Seismic Geology and Basin Analysis

Case Studies on Sedimentary Basins in China

1st Edition - June 23, 2024
Editor: Changsong Lin
Language: English
Paperback ISBN:
9 7 8 - 0 - 3 2 3 - 9 5 9 0 9 - 4
eBook ISBN:
9 7 8 - 0 - 3 2 3 - 9 5 9 1 0 - 0

Seismic Geology and Basin Analysis: Case Studies on Sedimentary Basins in China introduces the principles, approaches and techniques needed to solve problems using seismic d… Read more

Purchase options

SUSTAINABLE DEVELOPMENT

Innovate. Sustain. Transform.

Save up to 30% on top Physical Sciences & Engineering titles!

Explore now

Physical science & engineering for sustainable development book covers

Institutional subscription on ScienceDirect

Request a sales quote

Seismic Geology and Basin Analysis: Case Studies on Sedimentary Basins in China introduces the principles, approaches and techniques needed to solve problems using seismic data calibrated with well log, cores and outcrop profiles. The book emphasizes the adoption of seismic techniques into basin analysis and broadens the usage of seismic data in geological research which may be referred to as “seismic geology.” The principle of the book is mainly summarized from a series of case studies in different basins in China. In addition, through this book readers can understand the primary characteristics and basin fill evolution of major petroleum basins around the world.

When starting research on a basin, researchers and professionals are confronted with how to reveal the general architecture of basin fills and depict three-dimensional geometry, and the internal architecture of subsurface depositional bodies and their arrangement, hence this book is a great tome on necessary areas of exploration.

