did-you-know? rent-now

Amazon no longer offers textbook rentals. We do!

did-you-know? rent-now

Amazon no longer offers textbook rentals. We do!

We're the #1 textbook rental company. Let us show you why.

9780632049769

Sedimentology and Sedimentary Basins: From Turbulence to Tectonics

by
  • ISBN13:

    9780632049769

  • ISBN10:

    0632049766

  • Format: Paperback
  • Copyright: 1999-09-01
  • Publisher: Wiley-Blackwell
  • Purchase Benefits
  • Free Shipping Icon Free Shipping On Orders Over $35!
    Your order must be $35 or more to qualify for free economy shipping. Bulk sales, PO's, Marketplace items, eBooks and apparel do not qualify for this offer.
  • eCampus.com Logo Get Rewarded for Ordering Your Textbooks! Enroll Now
List Price: $119.95

Summary

Sedimentology is a core discipline of earth and environmental sciences. It enquires the origins, transport and deposition of mineral sediment on the Earth's surface. The subject is a link between positive effects arising from the building of relief by tectonics and the negative action of denudation in drainage catchments and tectonic subsidence in sedimentary basins.The author addresses the principles of the subject, emphasising the advantages of a general science approach and the importance of understanding modern processes. Sedimentology and Sedimentary Basins is not an encyclopaedia, but attempts to stimulate interdisciplinary thought across the whole subject area and related disciplines. The book has been designed to meet the needs of earth and environmental science undergraduates.Mike Leeder is currently at the School of Environmental Sciences, University of East Anglia, Norwich. Previously, he was at the School of Earth Sciences, University of Leeds. Mike believes that the first step in sedimentological problem-solving comes from field observations, the second step comes from a grasp of basic physics or chemistry, and the third step comes from the application of simple mathematics. The second edition of a well-established and very successful text. A core course in all earth science degree programmes. Features colour plates and boxed explanations of difficult derivations.

