Dynamics of Complex Intracontinental Basins The Central European Basin System 1st Edition by Ralf Littke, Ulf Bayer, Dirk Gajewski ISBN 366251835X 9783662518359 by Littke R., Bayer U., Et Al. (eds.) 3540850847 instant download after payment.

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ISBN 10: 366251835X 
ISBN 13: 9783662518359
Author: Ralf Littke, Ulf Bayer, Dirk Gajewski

Sedimentary basins host, among others, most of our energy and fresh-water resources: they can be regarded as large geo-reactors in which many physical and chemical processes interact. Their complexity can only be well understood in well-organized interdisciplinary co-operations. This book documents how researchers from different geo-scientific disciplines have jointly analysed the structural, thermal, and sedimentary evolution as well as fluid dynamics of a complex sedimentary basin system which has experienced a variety of activation and reactivation impulses as well as intense salt tectonics. In this book we have summarized our geological, geophysical and geochemical understanding of some of the most important processes affecting sedimentary basins in general and our view on the evolution of one of the largest, best explored and most complex continental sedimentary basins on Earth: The Central European Basin System.

Dynamics of Complex Intracontinental Basins The Central European Basin System 1st Table of contents:

Chapter 1 Characteristics of complexintracontinental sedimentary basins
Characteristics of complex intracontinentalsedimentary basins
1.1 Introduction
1.2 Classifications of basincomplexity
1.2.1 Tectonic processes –The plate tectonics approach
1.2.2 Crustal association–The strain localization approach
1.2.3 Sedimentary systems –The sedimentology approach
1.2.4 Fluid and mineral inventory –The diagenetic and/or petroleumsystem approach
1.3 Summary
Chapter 2 The Central European Basin System –an Overview
The Central European Basin System –an Overview
2.1 Introduction
2.2 Crustal association
2.3 Permian Basin formation andsubsequent subsidence
2.4 Subsequent formation ofsub-basins
2.5 Sedimentary history
2.6 Fluids within the CEBS
2.7. The CEBS – prototypeof a complex sedimentary basin
Chapter 3 Strain and temperature in space and time
Driving mechanisms for basin formationand evolution
3.1.1 Driving mechanisms for basinevolution
3.1.2 Kinematic models for basinformation
3.1.2.1 Purely thermal models
3.1.2.2 McKenzie’s kinematic model
3.1.2.3 Limitations of the McKenzie’smodel and correspondingimplementations
3.1.2.4 Non-uniform stretching models:discontinuous and continuousstretching with depth
3.1.2.5 Simple shear model of Wernicke
3.1.2.6 Asymmetrical stretching of thecrust
3.1.2.7 The role of intra-plate stresses:uplift and basin formation incompression
3.1.3 Rheological models
3.1.3.1 The role of rheology on the modesof continental deformation
3.1.3.2 Limitations of a kinematicapproach to continental deformation
3.1.3.3 Dynamic models forbasin formation and evolution
3.1.4 Modelling complex basins
Crustal structures and propertiesin the Central European Basin systemfrom geophysical evidence
3.2.1 Introduction
3.2.2 Structural inventory andphysical properties fromseismic observations
3.2.2.1 Overview
3.2.2.2 Detailed structural architecture andtectonic history from reflectionseismics
3.2.2.3 Crustal properties observed byseismic refractions and wide-anglereflections
3.2.2.4 Lithospheric features fromteleseismic investigations:Tomography and receiver functions
3.2.3 Conductive layers and bodiesfrom magnetotelluricobservations
3.2.4 Rock properties and densitystructure from potentialfield investigations
3.2.5 Summary
Strain and Stress
3.3.1 Introduction
3.3.2 Structural framework of theCEBS
3.3.3 Structural analysisand quantification of strain
3.3.3.1 Reactivation of extensionalstructures: detailed 3D studyaround the western Allertal faultzon
3.3.3.2 Large basement reverse faults andassociated thin-skinned thrusting:the Flechtingen High and
3.3.4 Stress history
3.3.4.1 Palaeostress analysis fromoutcrop and seismic data
3.3.4.2 Neotectonics, seismicity andpresent-day stress state