Title of Book
Cover image
Title page
Table of Contents
Copyright
Contributors
Foreword 1
Foreword 2
Preface
Part 1. Primary principles and approaches
Chapter 1. Introduction
Chapter 1.1 From seismic stratigraphy to sequence stratigraphy
Chapter 1.2. Seismic sedimentology and geomorphology
Chapter 1.3. Seismic geology and basin analysis
Chapter 2. Basin-fill units and stratigraphic surfaces
Chapter 2.1 Sequence stratigraphic units and their hierarchy
2.1.1 Depositional sequence
2.1.2 Hierarchy of sequence stratigraphic units
2.1.2.1 Sequence stratigraphic units
2.1.2.2 High order sequence stratigraphic units
2.1.2.2.1 First- and second-order sequence stratigraphic units
2.1.2.2.2 Third-order sequence stratigraphic units
2.1.2.2.3 Composite sequences
2.1.2.3 Lower order sequence stratigraphic units
Chapter 2.2. Boundaries of sequence stratigraphic units and their seismic reflections
2.2.1 Stratigraphic surfaces and stratal termination types
2.2.1.1 Stratigraphic surfaces
2.2.1.2 Stratal termination types
2.2.1.2.1 Truncation or denudation
2.2.1.2.2 Onlap and downlap
2.2.1.2.3 Toplap and offlap
2.2.2 Regressive-erosional unconformity
2.2.2.1 Subaerial erosional unconformity
2.2.2.2 Surface of forced regression
2.2.2.3 Maximum regressive surface
2.2.3 Transgressive surface
2.2.3.1 Initial flooding surface
2.2.3.2 Maximum flooding surface and condensed section
2.2.3.2.1 Maximum flooding surface
2.2.3.2.2 Condensed section
Chapter 2.3. Depositional systems tracts and their composite styles
2.3.1 Depositional systems tracts
2.3.1.1 Lowstand systems tracts
2.3.1.2 Transgressive systems tracts
2.3.1.3 Highstand systems tracts
2.3.1.4 Falling stage systems tracts
2.3.2 Depositional systems tracts in continental basins
2.3.2.1 Systems tracts in clastic lacustrine sedimentary sequences
2.3.2.2 Systems tracts of fluvial sedimentary sequences
2.3.3 Depositional systems tracts of carbonate sequences
Chapter 2.4. Genetic depositional types and trajectory analysis
2.4.1 Genetic depositional types
2.4.2 Trajectory of sedimentary systems
2.4.3 Clinoforms and trajectory classification
2.4.4 Quantitative description of trajectories
Chapter 3. Seismic sedimentary analysis
Chapter 3.1. Seismic facies
3.1.1 External shape
3.1.2 Internal reflection configuration
3.1.3 Reflection parameters
Chapter 3.2. Seismic sedimentological geomorphology
3.2.1 Basic analysis principle
3.2.2 Technical methods
Chapter 3.3. Seismic facies mapping and basin paleogeography
3.3.1 Paleogeography of sedimentary basins
3.3.2 Seismic paleogeographic mapping and interpretation
Chapter 4. Structural framework and tectonostratigraphy of sedimentary basins
Chapter 4.1 Tectonostratigraphic frameworks of sedimentary basins
Chapter 4.2. Tectonic unconformity and paleo-uplift
4.2.1 Unconformity erosion amount
4.2.2 Distribution patterns of unconformities
4.2.3 Paleo-uplift geomorphology
4.2.3.1 Development and evolution of paleo-uplifts in basins
4.2.3.2 Restoration of paleo-uplift landforms
Chapter 4.3. Syndepositional structures and structural slope-break zones
4.3.1 Syndepositional structures
4.3.1.1 Basin basement structure
4.3.1.2 Basin marginal faults
4.3.1.3 Intrabasinal syndepositional faults
4.3.1.4 Inverted structures
4.3.2 Tectonic paleogeomorphology
4.3.2.1 Syndepositional fault systems and the distribution of sedimentary sand bodies
4.3.3 Tectonic slope-break zone
4.3.3.1 Basic characteristics of tectonic slope-break zones
4.3.3.2 Distribution of tectonic slope-break zones and sedimentary systems
Part 2. Case studies
Chapter 5. Siliciclastic sequence stratigraphy and basin fill dynamic
Chapter 5.1 Lower Cretaceous depositional evolution from lacustrine to fluvial environment of an intracontinental depression and controlling factors, northern Tarim Basin
5.1.1 Geological setting
5.1.2 Basic information of seismic data
5.1.3 Sequence stratigraphy
5.1.3.1 Sequence boundary characteristics
5.1.3.1.1 Sequence boundary TK1bx
5.1.3.1.2 Sequence boundary TK1bs
5.1.3.1.3 Sequence boundary TK1bs-SB3 and SB4
5.1.3.1.4 Sequence boundary TE
5.1.3.2 Division of systems tracts
5.1.4 Depositional systems identification in seismic data
