Re-exploration programs for petroleum-rich sags in rift basins /

Re-exploration Programs for Petroleum-Rich Sags in Rift Basins covers the geological characteristics and potential of oil-rich depressions in a rifted basin. It describes up-to-date research and technology, detailing the current status of exploration. The overall aim of the book is to guide a new ro...

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Bibliographic Details
Main Authors: Zhao, Xianzheng (Author), Jin, Fengming (Author), Zhou, Lihong (Author), Wang, Quan (Author), Pu, Xiugang (Author)
Corporate Author: ScienceDirect (Online service)
Format: eBook
Language:English
Published: Cambridge, MA : Gulf Professional Publishing, [2018]
Subjects:
Online Access:Connect to the full text of this electronic book
Table of Contents:
  • Front Cover
  • Re-exploration Programs for Petroleum-Rich Sags in Rift Basins
  • Copyright
  • Contents
  • About the Authors
  • Petroleum Industry Press
  • Foreword 1
  • Foreword 2
  • Preface
  • Chapter 1: Connotation and Workflow of Re-exploration
  • 1. Necessity of Re-exploration for Oil-Rich Sags
  • 2. Connotation of Re-exploration for Oil-Rich Sags
  • 2.1. Definition of Re-exploration
  • 2.2. Connotation of Re-exploration
  • 3. Workflow of Re-exploration
  • 3.1. Constructing the Sag-Wide Merged 3D Seismic Data Platform
  • 3.2. Reconstructing the Basic Geology of the Sag
  • 3.2.1. Structural reconstruction
  • 3.2.2. Sedimentary reconstruction
  • 3.2.3. Reservoir reconstruction
  • 3.3. Quantitatively Characterizing the Spatial Distribution of Oil and Gas Resources
  • 3.4. Creating the New Model of Multiprospect Hydrocarbon Accumulation
  • 3.5. Multiprospect Overall Preexploration
  • 3.6. Integration of Reserve Addition and Productivity Construction
  • Chapter 2: Construction of Sag-Wide Merged 3D Seismic Data Platform
  • 1. Sag-Wide Merged 3D Seismic Survey
  • 1.1. Overall Deployment
  • 1.1.1. Type I blocks
  • 1.1.2. Type II blocks
  • 1.1.3. Type III blocks
  • 1.2. Second-Round 3D Seismic Data Acquisition
  • 1.2.1. Optimization of acquisition parameters
  • 1.2.2. Step-by-step implementation of second-round 3D seismic data acquisition
  • 1.3. Complex Target-Specific Data Acquisition
  • 1.4. Sag-Wide Merged 3D Seismic Data Processing
  • 1.4.1. Raoyang Sag
  • 1.4.2. Shenxian Sag
  • 1.4.3. Langgu Sag
  • 1.4.4. Baxian Sag
  • 1.4.5. Merged processing in the Jizhong Depression
  • 2. Urban/Mining Area 3D Seismic Survey
  • 2.1. Special Survey Geometry in Large Barrier Zones
  • 2.2. Comprehensive Survey of Near-Surface Barriers
  • 2.3. Realization of Special Survey Geometry in Large Urban/Mining Areas.
  • 2.3.1. Optimization of special survey geometry based on satellite photos
  • 2.3.2. Well-shot and vibroseis combined shooting in urban/mining areas
  • 2.4. Regularization Based on Irregular Folds
  • 2.5. Effect of Urban/Mining Area 3D Seismic Survey
  • 3. Multiphase 3D Seismic Fusion Survey
  • 3.1. Principle
  • 3.2. Multiphase 3D Fusion Geometry
  • 3.2.1. Fold design based on raw data
  • 3.2.2. Survey geometry design based on infilled sampling points
  • 3.2.3. Survey geometry design based on spliced azimuths
  • 3.3. Multiphase 3D Seismic Data Fusion Processing
  • 3.3.1. Bin grid unification and homogenization
  • 3.3.2. Integrated static correction based on time variant
  • 3.4. Effect of Multiphase 3D Seismic Fusion Survey
  • 4. Sag-Wide Merged 3D Seismic Data Processing
  • 4.1. Workflow and Approach of Sag-Wide Merged 3D Seismic Data Processing
  • 4.2. Establishment of Sag-Wide Near-Surface Structural Model
  • 4.2.1. Low-velocity zone correction
  • 4.2.2. Unified datum correction
  • 4.3. Quantitative Wavelet Shaping and Prestack Data Regularization
  • 4.4. Multidomain Multiinformation-Constrained Velocity Modeling
  • Chapter 3: Reconstruction of Sag-Wide Structural Framework
  • 1. Structural Interpretation of Sag-Wide 3D Seismic Data Volume
  • 1.1. ``Four-Step´´ Regional Seismic-Geology Stratigraphic Correlation
  • 1.1.1. Select critical wells for fine horizon calibration
  • 1.1.2. Combine well data and seismic data of main seismic lines to determine the stratigraphic correlation scheme
  • 1.1.3. Compare well data and seismic data to unify the geologic zonation of a whole sag
  • 1.1.4. Establish the drilling zonation database of the merged 3D survey
  • 1.2. Structural Interpretation Through ``Stereoscopic Quick Network Construction, and Combination of Plane and Section´´.