3.3.5 The CEBS´s structural evolution
Subsidence, inversion and evolution of thethermal field
3.4.1 Introduction
3.4.2 The CEBS as exampleof regional subsidence models
3.4.2.1 Late Carboniferous-Early Permian
3.4.2.2 Late Permian to Early Cretaceous
3.4.2.3 Late Cretaceous
3.4.2.4 Cenozoic
3.4.2.5 Summary
3.4.3 Temperature in sedimentarybasins
3.4.4 Maturity and temperature parametersin sedimentary basins
3.4.5 Variability of palaeotemperaturefields in the Central EuropeanBasin System
Chapter 4 Basin fill
Depositional history and sedimentarycycles in the Central European Basin System
4.1.1 Palaeoclimate, Palaeogeography,and Palaeoenvironment
4.1.2 Sedimentary cycles
4.1.2.1 Depositional cycle 1:Altmark (latest Carboniferous toEarly Permian)
4.1.2.2 Depositional cycle 2:Müritz (Early Permian)
4.1.2.3 Depositional cycle 3:Havel (Middle Permian)
4.1.2.4 Depositional cycle 4: Elbe, Zechstein,Lower and Middle Buntsandsteinparts (Late Permian toEa
4.1.2.5 Depositional cycle 5: Middle Buntsandsteinpart (Early Triassic) toMiddle Keuper part (Carnia
4.1.2.6 Depositional cycle 6:Middle Keuper (Norian) to Dogger(Bajocian)
4.1.2.7 Depositional cycle 7:Dogger (Bajocian) to LowerCretaceous (Berriasian)
4.1.2.8 Depositional cycle 8: Cretaceous
4.1.2.9 Depositional cycle 9:Tertiary (Palaeogene, Neogene)
4.1.3 Provenance of sediments in theCentral European Basin
Basin initiation: Volcanism and sedimentation
4.2.1 Late Palaeozoic basinsin central Europe –distribution, volcanic activityand magmagenetic asp
4.2.2 Data base, distributionand volumes of Late Palaeozoicvolcanics in the CEBS
4.2.3 Stratigraphy and geochronologyof volcanic successions in theSPB
4.2.4 Volcanic facies in the SPB
4.2.5 Syn- to postvolcanic sedimentationduring the Lower Rotliegendand Upper Rotliegend I
4.2.6 Landscape evolution during theinitial phase of the SPB
Upper Rotliegend to Early Cretaceous basindevelopment
4.3.1 Introduction
4.3.2 Upper Rotliegend II
4.3.3 Zechstein
4.3.4 Buntsandstein
4.3.5 Muschelkalk
4.3.6 Keuper
4.3.7 Jurassic
4.3.8 Early Cretaceous
Sedimentation during basin inversion
4.4.1 Introduction
4.4.2 Basin Formation
4.4.2.1 Flexural marginal troughs
4.4.2.2 Flexural (thrust load) basins
4.4.2.3 Half ramp (piggy back) basins
4.4.2.4 Basins due to basement folding
4.4.2.5 Rim synclines and collapse basins
4.4.3 Effects of basin inversion ondeposition
4.4.3.1 General remarks
4.4.3.2 Swells and troughs –condensation and thicknessenhancement
4.4.3.3 Clastic deposition – the result ofuplift and erosion
4.4.3.4 Ironstones and phosphoritesaround inversion structures anddiapirs
4.4.4 Sedimentation during inversionin the Central European Basin
4.4.4.1 Basins related to inverted grabenstructures– the Münsterland Basin
4.4.4.2 Basin evolution in front of abasement thrust:The Harz example
4.4.5 The North German Basinduring the Tertiary
Glaciation, salt and the present landscape
4.5.1 Introduction
4.5.2 Modern topography and glacialisostasy
4.5.3 Crustal movements, seismicityand landscape formation
4.5.3.1 Regional and case studies
Chapter 5 Salt dynamics
Salt as sediment in the Central European Basinsystem as seen from a deep time perspective
5.1.1 Introduction
5.1.2 Mother brines: isochemicalsystems?
5.1.3 Evaporite sedimentsand climate
5.1.4 Evaporites volumesin deep time
5.1.5 Evaporite volumes & tectonics?
5.1.6 Episodic halokinesis
Flow and Transport Properties of Salt Rocks
5.2.1 Introduction
5.2.2 Physical propertiesof evaporites
5.2.3 Deformation mechanismsand rheology of halite inexperiments
5.2.3.1 Deformation mechanisms andassociated processes
5.2.3.2 Rheological behaviour –“flow laws”
5.2.4 Deformation mechanismsand rheology of carnallite andbischofite
5.2.5 Natural laboratories
5.2.5.1 Evidence for diffuse dilatancy andfluid flow in rock salt in the deepsubsurface
5.2.5.2 Fluid Flow in Fractures:A case study of the Neuhof MineGermany
5.2.5.3 Deformation mechanisms inweakly deformed bedded salt inHengelo, the Netherlands
5.2.5.4 Deformation mechanisms in saltdomes
5.2.5.5 Salt glaciers
5.2.6 Discussion and outlook
Dynamics of salt structures
