Physical principles of sedimentary basin analysis:
"This book is based on lecture notes about the physical processes that govern sedimentary basins. The notes were the basis for a one-semester seminar named "Heat and fluid flow in sedimentary basins" offered by UNIK, an affiliate of the University of Oslo at Kjeller. As the title sugg...
Gespeichert in:
| 1. Verfasser: | |
|---|---|
| Format: | Buch |
| Sprache: | English |
| Veröffentlicht: |
Cambridge [u.a.]
Cambridge Univ. Press
2010
|
| Ausgabe: | 1. publ. |
| Schlagworte: | |
| Online-Zugang: | Inhaltsverzeichnis |
| Zusammenfassung: | "This book is based on lecture notes about the physical processes that govern sedimentary basins. The notes were the basis for a one-semester seminar named "Heat and fluid flow in sedimentary basins" offered by UNIK, an affiliate of the University of Oslo at Kjeller. As the title suggests, this book is about the physical principles of processes in sedimentary basins like for instance heat and fluid flow. The subject is approached by deriving the basic equations from fundamental principles like mass and energy conservation. The equations are then solved for simple problems that give insight into the processes.It should be possible to reproduce most of the solutions, calculations and plots presented in the book with a modest effort and a minimum of computer facilities"--Provided by publisher "Presenting a rigorous treatment of the physical and mechanical basis for the modelling of sedimentary basins, this book supplies geoscientists with practical tools for creating their own models. It begins with a thorough grounding in properties of porous media, linear elasticity, continuum mechanics and rock compressibility. Chapters on heat flow, subsidence, rheology, flexure and gravity consider sedimentary basins in the context of the Earth's lithosphere, and the book concludes with coverage of pore space cementation, compaction and fluid flow. The volume introduces basic, state-of-the-art models and demonstrates how to reproduce results using tools like MATLAB and Octave. Main equations are derived from first principles, and their basic solutions obtained and then applied. Separate notes sections supply more technical details, and the text is illustrated throughout with real-world examples, applications and test exercises. This is an accessible introduction to quantitative modelling of basins for graduate students, researchers and oil industry professionals"--Provided by publisher |
| Beschreibung: | XV, 527 S. Ill., graph. Darst. |
| ISBN: | 9780521761253 |
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| 520 | 3 | |a "Presenting a rigorous treatment of the physical and mechanical basis for the modelling of sedimentary basins, this book supplies geoscientists with practical tools for creating their own models. It begins with a thorough grounding in properties of porous media, linear elasticity, continuum mechanics and rock compressibility. Chapters on heat flow, subsidence, rheology, flexure and gravity consider sedimentary basins in the context of the Earth's lithosphere, and the book concludes with coverage of pore space cementation, compaction and fluid flow. The volume introduces basic, state-of-the-art models and demonstrates how to reproduce results using tools like MATLAB and Octave. Main equations are derived from first principles, and their basic solutions obtained and then applied. Separate notes sections supply more technical details, and the text is illustrated throughout with real-world examples, applications and test exercises. This is an accessible introduction to quantitative modelling of basins for graduate students, researchers and oil industry professionals"--Provided by publisher | |
