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Seismic geology and basin analysis : case studies on sedimentary basins in China /

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.

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Bibliografiske detaljer
Andre forfattere: Lin, Changsong (Editor)
Format: Electronisk eBog
Sprog:engelsk
Udgivet: Amsterdam ; Cambridge, MA : Elsevier, [2024]
Fag:
Sedimentary basins > China.
Seismology > China.
Sismologie > Chine.
Sedimentary basins
Seismology
China
Online adgang:ScienceDirect
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Indholdsfortegnelse:
  • Front Cover
  • Seismic Geology and Basin Analysis
  • Seismic Geology and Basin Analysis: Case Studies on Sedimentary Basins in China
  • Copyright
  • Contents
  • Contributors
  • Preface
  • 1
  • Primary principles and approaches
  • 1
  • Introduction
  • 1.1
  • From seismic stratigraphy to sequence stratigraphy
  • References
  • 1.2
  • Seismic sedimentology and geomorphology
  • References
  • 1.3
  • Seismic geology and basin analysis
  • 2
  • Basin-fill units and stratigraphic surfaces
  • 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
  • References
  • 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
  • References
  • 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
  • References
  • 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
  • References
  • 3
  • Seismic sedimentary analysis
  • 3.1
  • Seismic facies
  • 3.1.1 External shape
  • 3.1.2 Internal reflection configuration
  • 3.1.3 Reflection parameters
  • References
  • 3.2
  • Seismic sedimentological geomorphology
  • 3.2.1 Basic analysis principle
  • 3.2.2 Technical methods
  • References
  • 3.3
  • Seismic facies mapping and basin paleogeography
  • 3.3.1 Paleogeography of sedimentary basins
  • 3.3.2 Seismic paleogeographic mapping and interpretation
  • References
  • 4
  • Structural framework and tectonostratigraphy of sedimentary basins
  • 4.1
  • Tectonostratigraphic frameworks of sedimentary basins
  • 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
  • References
  • 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
  • References
  • 2
  • Case studies
  • 5
  • Siliciclastic sequence stratigraphy and basin fill dynamic
  • 5.1
  • Lower Cretaceous depositional evolution from lacustrine to fluvial environment of an intracontinental depress ...
  • 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
  • References
  • 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
  • References
  • 5.3
  • Evolution of depositional sequences in response to tectonism, sea-level change, and sediment supply on the no ...
  • 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
  • References
  • 5.4
  • Changes of the Oligocene to Quaternary deltaic depositional architecture from inner-shelf to shelf-margin, th ...
  • 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
  • References
  • 5.5
  • Sedimentary pattern and filling process in the central canyon: A case study in the eastern Lingshui depressio ...
  • 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.

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