5.3.1 Introduction
5.3.2 Concepts of salt tectonics
5.3.3 Salt geometries and kinematics– a case study
5.3.3.1 Subsurface geometries fromseismic interpretation
5.3.3.2 Salt tectonic evolution basedon retro-deformation
5.3.3.3 First phase of salt movement:Zechstein to Middle Keuper
5.3.3.4 Second phase of salt movement:Middle Keuper to Top Jurassic
5.3.3.5 Third phase of salt movement:Early Cretaceous to recent
5.3.4 Salt sediment interaction
5.3.5 Multiphase salt dynamics in theCEBS
Dynamics of salt basins
5.4.1 Introduction
5.4.2 Regional pattern of saltstructures in the CEBS
5.4.3 History of salt movementsin the CEBS
5.4.3.1 Salt movements in relationto Mid-Late Triassic regionalextension
5.4.3.2 The salt during Jurassic-EarlyCretaceous basin differentiation
5.4.3.3 Salt movements during LateCretaceous-Early Tertiarycompression
5.4.3.4 Salt movements in relation toLate Tertiary regional extension
5.4.4 Case Study Glückstadt Graben
5.4.4.1 Structural features of theGlückstadt Graben
5.4.4.2 3D reconstruction ofsalt movements
5.4.4.3 Salt movements in relation totectonic events
5.4.5 Case Study NE German Basin
5.4.6. Case Study SW Baltic Sea
5.4.7 General findings forsalt-containingintra-continental basins
Temperature fields, petroleum maturationand fluid flow in the vicinity of salt domes
5.5.1 Introduction
5.5.2 Impact of salt structures ontemperature field and oilmaturation
5.5.2.1 General Concept
5.5.2.2 The example of the Büsum saltdiapir
5.5.3 Fluid flow in salt
5.5.4 Impact of salt structures ongroundwater transportprocesses within sedimentarybasins
5.5.4.1 Brief description of driving forcesin large-scale groundwater flowsystems
5.5.4.2 Example: Gulf Coast region of theUnited States
5.5.4.3 Numerical example of thermallyinducedflow in relation to saltdome environment (includingchem
Chapter 6 Fluid systems
Fluids in sedimentary basins: an overview
6.1.1 Relevance of geofluids
6.1.2 Definitions
6.1.3 Subsurface aqueous fluids
6.1.3.1 Introduction
6.1.3.2 Types of fluids
6.1.3.3 Present-day fluids in the NGB
6.1.4 Petroleum fluids
Transport processes
6.2.1 Introduction
6.2.2 Physical mechanismsand concepts
6.2.2.1 Overview
6.2.2.2 Porosity
6.2.2.3 Permeability
6.2.2.4 Permeability-porosityrelationships
6.2.3 Fault seals and top seals
6.2.3.1 Overview
6.2.3.2 Micro- and macroscale processes
6.2.3.3 Application to fluid-rock systems
6.2.3.4 (Hydro) fractured seal
6.2.3.5 Brittle and Ductile Seals
6.2.3.6 Fault Seals
6.2.3.7 Numerical modelling of petroleumflow
6.2.4 Geological aspects of fluidtransport
6.2.4.1 Fluid flow regimes
Fluid-rock interactions
6.3.1 Introduction
6.3.2 Evolution of deep brines
6.3.2.1 Origin of saline brines
6.3.2.2 Fluid-rock interactions modifyingthe composition of brines
6.3.3 Palaeo-fluid reconstruction
6.3.3.1 Methods of palaeo-fluidreconstruction
6.3.3.2 Synthesis of fluid evolution in thePermian Rotliegend of the NorthGerman Basin
6.3.4 Organic-inorganic interactions
6.3.5 Modelling fluid-rock interactions
6.3.6 Geological applications
Petroleum systems
6.4.1 Concepts of petroleum systemmodelling
6.4.2 Petroleum Source Rocks
6.4.3 Shallow and microbial gas
6.4.4 Sources of deep gas
6.4.5 Petroleum alteration -biodegradation
6.4.6 Overpressured reservoirs
6.4.7 Effects of glaciation onpetroleum systems
Origin and distribution of non-hydrocarbongases
6.5.1 Introduction
6.5.2 Nitrogen
6.5.2.1 Nitrogen geochemistry and thenitrogen cycle
6.5.2.2 Nitrogen in the NGB
6.5.2.3 Mechanisms and conditions ofnitrogen release
6.5.2.4 Summary
6.5.3 Carbon dioxide
6.5.3.1 CO2–rich natural gases in theCEBS
6.5.3.2 Origins of CO2 in Ca2 reservoirrocks
6.5.3.3 Summary
6.5.4 Hydrogen sulfide (H2S)
6.5.4.1 Overview
6.5.4.2 Microbial and thermochemicalsulfate reduction
6.5.4.3 Important reaction steps
6.5.4.4 Common Products in NaturalEnvironments
6.5.4.5 Temperature ranges and reactionkinetics of BSR and TSR
6.5.4.6 Heat released
6.5.4.7 Distinguishing between BSR andTSR
6.5.4.8 H2S-rich gases in theNorth German Basin
6.5.5 Evidence from vein mineralisationand fluid inclusions

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