5.1.4.1 Seismic facies in Baxigai Formation (SQ1)
5.1.4.2 Seismic facies in Bashijiqike Formation (SQ2–SQ4)
5.1.5 Conclusion
Chapter 5.2. Deep-water gravity-flow deposits of the Late Ordovician in the Tarim Basin
5.2.1 Introduction
5.2.2 Geological setting
5.2.3 Methods and database
5.2.4 Sequence stratigraphic framework
5.2.5 Depositional architecture of the gravity flow systems
5.2.5.1 Lithofacies and lithofacies associations
5.2.5.2 Depositional-paleogeomorphological elements
5.2.5.2.1 Submarine canyons or incised channels
5.2.5.2.2 Broad and shallow erosional channels
5.2.5.2.3 Erosional-depositional channel and levee-overbank complexes
5.2.5.2.4 Frontal splays-lobes and nonchannelized turbidite sheets
5.2.5.2.5 Calciclastic lower slope fans and channels-lobes or sheets
5.2.5.2.6 Debris flow complexes
5.2.6 Systems tract architecture and sea-level change
5.2.7 Tectonic and paleogeographical setting of the Late Ordovician Tarim Basin
5.2.7.1 Tectonic setting
5.2.7.2 Paleogeography and sediment dispersal patterns
5.2.8 Distribution of potential reservoirs in gravity flow depositional systems
5.2.9 Conclusions
Chapter 5.3. Evolution of depositional sequences in response to tectonism, sea-level change, and sediment supply on the northern continental margin of the South China Sea
5.3.1 Introduction
5.3.2 Geological setting
5.3.3 Depositional systems and depositional-geomorphological characteristics
5.3.3.1 Shelf-edge delta and clastic shoreline depositional systems
5.3.3.1.1 Lithofacies associations and depositional facies
5.3.3.1.2 Seismic sedimentological and geomorphological characteristics
5.3.3.2 Prodelta slope turbidite fan systems
5.3.3.2.1 Lithofacies associations and depositional facies
5.3.3.2.2 Seismic sedimentological and geomorphological characteristics
5.3.3.3 Incised valleys and unidirectionally migrating channel systems
5.3.3.4 Fine-grained slope fan depositional systems
5.3.3.5 Large-scale fault-slump complexes and soft deformed beds
5.3.3.6 Clinoforms of the continental slope margin
5.3.4 Sequence architecture and depositional evolution
5.3.4.1 Composite sequence 3 (CS3)
5.3.4.2 Composite sequence 4 (CS4)
5.3.4.3 Composite sequence 5 (CS5)
5.3.4.4 Composite sequence 6 (CS6)
5.3.4.5 Composite sequence 7 (CS7)
5.3.5 Constraints on the depositional–geomorphological evolution
5.3.5.1 Migration of the continental slope-break zone
5.3.5.2 Evolution of the deposition and tectonic setting
5.3.5.2.1 Late Oligocene to Middle Miocene (CS3-5)
5.3.5.2.2 Middle Miocene to Quaternary (CS5-7)
5.3.5.3 Sea-level changes
5.3.5.4 Sediment supply and climate change
5.3.6 Conclusions
Chapter 5.4. Changes of the Oligocene to Quaternary deltaic depositional architecture from inner-shelf to shelf-margin, the Pearl River Mouth Basin, northern South China Sea
5.4.1 Introduction
5.4.2 Geologic setting
5.4.3 Data and research methods
5.4.4 Lithofacies associations and depositional environments
5.4.4.1 Lithofacies associations FA1–3: fluvial to delta–plain deposits
5.4.4.1.1 Description
5.4.4.1.2 Interpretation
5.4.4.2 Lithofacies associations FA4–6: delta-front deposits
5.4.4.2.1 Description
5.4.4.2.2 Interpretation
5.4.4.3 Lithofacies associations FA8 and FA9: delta-margin sandy bars and foreshore deposits
5.4.4.3.1 Description
5.4.4.3.2 Interpretation
5.4.4.4 Lithofacies associations FA10–FA11: sandy slope-fan deposits
5.4.4.4.1 Description
5.4.4.4.2 Interpretation
5.4.4.5 Lithofacies associations FA12–13: slump deformed beds and debris flow deposits
5.4.4.5.1 Description
5.4.4.5.2 Interpretation
5.4.5 Seismic facies and geomorphology
5.4.6 Inner-shelf delta systems
5.4.7 Shelf-edge deltas and associated slope-fan systems
5.4.7.1 Shelf-edge delta systems
5.4.7.2 Slope fan systems related to shelf edge delta
5.4.8 Evolution of the deltaic systems and controlling processes
5.4.8.1 Time-space distribution of the deltaic systems with the relative sea-level change
5.4.8.2 Late Oligocene to Early Miocene: inner-shelf to shelf-edge deltaic systems
5.4.8.3 Early Miocene to Pliocene: inner-shelf to outer-shelf deltaic systems
