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Deep marine systems : processes, deposits, environments, tectonics and sedimentation / Kevin T. Pickering & Richard N. Hiscott ; with contribution from Thomas Heard.
- Format:
- Book
- Author/Creator:
- Pickering, K. T. (Kevin T.), author.
- Hiscott, Richard N., author.
- Series:
- Wiley Works
- Language:
- English
- Subjects (All):
- Marine sediments.
- Plate tectonics.
- Physical Description:
- 1 online resource (1393 p.)
- Edition:
- First edition.
- Place of Publication:
- West Sussex, England : Wiley : American Geophysical Union, 2016.
- Language Note:
- English
- Summary:
- Deep-water (below wave base) processes, although generally hidden from view, shape the sedimentary record of more than 65% of the Earth's surface, including large parts of ancient mountain belts. This book aims to inform advanced-level undergraduate and postgraduate students, and professional Earth scientists with interests in physical oceanography and hydrocarbon exploration and production, about many of the important physical aspects of deep-water (mainly deep-marine) systems. The authors consider transport and deposition in the deep sea, trace-fossil assemblages, and facies stacking patterns as an archive of the underlying controls on deposit architecture (e.g., seismicity, climate change, autocyclicity). Topics include modern and ancient deep-water sedimentary environments, tectonic settings, and how basinal and extra-basinal processes generate the typical characteristics of basin slopes, submarine canyons, contourite mounds and drifts, submarine fans, basin floors and abyssal plains.
- Contents:
- Intro
- Title Page
- Copyright
- Table of Contents
- Preface
- About the companion website
- Part 1: Process and product
- Chapter One: Physical and biological processes
- 1.1 Introduction
- 1.2 Shelf-edge processes
- 1.3 Deep, thermohaline, clear-water currents
- 1.4 Density currents and sediment gravity flows
- 1.5 Turbidity currents and turbidites
- 1.6 Concentrated density flows and their deposits
- 1.7 Inflated sandflows and their deposits
- 1.8 Cohesive flows and their deposits
- 1.9 Accumulation of biogenic skeletons and organic matter
- 1.10 Summary
- Chapter Two: Sediments (facies)
- 2.1 Introduction
- 2.2 Facies classifications
- 2.3 Facies Class A: Gravels, muddy gravels, gravelly muds, pebbly sands, ≥5% gravel grade
- 2.4 Facies Class B: Sands, >
- 80% sand grade, <
- 5% pebble grade
- 2.5 Facies Class C: Sand-mud couplets and muddy sands, 20-80% sand grade, <
- 80% mud grade (mostly silt)
- 2.6 Facies Class D: Silts, silty muds, and silt-mud couplets, >
- 80% mud, ≥40% silt, 0-20% sand
- 2.7 Facies Class E: ≥95% mud grade, <
- 40% silt grade, <
- 5% sand and coarser grade, <
- 25% biogenics
- 2.8 Facies Class F: Chaotic deposits
- 2.9 Facies Class G: Biogenic oozes (>
- 75% biogenics), muddy oozes (50-75% biogenics), biogenic muds (25-50% biogenics) and chemogenic sediments, <
- 5% terrigenous sand and gravel
- 2.10 Injectites (clastic dykes and sills) (Figs 2.46-2.50)
- 2.11 Facies associations
- Chapter Three: Deep-water ichnology
- 3.1 Introduction
- 3.2 General principles of ichnology
- 3.3 Colonisation of SGF deposits: Opportunistic and equilibrium ecology
- 3.4 Ichnofacies
- 3.5 Ichnofabrics
- 3.6 Trace fossils in core
- 3.7 Case study I: Trace fossils as diagnostic indicators of deep-marine environments, Middle Eocene Ainsa-Jaca basins, Spanish Pyrenees.