Table of Contents

Preface xiii
Acknowledgements xv
Part 1: Introduction
Sedimentology in the earth sciences
3(12)
Introduction: sedimentology and earth cycling
3(4)
Erosional drainage basins and depositional sedimentary basins
7(1)
Global sediment discharge and earth recycling: the rock cycle
7(2)
Comparative interplanetary sedimentology
9(1)
Practical sedimentology
10(1)
A brief history of sedimentology
11(4)
Part 2: Origin and Types of Sediment Grains
Water--rock interactions: chemical and physical breakdown of catchment bedrock to soil and clastic sediment grains
15(28)
Introduction
15(1)
Natural waters as proton donors: pH, acid hydrolysis and limestone weathering
16(4)
Metallic ions, electron transfer and Eh--pH diagrams
20(1)
Behaviour of silicate minerals during chemical weathering: breakdown products and newly formed minerals
21(8)
Acid rain and whole-catchment studies of chemical weathering
29(1)
The rates and mechanisms of chemical weathering
29(5)
A simple index of chemical alteration (CIA)
34(2)
Vegetation, chemical weathering and the Precambrian controversy
36(2)
Physical weathering
38(1)
Soils valves and filters for the natural landscape
39(4)
The inorganic and organic precipitation of sediment: chemical biochemical and biological
43(34)
Marine and freshwater chemical composition: chemical fluxes to and from the oceans
43(1)
The carbonate system in the oceans
44(4)
Advances in understanding carbonate reaction kinetics and their significance
48(3)
Pre-Recent and future CaCO3 reactions
51(1)
Ooids
52(4)
Carbonate grains from plants and animals
56(3)
Carbonate muds, oozes and chalks
59(1)
Other carbonate grains of biological origins
60(1)
Organic productivity, sea-level and atmospheric controls of biogenic CaCO3 deposition rates
61(1)
CaCO3 dissolution in the deep ocean and the oceanic CaCO3 compensation mechanism
61(3)
Evaporite salts and their inorganic precipitation
64(5)
Silica and pelagic plankton
69(2)
Iron minerals and biomineralizers
71(2)
Phosphates
73(4)
Part 3: User's Guide to Sedimentological Fluid Dynamics
Back to basics: fluid flow in general
77(24)
Introduction
77(1)
Material properties of fluids
77(7)
Plastic behaviour
84(1)
Dimensionless numbers
85(1)
Reference frames for flows
85(1)
The concepts of flow steadiness and uniformity
86(3)
Visualization of flow patterns
89(1)
Ideal (potential) flow
90(7)
Dynamics of fluid motion
97(1)
Strategies for coping with the dynamic equations
97(4)
Flow in the real world: laminar and turbulent behaviour
101(22)
Osborne Reynolds and types of flow
101(4)
The distribution of velocity in viscous flows: the boundary layer
105(1)
Turbulent flow
106(4)
The distribution of velocity in turbulent flows
110(1)
Shear velocity, bed roughness, bed shear stress and flow power
110(5)
The periodic coherent structures of turbulent shear flows
115(4)
Shear flow instabilities, flow separation and secondary currents
119(4)
Sediment grains in fluids: settling, transport and feedback
123(22)
Introduction
123(1)
Fall of grains through stationary fluids
123(3)
Natural flows carrying particulate material are complex
126(1)
Fluids as transporting machines
126(1)
Initiation of particle motion
127(4)
Initiation of motion by air flow
131(1)
Paths of grain motion
131(4)
Solid transmitted stresses
135(2)
A dynamic sediment suspension theory
137(3)
A warning: nonequilibrium effects may dominate natural sediment transport systems
140(1)
Steady state, deposition or erosion: the sediment continuity equation
140(5)
Part 4: Sediment Transport and Sedimentary Structures
Bedforms and structures formed by unidirectional water flows over granular sediment
145(16)
The `trinity' of flow, transport and bedform
145(1)
Current ripples
145(5)
Lower-stage plane beds and cluster bedforms
150(1)
Duniods (bars, 2D dunes)
150(1)
Dunes
150(4)
Upper-stage plane beds
154(1)
Antidunes, transverse ribs, chutes and pools, and related forms
155(1)
Bedforms and sediment transport in poorly sorted sediment
155(1)
Bedform phase diagrams
156(1)
Bedform `lag' effects
157(1)
Bedform theory
157(2)
Measurement of palaeocurrents and problems arising from trough-shaped sets of cross-stratification
159(2)
Bedforms and structures formed by atmospheric flows
161(15)
Introduction: some contrasts between air and water flows
161(3)
Aeolian bedforms in general
164(1)
Ballistic ripples and ridges
165(3)
Dunes in general
168(1)
Flow-transverse dunes
168(3)
Flow-parallel dunes
171(2)
Complex flow dunes
173(1)
Vegetated parabolic dunes
173(3)
Oscillatory water waves, combined flows and tides: their bedforms and structures
176(18)
Introduction
176(1)
Simple wave theory
177(5)
Near-bed flow and bedforms
182(3)
Combined flows, wave--current ripples and hummocky cross-stratification
185(3)
Tidal flows
188(6)
Bedforms and cohesive sediment transport and erosion
194(7)
The `special' case of clays and cohesive beds
194(2)
Flow erosion of cohesive beds
196(4)
Erosion by `tools'
200(1)
Sediment gravity flows and their deposits
201(25)
Introduction and static grain aggregates
201(1)
Static friction and stability of granular masses
202(2)
Grain flow avalanches: from cross-bedding to megabreccias
204(4)
Debris flows
208(7)
Turbidity flows
215(11)
Liquefaction, liquefaction structures and other `soft' sediment deformation structures
226(11)
Liquefaction
226(2)
Sedimentary structures formed by and during liquefaction
228(4)
Submarine landslides, growth faults and slumps
232(2)
Desiccation and synaeresis shrinkage structures
234(3)
Part 5: External Controls on Sediment Derivation, Transport and Deposition
Climate and sedimentary processes
237(21)
Introduction: climate as a fundamental variable in sedimentology
237(1)
Solar radiation: ultimate fuel for the climate machine
238(1)
Earth's reradiation and the `greenhouse' concept
238(3)
Radiation balance, heat transfer and simple climatic models
241(2)
Climate and the water cycle
243(2)
General atmospheric circulations
245(3)
Global climates: a summary
248(4)
Climate change
252(4)
Sedimentological evidence for palaeoclimate
256(2)
Changing sea level and sedimentary sequences
258(9)
Introduction: sea level as datum
258(1)
Sea-level changes
258(1)
Rates and magnitude of sea-level change