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Datensatz im Suchindex
| _version_ | 1804141085630398464 |
|---|---|
| adam_text | PHYSICAL PRINCIPLES OF SEDIMENTARY BASIN ANALYSIS MAGNUS WANGEN
INSTITUTE FOR ENERGY TECHNOLOGY, NORWAY CONTENTS PREFACE ACKNOWLEDGMENTS
PRELIMINARIES 1.1 1.2 NOTATION FURTHER READING PROPERTIES OF POROUS
MEDIA 2.1 2.2 2.3 2.4 2.5 2.6 2.7 2.8 2.9 2.10 2.11 2.12 2.13 POROSITY
THE CORRELATION FUNCTION AND SPECIFIC SURFACE THE PENETRABLE GRAIN MODEL
DARCY S LAW POTENTIAL FLOW AND GRAVITY PERMEABILITY AS A FUNCTION OF
POROSITY EMPIRICAL PERMEABILITY RELATIONSHIPS THE ROTATION MATRIX
ANISOTROPIC PERMEABILITY DIRECTIONAL PERMEABILITY AVERAGE PERMEABILITY
FOURIER S LAW AND HEAT CONDUCTIVITY FURTHER READING LINEAR ELASTICITY
AND CONTINUUM MECHANICS 3.1 3.2 3.3 3.4 3.5 3.6 3.7 3.8 3.9 3.10 3.11
HOOKE S LAW, YOUNG S MODULUS AND POISSON S RATIO BULK MODULUS SHEAR
MODULUS STRAIN STRESS ROTATION OF STRESS AND STRAIN PRINCIPAL STRESS
MOHR S CIRCLES STRESS ELLIPSOID DEVIATORIC STRESS LINEAR STRESS-STRAIN
RELATIONS PAGE XM XV 1 1 2 3 3 6 9 12 14 15 18 20 23 25 27 31 37 38 38
38 39 40 43 46 47 51 53 55 56 VIII CONTENTS 3.12 THERMAL STRESS 60 3.13
THERMAL STRESS COMPARED WITH LITHOSTATIC STRESS 60 3.14 BUOYANCY AND
EFFECTIVE STRESS 61 3.15 EFFECTIVE STRESS IN 3D 63 3.16 EULER AND
LAGRANGE COORDINATES 64 3.17 AN IMPORTANT LAGRANGE COORDINATE 67 3.18
CONSERVATION LAWS IN ID 68 3.19 MASS CONSERVATION 69 3.20 MOMENTUM
BALANCE (NEWTON S SECOND LAW) 70 3.21 PARTICLE PATHS AND STREAMLINES 74
3.22 STREAMLINES IN 2D 75 3.23 FURTHER READING 79 4 COMPRESSIBILITY OF
ROCKS AND SEDIMENTS 80 4.1 ROCK COMPRESSIBILITY . 80 4.2 MORE
COMPRESSIBILITIES 84 4.3 COMPRESSIBILITY OF POROSITY AND THE SOLID
VOLUME 86 4.4 EFFECTIVE PRESSURE COEFFICIENTS 88 4.5 COMPACTION OF
SEDIMENTS 88 4.6 GRAVITATIONAL COMPACTION OF A HYDROSTATIC CLAY LAYER 90
4.7 FURTHER READING 93 5 BURIAL HISTORIES 94 5.1 POROSITY AS A FUNCTION
OF NET SEDIMENT THICKNESS 95 5.2 PRE-CALIBRATION OF BURIAL HISTORY
CALCULATIONS 97 5.3 POROSITY AS A FUNCTION OF Z 99 5.4 EROSION 100 5.5
NUMERICAL COMPACTION COMPUTATION 102 5.6 FURTHER READING 104 6 HEAT FLOW
105 6.1 THE TEMPERATURE EQUATION 106 6.2 STATIONARY ID TEMPERATURE
SOLUTIONS 109 6.3 HEAT GENERATION 112 6.4 STATIONARY ID TEMPERATURE
SOLUTIONS WITH HEAT GENERATION 115 6.5 HEAT FLOW AND GEOTHERMS IN STABLE
CONTINENTAL AREAS 122 6.6 STATIONARY GEOTHERMS IN THE LITHOSPHERIC
MANTLE 124 6.7 SEDIMENT MATURITY AND VITRINITE REFLECTANCE 127 6.8
STATIONARY HEAT FLOW IN A SPHERE 132 6.9 TRANSIENT COOLING OF A SPHERE
134 6.10 HEAT FLOW AND SALT DOMES 138 6.11 FORCED CONVECTIVE HEAT
TRANSFER 140 6.12 TRANSIENT CONVECTIVE HEAT FLOW 147 6.13 HEAT FLOW IN
FRACTURES 151 6.14 INSTANTANEOUS HEATING OR COOLING OF SEMI-INFINITE
HALF-SPACE 154 CONTENTS IX 6.15 COOLING SILLS AND DIKES 159 6.16