  • 1.2.1. SOF to improve the capacity of fault identification based on seismic data
  • 1.2.2. Massively-merged time slices to quickly interpret first-order and second-order faults
  • 1.2.3. Massively merged geometric seismic attributes to assist the interpretation of third-order and fourth-order faults
  • 1.2.4. Automatic tracing of horizons with strong reflection and good continuity
  • 1.2.5. Stereoscopic quick network construction by combining plane and section to set up interpretation framework
  • 1.2.6. Geologic knowledge to guide the precise interpretation of complex structure zones
  • 1.2.7. Seismic attribute fusion to make precise structural interpretation
  • 2. Overall Structural Features
  • 2.1. Structural Framework of ``Belts in an EW Direction and Regions in an SN Direction´´
  • 2.1.1. Belts in an EW direction
  • Central uplift
  • Western sag belt
  • Eastern sag belt
  • 2.1.2. Regions along SN direction
  • North region
  • Central region
  • South region
  • 2.2. Features of Basement Faults
  • 2.2.1. Fault properties
  • 2.2.2. Fault orders
  • 2.2.3. Fault assemblage styles
  • Fault assemblage styles in plane
  • Parallel fault assemblage
  • Net-like fault assemblage
  • Parallel-arc fault assemblage
  • Comb-like fault assemblage
  • Broom-like fault assemblage
  • Linear fault assemblage
  • Oblique fault assemblage
  • En echelon fault assemblage
  • Fault assemblage styles on sections
  • Fault assemblage styles on sections
  • Step-shaped fault-block assemblage
  • Graben-horst assemblage
  • 2.3. Structural Styles
  • 2.3.1. Extensional structural style
  • Drape anticline structure on a buried hill
  • Anticline structure with subsided top of basement uplift
  • Roll-over anticline structure
  • Graben antiformal structure with stratigraphic compensation
  • Gravity-slip anticline
  • 2.3.2. Strike-slip structural style
  • Negative flower structure.
  • En echelon structure
  • Broom-like structure
  • 2.3.3. Compressional structural style
  • 3. Features of Weak Structure Zones
  • 3.1. Basic Features of Weak Structure Zones
  • 3.2. Identification Indexes of Weak Structure Zones
  • 3.2.1. Bottom curvature K (m-1)
  • 3.2.2. Derivative of formation thickness variation rate Ah (km-1)
  • Formation thickness variation rate
  • Derivative of formation thickness variation rate
  • Areal density of faults
  • 3.2.3. Areal density of fault throw M (km2)
  • 3.3. Distribution of Weak Structure Zones
  • 3.4. Evolution of Weak Structure Zones
  • 3.4.1. Zoning of tectonic activity intensity in the Kongdian Formation-Sha 4 Member
  • 3.4.2. Zoning of tectonic activity intensity in the Sha 3 Member-Sha 2 Member
  • 3.4.3. Zoning of tectonic activity intensity in the Sha 1 Member-Dongying Formation
  • 3.4.4. Zoning of tectonic activity intensity in the Neogene-Quaternary
  • 3.4.5. Evolution patterns of weak structure zones
  • 4. Structural Evolution Features
  • 4.1. Thrusting in an SE Direction During the Yanshanian Orogeny
  • 4.2. Extension in an SEE Direction During the Deposition of the Kongdian Formation-Sha 4 Member
  • 4.3. Extension in an SE Direction During the Deposition of the Sha 3 Member-Sha 2 Member
  • 4.4. Extension and Strike-slipping in an SSE Direction During the Deposition of Sha 1 Member-Dongying Formation
  • 4.5. Sagging During the Neogene
  • Chapter 4: Reconstruction of Sag-Wide Depositional System
  • 1. Establishment of Sequence Stratigraphic Framework
  • 1.1. Identification of the Sequence Boundary
  • 1.1.1. Identification of the first- and second-order sequence boundaries
  • 1.1.2. Identification of the third-order SB
  • 1.1.3. Identification of the boundary in sequence
  • FFS (First Flooding Surface)
  • Maximum Flooding Surface (MFS)
  • 1.2. Establishment of Sequence Stratigraphic Framework.
  • 1.2.1. Sequence division and correlation
  • Lower sequence
  • Middle sequence
  • Upper sequence
  • SQ1
  • SQ2
  • SQ3
  • SQ4
  • SQ5
  • SQ6
  • SQ7
  • SQ8
  • SQ9
  • SQ10
  • SQ11
  • SQ12
  • SQ13
  • 1.2.2. Systems tract division
  • Division of lacustrine sequence systems tract (LSST)
  • LST
  • TST
  • HST
  • Division of fluvial sequence systems tract (FSST)
  • Base-level rising systems tract
  • Base-level falling systems tract
  • Division of parasequence and parasequence set
  • Prograde parasequence set (PPSS)
  • Retrogradational parasequence set (RPSS)
  • Aggradational parasequence set (APSS)
  • 1.3. Characteristics and Controlling Factor of Sequence Stratigraphy
  • 1.3.1. Characteristics of sequence stratigraphy
  • Vertical and horizontal sequence developments have obvious differences
  • Different types of subsags have multiple types of superimposition patterns
  • Superimposition pattern of inherited subsag sequence
  • Superimposition pattern of reverse subsag sequence
  • Superimposition pattern of early growth type subsag sequence
  • Superimposition pattern of offset type subsag sequence
  • Superimposition pattern of systems tract is different in different zones and different stages
  • Superimposition pattern of systems tract is different in different zones
  • a. Superimposition pattern of the systems tract in gentle slope belt
  • b. Superimposition pattern of the systems tract in steep slope belt
  • Superimposition pattern of systems tract is different at different stages
  • a. Superimposition pattern of rapid lake-forming systems tract
  • b. Superimposition pattern of slow lake-forming systems tract
  • 1.3.2. Controlling factor of sequence stratigraphy
  • The stage of regional tectonic activities controls the development of second-order sequences
  • Difference of boundary fault activities controls the configuration of third-order sequences.