5.4.8.4 Pleistocene to Early Holocene: outer-shelf to shelf-edge deltaic systems
5.4.9 Conclusions
Chapter 5.5. Sedimentary pattern and filling process in the central canyon: A case study in the eastern Lingshui depression, Qiongdongnan Basin
5.5.1 Introduction
5.5.2 Geological setting
5.5.3 Methods and materials
5.5.4 Results
5.5.4.1 Seismic facies and sedimentary elements within the central canyon
5.5.4.1.1 Erosion surfaces
5.5.4.1.2 Basal lag
5.5.4.1.3 Turbidite channel complexes
5.5.4.1.4 Lobe complex
5.5.4.1.5 Mass transport deposits
5.5.4.1.6 Pelagic deposits
5.5.4.2 Sedimentary units
5.5.5 Discussion
5.5.5.1 Stacking patterns and filling processes
5.5.5.1.1 Phase 1: Repeated cut and fill
5.5.5.1.2 Phase 2: High N:G channel complex
5.5.5.1.3 Phase 3: Low N:G channel and pelagic shale
5.5.5.1.4 Phase 4: Sandy-lobe complex sedimentary phases
5.5.5.1.5 Phase 5: Mass transport deposits
5.5.5.2 Analysis of the possible controlling factors
5.5.5.2.1 Ancient seafloor morphology
5.5.5.2.2 Sediment supply
5.5.5.2.3 Sea-level fluctuations
5.5.5.2.4 Tectonic activities
5.5.6 Conclusions
Chapter 5.6. Source to sink systems of the upper Oligocene delta and slope fan systems, the Pearl River Mouth Basin
5.6.1 Introduction
5.6.2 Geological setting
5.6.3 Data and methods
5.6.4 Lithofacies associations and depositional environments
5.6.4.1 Lithofacies associations FA1-4: Shelf margin slump deposits and gravity flow channel fills
5.6.4.1.1 Description
5.6.4.1.2 Interpretation
5.6.4.2 Lithofacies associations FA5-9: Slope deposits
5.6.4.2.1 Description
5.6.4.2.2 Interpretation
5.6.5 Seismic facies and geomorphology
5.6.5.1 SF1-2: Shelf margin incised channel fills
5.6.5.1.1 Description
5.6.5.1.2 Interpretation
5.6.5.2 SF3: Slump and debris flow deposits
5.6.5.2.1 Description
5.6.5.2.2 Interpretation
5.6.5.3 SF4: Slope gully fills
5.6.5.3.1 Description
5.6.5.3.2 Interpretation
5.6.5.4 SF5: Lower slope slump-debris flow deposits
5.6.5.4.1 Description
5.6.5.4.2 Interpretation
5.6.5.5 SF6–SF8: Slope fan deposits
5.6.5.5.1 Description
5.6.5.5.2 Interpretation
5.6.6 Variation of deposition from shelf-edge to lower slope
5.6.6.1 Shelf-edge incised channels and shelf-edge deltas
5.6.6.2 Amalgamated slump-channels
5.6.6.3 Slope gullies
5.6.6.4 Debris flow and slope fan deposits
5.6.7 Sequence stratigraphy
5.6.8 Sediment dispersal from shelf-edge to slope fan deposits
5.6.9 Sea-level change and steep slope clinoform
5.6.10 Conclusions
Chapter 5.7. Shelf-margin depositional architecture variability across the mid-Pleistocene climate transition, the Pearl River Mouth Basin
5.7.1 Sequence framework and chronological constraints
5.7.1.1 Sequence classification
5.7.1.2 Chronological constraints
5.7.2 Sequence architecture and depositional systems tracts
5.7.2.1 Sequence architecture
5.7.2.2 Depositional systems tracts
5.7.3 Control of the Milankovitch glacio-eustatic cycles
5.7.3.1 High-frequency (Milankovitch) sequence framework
5.7.3.2 Coupling of the sequences with Milankovitch cycles
5.7.4 Control of the climatic transition
5.7.4.1 Climatic condition of the Quaternary
5.7.4.2 Sea-level changes driven by climatic conditions
5.7.4.3 Variations in sediment supply driven by climatic conditions
5.7.4.4 Deposition responses to climate conditions
5.7.5 Conclusions
Chapter 5.8. Sequence architecture, depositional evolution, and controlling process, the Erlian Basin
5.8.1 Introduction
5.8.2 Basin setting
5.8.3 Sequence classification
5.8.4 Depositional systems
5.8.4.1 Alluvial fan deposits
5.8.4.2 Fan delta and braided delta deposits
5.8.4.3 Shallow lacustrine and deep lacustrine fine-grained deposits
5.8.4.4 Sublacustrine fan deposits
5.8.4.5 Incised valley fills
5.8.5 Depositional systems tracts
5.8.6 Basin filling evolution and reservoir facies
5.8.7 Controls on sequence development
5.8.7.1 Syndepositional faulting
5.8.7.2 Lake-level variation
5.8.7.3 Balance between accommodation and sediment supply
5.8.7.4 Simulation
5.8.8 Conclusions
Chapter 6. Carbonate platform architecture and depositional evolution
Chapter 6.1 Depositional architectures and their controlling processes of the Ordovician carbonate platform margins in the Tarim Basin