259(1)
Origins of global sea-level change: slow vs. fast eustasy
260(3)
Sequence stratigraphy: layers, cheesewires and bandwagons
263(4)
Tectonics, denudation rates and sediment yields
267(28)
Basic geodynamics of uplift
267(1)
Elevation and gradients
267(4)
Catchment processes
271(2)
Erosion and denudation
273(1)
Large-scale studies of denudation rates
274(4)
Basinal studies of denudation and sediment flux: the inverse approach
278(3)
Sediment supply, vegetation and climate change: implications for basin stratigraphy
281(7)
Marine strontium isotope ratio and continental erosion rates
288(7)
Part 6: Sediment Deposition, Environments and Facies in Continental Environments
Aeolian sediments in low-latitude deserts
295(12)
Introduction
295(1)
Physical processes and erg formation
295(5)
Modern desert bedform associations and facies
300(1)
Aeolian architecture
301(1)
Climate change, erg abandonment and desert--lake--river sedimentary cycles
302(2)
Ancient desert facies
304(3)
Rivers
307(23)
Introduction
307(1)
Channel magnitude and gradient
307(3)
Channel form
310(1)
Channel sediment transport processes, bedforms and internal structures
311(9)
The floodplain
320(2)
Channel belts, alluvial ridges, combing and avulsion
322(2)
River channel changes, adjustable variables and equilibrium
324(2)
The many causes of channel incision--aggradation cycles
326(2)
Fluvial architecture: scale, controls and time
328(1)
Fluvial deposits in the geological record
328(2)
Alluvial fans and fan deltas
330(10)
Introduction
330(1)
Controls on the size (area) of fans
330(3)
Physical processes on alluvial fans
333(1)
Debris-flow-dominated alluvial fans
334(1)
Stream-flow-dominated alluvial fans
334(1)
Recognition of ancient alluvial fans
335(2)
Fan deltas
337(3)
Lakes
340(17)
Introduction
340(1)
Lake stratification
341(2)
Clastic input by rivers and the effect of turbidity currents
343(1)
Wind-forced physical processes
343(1)
Chemical processes and cycles
344(3)
Biological processes and cycles
347(1)
Modern temperate lakes and their sedimentary facies
347(1)
Lakes in the East African rifts
348(3)
Lake Baikal
351(1)
Shallow saline lakes
351(1)
The succession of facies as lakes evolve
352(3)
Ancient lake facies
355(2)
Ice
357(14)
Introduction
357(1)
Physical processes of ice flow
358(1)
Glacier flow and surges
358(2)
Sediment transport, erosion and deposition by flowing ice
360(2)
Glacigenic sediment: nomenclature and classification
362(1)
Quaternary and modern glacial environments and facies
363(1)
Ice-produced glacigenic facies and the periglacial realm
363(1)
Glaciofluvial processes at and within the ice front
364(1)
Glacimarine environments
365(1)
Glacilacustrine environments
366(1)
Glacial facies in the pre-Quaternary geological record
366(5)
Part 7: Sediment Deposition, Environments and Facies in Marine Environments
Estuaries
371(12)
Introduction
371(1)
Estuarine dynamics
372(6)
Modern estuarine facies
378(3)
Estuaries and sequence stratigraphy
381(1)
Ancient estuarine facies
381(2)
River deltas
383(15)
Introduction
383(1)
Physical processes
384(5)
Mass movements and slope failure on the subaqueous delta
389(1)
Organic deposition in deltas
390(1)
Delta case histories
390(8)
`Linear' clastic shorelines
398(16)
Introduction
398(2)
Physical processes on linear coasts
400(4)
Beach dynamics and sedimentation
404(2)
Barrier--inlet systems and their deposits
406(5)
Tidal flats and chenier ridges
411(2)
Ancient clastic shoreline facies
413(1)
Carbonate-evaporite shorelines shelves and basins
414(30)
Introduction: carbonate `factories' and their consequences
414(4)
Arid carbonate tidal flats and evaporite sabkhas
418(3)
Humid carbonate tidal flats and marshes
421(4)
Shorefaces, lagoons and bays
425(2)
Enhanced-salinity bays and embayments
427(1)
Tidal delta and margin-spillover carbonate tidal sands
427(1)
Open carbonate shelf ramps
428(1)
Platform margin reefs and carbonate build-ups generally
429(7)
Platform margin slopes and basins
436(3)
Carbonate sediments, cycles, sequences and sea-level changes
439(1)
Destruction of carbonate environments: siliciclastic input and eutrophication
440(1)
Subaqueous evaporites
441(3)
Shelves
444(21)
Introduction
444(1)
Shelf water dynamics: general
445(1)
Shelf tides
446(4)
Wind drift currents
450(2)
Storm set-up and wind-forced geostrophic currents
452(1)
Shelf density currents
453(2)
Across-shelf transport
455(1)
Recent shelf facies
455(8)
Ancient clastic shelf facies
463(2)
Oceanic processes and sediments
465(32)
Introduction
465(1)
Physical oceanic processes: general
465(2)
Surface oceanic currents and circulation
467(3)
Oceanic deep currents and circulation
470(3)
Sculpturing and resedimentation: canyons, slides, slumps and debris flows
473(4)
Submarine fans
477(7)
Biological and chemical oceanic processes
484(2)
Pelagic oceanic sediments
486(1)
Palaeo-oceanography of modern oceans
487(4)
Anoxic events of seas and oceans
491(1)
Hypersaline oceans
492(5)
Part 8: Sedimentology in Sedimentary Basins
Tectonic subsidence and deposition
497(10)
Introduction: basins and basin analysis
497(1)
Preservation of sediment in basins
497(2)
Tectonic subsidence of sedimentary basins: in a nutshell
499(8)
Sedimentology in sedimentary basins: a user's guide
507(24)
Introduction
507(1)
Continental rifts
507(4)
Proto-oceanic rifts
511(2)
Coastal plains, shelf terraces and continental rises
513(2)
Convergent/destructive margin basins: some general comments
515(2)
Subduction zones: trenches and trench-slope basins
517(3)
Fore-arc basins
520(2)
Intra-arc basins
522(1)
Back-arc basins
522(2)
Foreland basins
524(5)
Strike-slip basins
529(2)
References 531(50)
Index 581

Supplemental Materials

What is included with this book?

The New copy of this book will include any supplemental materials advertised. Please check the title of the book to determine if it should include any access cards, study guides, lab manuals, CDs, etc.

The Used, Rental and eBook copies of this book are not guaranteed to include any supplemental materials. Typically, only the book itself is included. This is true even if the title states it includes any access cards, study guides, lab manuals, CDs, etc.

Rewards Program