- 3.8 Case study II: Subsurface ichnological characterisation of the Middle Eocene Ainsa deep-marine system, Spanish Pyrenees
- 3.9 Summary of ichnology studies in deep-water systems
- 3.10 Concluding remarks
- Chapter Four: Time-space integration
- 4.1 Introduction
- 4.2 Submarine fan growth phases and sequence stratigraphy
- 4.3 Tectono-thermal/glacio-eustatic controls at evolving passive continental margins
- 4.4 Eustatic sea-level changes at active plate margins
- 4.5 Changing relative base level and sediment delivery processes
- 4.6 Autocyclic processes
- 4.7 Palaeo-seismicity and the stratigraphic record
- 4.8 Deconvolving tectonic and climatic controls on depositional sequences in tectonically active basins: Case study from the Eocene, Spanish Pyrenees
- 4.9 Problems in determining controls on sediment delivery
- 4.10 Carbonate versus siliciclastic systems
- 4.11 Computer simulations of deep-water stratigraphy
- 4.12 Laboratory simulations of deep-water stratigraphy
- 4.13 Supercritical versus subcritical fans
- 4.14 Hierarchical classification of depositional units
- 4.15 Concluding comments
- Chapter Five: Statistical properties of sediment gravity flow (SGF) deposits
- 5.1 Introduction
- 5.2 Cloridorme Formation, Middle Ordovician, Québec
- 5.3 Vertical trends
- Part 2: Systems
- Chapter Six: Sediment drifts and abyssal sediment waves
- 6.1 Introduction
- 6.2 Distribution and character of contourites and sediment drifts, North Atlantic Ocean
- 6.3 Facies of muddy and sandy contourites
- 6.4 Seismic facies of contourites
- 6.5 The debate concerning bottom-current reworking of sandy fan sediments
- 6.6 Ancient contourites
- 6.7 Facies model for sediment drifts
- Chapter Seven: Submarine fans and related depositional systems: modern
- 7.1 Introduction
- 7.2 Major controls on submarine fans.
- 7.3 Submarine canyons
- 7.4 Architectural elements of submarine-fan systems
- 7.5 The distribution of architectural elements in modern submarine fans
- 7.6 Modern non-fan dispersal systems
- 7.7 Concluding remarks
- Chapter Eight: Submarine fans and related depositional systems: ancient
- 8.1 Introduction
- 8.2 Ancient submarine canyons
- 8.3 Ancient submarine channels
- 8.4 Comparing modern and ancient channels
- 8.5 Ancient lobe, lobe-fringe, fan-fringe and distal basin-floor deposits
- 8.6 Seafloor topography and onlaps
- 8.7 Scours
- 8.8 Basin-floor sheet-like systems
- 8.9 Prodeltaic clastic ramps
- 8.10 Concluding remarks
- Chapter Nine: Evolving and mature extensional systems
- 9.1 Introduction
- 9.2 Models for lithospheric extension
- 9.3 Subsidence and deep-water facies of rifts and young passive margins
- 9.4 The post-breakup architecture of passive margins
- 9.5 Failed rift systems
- 9.6 Fragments of ancient passive margins
- 9.7 Concluding remarks
- Part 3: Plate tectonics and sedimentation
- Chapter Ten: Subduction margins
- 10.1 Introduction
- 10.2 Modern subduction factories
- 10.3 Arc-arc collision zones
- 10.4 Forearc summary model
- 10.5 Marginal/backarc basins
- 10.6 Ancient convergent-margin systems
- 10.7 Forearc/backarc cycles
- 10.8 Concluding remarks
- Chapter Eleven: Foreland basins
- 11.1 Introduction
- 11.2 Modern foreland basins
- 11.3 Ancient deep-marine foreland basins
- 11.4 Concluding remarks
- Chapter Twelve: Strike-slip continental margin basins
- 12.1 Introduction
- 12.2 Kinematic models for strike-slip basins
- 12.3 Suspect terranes
- 12.4 Depositional models for strike-slip basins
- 12.5 Modern strike-slip mobile zones
- 12.6 Ancient deep-marine oblique-slip mobile zones
- 12.7 Concluding remarks
- References
- Index
- End User License Agreement.
- Notes:
- "This work is a co-publication between the American Geophysical Union and Wiley"--Cover.
- Includes bibliographical references and index.
- Description based on print version record.
- ISBN:
- 9781118865415
- 1118865413
- 9781118865422
- 1118865421
- 9781118865484
- 1118865480
- OCLC:
- 908192785
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