6.1.1 Introduction
6.1.2 Regional geological setting
6.1.3 Research methods
6.1.4 Stratigraphy and lithofacies associations
6.1.5 Depositional sequence framework of the carbonate platform margin zone
6.1.5.1 Sequence stratigraphic unit CS1
6.1.5.2 Sequence stratigraphic unit CS2
6.1.5.3 Sequence stratigraphic unit CS3
6.1.5.4 Sequence stratigraphic unit CS4
6.1.5.5 Sequence stratigraphic units CS5 and CS6
6.1.6 The evolution of the carbonate platform margin and their constraints of tectonism and sea-level changes
6.1.6.1 Arcuate carbonate platform margin zone of the Early and Middle Ordovician along the Manjiaer deep-water basin slope margin
6.1.6.2 Evolution of the carbonate platform from the Middle to Late Ordovician
6.1.6.3 Sea-level history
6.1.7 Conclusion
Chapter 6.2. Modeling of stratigraphic architecture of carbonate platform margin, Late Ordovician Lianglitage Formation, Central Tarim Basin
6.2.1 Introduction
6.2.2 Geological setting
6.2.3 Sequence stratigraphy and sedimentary characteristics
6.2.4 Carbonate platform architecture of the Lianglitage Formation
6.2.5 Controlling factors of carbonate deposition
6.2.5.1 Influences of sea-level change on the architecture of carbonate platform
6.2.5.2 Carbonate productivity
6.2.5.3 Subsidence of gravitational balance
6.2.6 Model result analysis
6.2.7 Conclusions
Chapter 6.3. Microfacies and depositional environments of Late Ordovician Lianglitage Formation, the Tazhong Uplift, the Tarim Basin
6.3.1 Geological setting and stratigraphy
6.3.2 Materials and methods
6.3.3 Depositional sequences
6.3.4 Microfacies analysis
6.3.5 Sedimentary models
6.3.6 Discussion
6.3.7 Conclusions
Chapter 6.4. Paleocave architectures and controlling processes of the Ordovician carbonate paleokarst systems in the western margin and central Tarim Basin
6.4.1 Geological setting and stratigraphy
6.4.2 Materials and methods
6.4.3 Distribution of unconformities
6.4.4 Paleokarst characteristics in the Ordovician carbonate system
6.4.4.1 Large caves
6.4.4.2 Karst cave fills in the Ordovician carbonate system
6.4.4.3 Dense vugs and small caves
6.4.4.4 Dissolution fractures
6.4.5 Paleokarst system along the unconformities in the Tazhong area
6.4.6 Paleokarst sequence correlation between wells
6.4.7 Controlling factors of paleokarst
6.4.7.1 Tectonic movements and unconformities
6.4.7.2 Tectonic geomorphology
6.4.7.3 Lithofacies
6.4.7.4 Faults and fractures
6.4.8 Conclusion
Chapter 7. Unconformities, paleostructural geomorphology and tectonosedimentology
Chapter 7.1 Major unconformities, stratigraphic architecture, and tectonosedimentary evolution of the superimposed Tarim Basin
7.1.1 Introduction
7.1.2 Geological setting
7.1.3 Data and methods
7.1.4 Distribution of major unconformities
7.1.5 Tectonostratigraphy framework and basin filling
7.1.5.1 Tectonostratigraphic unit I
7.1.5.2 Tectonostratigraphic unit II
7.1.5.3 Tectonostratigraphic unit III
7.1.5.4 Tectonostratigraphic unit IV
7.1.5.5 Tectonostratigraphic unit V
7.1.5.6 Tectonostratigraphic unit VI
7.1.5.7 Tectonostratigraphic unit VII
7.1.6 Conclusions
Chapter 7.2. Mesozoic tectonic unconformities in the Tarim Basin: Distribution, geomorphology, and evolution of tectonogeography
7.2.1 Introduction
7.2.2 Geological setting
7.2.3 Data and methods
7.2.4 Distribution of Mesozoic major unconformities
7.2.4.1 Distribution of unconformity TT and uplifting of the Tabei Uplift
7.2.4.2 Distribution of unconformity TJ and enlargement of palaeouplifts
7.2.4.3 Distribution of unconformity TK indicating another tectonic deformation event
7.2.4.4 Distribution of unconformity TE and exposure of Wensu Paleouplift
7.2.5 Evolution of geomorphology
7.2.6 Reconstruction of tectonopaleogeography
7.2.6.1 Sequence classification
7.2.6.2 Deposits identification
7.2.6.2.1 Braided river delta depositional system
7.2.6.2.2 Delta depositional system
7.2.6.2.3 Beach bar depositional system
7.2.6.2.4 Alluvial fan/fan delta depositional system combination
7.2.6.3 Filling stratigraphy
7.2.6.4 Paleogeographic evolution
7.2.6.4.1 Late Triassic (I-SQ3)
7.2.6.4.2 Early Jurassic (II-SQ1)
