5．1．2 Strata Characteristics
5．2 Sequence Stratigraphy Framework
5．2．1 Recognition of Sequence Boundaries
5．2．2 The Establishment of Sequence Stratigraphy Framework by Combination of Wells and Seismic Data
5．3 Sedimentary Systems and “Windfield-Source-Basin System” Depositional Dynamics
5．3．1 Sedimentary Facies
5．3．2 Depositional Model of Beach-Bar Deposits in the West Sag，Liaohe Depression
5．3．3 Windfield-Source-Basin System in the Upper Es4 West Sag，Liaohe Depression
5．4 Detailed Study of Beach-Bar Deposits
5．4．1 High-Resolution Stratigraphy Framework
5．4．2 Sedimentary Systems of Beach-Bar in the Shubei Area
5．5 Controlling Factors for the Distribution of Beach-Bar Deposits
5．5．1 Reconstruction of Paleo-Geomorphology
5．5．2 Reconstruction of Paleo-Water Depth
5．5．3 Reconstruction of Paleo-Source
5．5．4 Reconstruction of Paleo-Windfield
5．5．5 Controlling Effect of Windfield-Source-Basin System on Beach-Bar Deposition
References

6 The Sedimentary Characteristics of Paleogene Conglomerates and Their Sedimentary Dynamics in Source-to-Sink System in the Langgu Sag
6．1 Geologic Background
6．2 Sedimentary Characteristics of the Conglomerate Body
6．2．1 Rock Type
6．2．2 Texture Characteristics
6．2．3 Sedimentary Structures
6．2．4 Gravel Compositions
6．2．5 Interstitial Components
6．2．6 Mudstone Between Conglomerates
6．3 Palaeogeomorphology Restoration
6．3．1 Residual Topography of Highs
6．3．2 Morphology of the Basin Controlling Fault
6．3．3 Basin Paleomorphology
6．3．4 Paleomorphology Models
6．4 Paleo-Provenance Restoration
6．4．1 Residual Strata
6．4．2 Distribution of Gravel Components in Conglomerate
6．4．3 The Paleogeologic Evolution of the Daxing High
6．5 Source-Basin and Sedimentary Model
6．5．1 Fault-Trough Gravity Flow
6．5．2 Debris Flow Nearshore Subaqueous Fan
6．5．3 Mudslides Nearshore Subaqueous Fan
6．5．4 Distribution Characteristics of the Conglomerate
6．6 Reservoir and Oil-Gas
6．6．1 Controls of Gravels on Reservoir
6．6．2 Controls of Conglomerate Genetic Types on Hydrocarbons
References

7 A Source-to-Sink Study of the Paleogene Shulu Sag：Characteristics and Depositional Dynamics of Its Deposits
7．1 Geological Background
7．1．1 Overview
7．1．2 Regional Tectonic Features
7．1．3 Basin Evolution
7．1．4 Stratigraphy
7．1．5 Sequence Stratigraphy of the Lower Es3 Submember
7．2 Sedimentary Characteristics of the Lower Es3 Submember
7．2．1 Rock Classification Scheme
7．2．2 Gravel Composition
7．2．3 Well Log Identification
7．2．4 Lithology Distribution
7．3 The Impact of Tectonic Activity on Sedimentation
7．3．1 Types and Characteristics of Seismites
7．3．2 Seismites Sequence
7．3．3 Criterion of Seismites
7．4 Provenance and Depositional Processes of the Calcirudites
7．4．1 Depositional Environments and Facies Models of the Calcirudites
7．4．2 Distribution of the Calcirudites
7．4．3 Relationship Between Two Types of Calcirudites
References

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