7.2.6.4.3 Late period of the K1kp (Ⅲ-SQ4)
7.2.6.4.4 Late period of K1bs (Ⅳ-SQ3)
7.2.7 Conclusions
Chapter 7.3. Tectonic geomorphology and depositional pattern of the Paleozoic central uplift belt in the Tarim Basin
7.3.1 Introduction
7.3.2 Geological setting and tectono-stratigraphic sequences
7.3.3 Methodology for paleogeomorphic reconstruction
7.3.3.1 Flattening the overlying sedimentary layers of uplift
7.3.3.2 Distribution pattern of unconformities and relevant uplift paleogeomorphology
7.3.4 Paleozoic paleostructural geomorphology and its constraint on the development of sedimentary facies
7.3.4.1 Middle to Late Ordovician
7.3.4.2 Paleostructural geomorphology of Early Silurian and Late Devonian
7.3.5 Conclusions
Chapter 7.4. Geomorphology control on the distribution of depositional systems, Devonian Donghetang Formation in the Tarim Basin
7.4.1 Introduction
7.4.2 Regional setting
7.4.3 Data and methods
7.4.3.1 Seismic, well, and outcrop data
7.4.3.2 Paleogeomorphology reconstruction
7.4.4 Sequence composition and depositional system of Donghetang Formation
7.4.4.1 Sequence stratigraphic framework
7.4.4.2 Depositional systems within sequence SQ_Ddh
7.4.4.2.1 Shoreface system
7.4.4.2.2 Delta systems
7.4.5 Depositional paleogeomorphology of sequence SQ_Ddh
7.4.5.1 Paleogeomorphology reconstruction method
7.4.5.2 Paleogeomorphology
7.4.6 The impact of paleogeomorphology on the development of the sedimentary system
7.4.6.1 Paleogeomorphology and depositional system development
7.4.6.2 Favorable reservoir distribution and paleogeomorphology
7.4.7 Conclusions
Chapter 7.5. Controls of syndepositional structures on the development of paleogeomorphology and depositional systems, Bohai Bay Basin
7.5.1 Basin setting
7.5.2 Basin filling sequence and episodic rifting
7.5.3 Control of syndepositional faults and their arrangements on depositional patterns
7.5.3.1 Fault slope-break zones
7.5.3.2 Arrangement patterns of fault slope-break zones and the distribution of depositional systems
7.5.3.3 Control of fault slope-break zones on the depositional pattern of deep lacustrine sequences of the third member of the Shahejie Formation
7.5.4 Structural paleogeomorphic features of distinctive syndepositional fault arrangements and the related sandy sediment dispersal systems
7.5.4.1 Comb-like structure
7.5.4.2 Fault transfer accommodation zones and fault tips
7.5.4.3 Broom-like and fork-shaped structures
7.5.5 Prediction of sandstone reservoirs along fault slope-break zones
7.5.6 Discussion and conclusion
Chapter 7.6. Syndepositional fault constraints on sequence architecture and depositional systems in a multiple-rift lacustrine basin, the central Bohai Bay Basin
7.6.1 Introduction
7.6.2 Geological setting
7.6.3 Methods
7.6.4 Result
7.6.4.1 Sequence stratigraphy
7.6.4.2 Thickness patterns
7.6.4.3 Depositional systems
7.6.4.4 Fan-delta deposits
7.6.4.5 Braid-delta deposits
7.6.4.6 River-delta deposits
7.6.4.7 Shallow lacustrine deposits
7.6.4.8 Deep lacustrine deposits
7.6.4.9 Sublacustrine fan deposits
7.6.5 Discussion
7.6.5.1 Lake depths
7.6.5.2 Basin evolution
7.6.6 Controls on sequence evolution
7.6.6.1 Tectonics
7.6.6.2 Sediment supply
7.6.6.3 Climate
7.6.6.4 Hydrocarbon potential
7.6.7 Conclusions
Chapter 7.7. Breakup unconformities in the Pearl River Mouth Basin: Significance for the evolution of basin dynamics and paleogeography
7.7.1 Introduction
7.7.2 Geological background and basin expansion history
7.7.3 Methods and data
7.7.4 Results
7.7.4.1 Fault activity
7.7.4.2 Breakup unconformity
7.7.4.3 Uplift area (angular unconformity zone)
7.7.4.4 Subuplift (local unconformity and onlap zone)
7.7.4.5 Conformity zone
7.7.4.6 Erosion amount and distribution
7.7.5 Discussion
7.7.5.1 Erosion amount in different basin positions
7.7.5.2 Fault activity and prolonged syn-rift stage
7.7.6 Conclusion
Index

Life Sciences

Physical Sciences & Engineering

Social Sciences & Humanities

Health

Seismic Geology and Basin Analysis

Case Studies on Sedimentary Basins in China

Purchase options

Innovate. Sustain. Transform.

Institutional subscription on ScienceDirect

Changsong Lin

Related books