SOLIDIFICATION AND LATENT HEAT OF FUSION 167 6.17 SOLIDIFICATION OF
SILLS AND DIKES 170 6.18 PERIODIC HEATING OF THE SURFACE 173 6.19
VARIABLE SURFACE TEMPERATURE 177 6.20 TEMPERATURE TRANSIENTS FROM
SEDIMENT DEPOSITION OR EROSION 181 6.21 CONSERVATION OF ENERGY ONCE MORE
186 6.22 MANTLE ADIABAT 191 6.23 FURTHER READING . 193 SUBSIDENCE 194
7.1 ISOSTATIC SUBSIDENCE 194 7.2 THICKNESS OF CRUSTAL ROOTS 198 7.3
SUBSIDENCE FROM EUSTATIC SEA LEVEL CHANGES . 200 7.4 BASIN SUBSIDENCE BY
CRUSTAL THINNING 200 7.5 THE MCKENZIE MODEL OF BASIN SUBSIDENCE 202 7.6
THE THERMAL TRANSIENT OF THE MCKENZIE MODEL 207 7.7 THE SURFACE HEAT
FLOW OF THE MCKENZIE MODEL 211 7.8 THE THERMAL SUBSIDENCE OF THE
MCKENZIE MODEL 213 7.9 LITHOSPHERIC STRETCHING OF FINITE DURATION 215
7.10 FINITE DURATION STRETCHING AND TEMPERATURE 221 7.11 LITHOSPHERIC
EXTENSION, PHASE CHANGES AND SUBSIDENCE/UPLIFT 224 7.12 LITHOSPHERIC
EXTENSION AND DECOMPRESSION MELTING 230 7.13 THERMAL SUBSIDENCE OF THE
OCEANIC LITHOSPHERE 238 7.14 BACKSTRIPPING AND TECTONIC SUBSIDENCE 242
7.15 SUBSIDENCE OF THE VJZTRING MARGIN, NE ATLANTIC 246 7.16 STRETCHING
AND THINNING OF THE SEDIMENTS 252 7.17 FURTHER READING 259 RHEOLOGY:
FRACTURE AND FLOW 260 8.1 FAULTS 260 8.2 FRICTION 260 8.3 STICK-SLIP
FAULTING 263 8.4 THE SLIDER-BLOCK MODEL OF STICK-SLIP MOTION 264 8.5
FRACTURE 268 8.6 HYDROFRACTURING 271 8.7 DUCTILE FLOW AND YIELD STRENGTH
ENVELOPES 273 8.8 FURTHER READING 281 FLEXURE OF THE LITHOSPHERE 282 9.1
EQUATION FOR FLEXURE OF A PLATE 282 9.2 FLEXURE FROM A POINT LOAD 289
9.3 FLEXURE FROM A POINT LOAD ON A BROKEN PLATE 294 9.4 FLEXURE AND
LATERAL VARIATIONS OF THE LOAD 295 X . CONTENTS 9.5 THE DEFLECTION OF A
PLATE UNDER COMPRESSION 298 9.6 DAMPED FLEXURE OF A PLATE ABOVE A
VISCOUS MANTLE 301 9.7 THE EQUATION FOR VISCOELASTIC FLEXURE OF A PLATE
302 9.8 ELASTIC AND VISCOUS DEFORMATIONS 304 9.9 FLEXURE OF A
VISCOELASTIC PLATE 307 9.10 BUCKLING OF A VISCOUS PLATE 310 9.11 FURTHER
READING 315 10 GRAVITY AND GRAVITY ANOMALIES 316 10.1 NEWTON S LAW OF
GRAVITY 316 10.2 POTENTIAL ENERGY AND THE POTENTIAL 321 10.3
CONSERVATIVE FIELDS 323 10.4 GAUSS S LAW 323 10.5 BOUGUER S FORMULA FOR
GRAVITY DUE TO A HORIZONTAL LAYER - 325 10.6 LAPLACE S AND POISSON S
EQUATIONS FOR THE POTENTIAL 327 10.7 GRAVITY FROM A BURIED SPHERE 329
10.8 GRAVITY FROM A HORIZONTAL CYLINDER 330 10.9 GRAVITY FROM A PRISM
WITH RECTANGULAR CROSS-SECTION 332 10.10 GRAVITY FROM A 2D POLYGONAL
BODY 334 10.11 EXCESS MASS CAUSING GRAVITY ANOMALIES 340 10.12 VERTICAL
CONTINUATION OF GRAVITY 341 10.13 REDUCTION OF GRAVITY DATA 344 10.14
GRAVITY AND ISOSTASY OVER CONTINENTS 347 10.15 GRAVITY AND SEA BED
TOPOGRAPHY 356 10.16 FURTHER READING 360 11 QUARTZ CEMENTATION OF
SANDSTONES 361 11.1 INTRODUCTION 361 11.2 QUARTZ KINETICS AND
PRECIPITATION RATES 362 11.3 SURFACE AREA 364 11.4 ISOTHERMAL QUARTZ
CEMENTATION 365 11.5 CALIBRATION OF QUARTZ KINETICS 367 11.6 CEMENTATION
DURING CONSTANT BURIAL 369 11.7 CEMENTATION FOR GENERAL BURIAL HISTORIES
374 11.8 STRAIN RATE 375 11.9 A REACTION-DIFFUSION EQUATION FOR SILICA
377 11.10 THE SILICA CONCENTRATION BETWEEN STYLOLITES 379 11.11 FURTHER
READING 3 84 12 OVERPRESSURE AND COMPACTION: EXACT SOLUTIONS 385 12.1
THE PRESSURE EQUATION IN ID 386 12.2 THE DARCY FLUX CAUSED BY COMPACTION
388 12.3 VOID RATIO AS A FUNCTION OF DEPTH 389 12.4 A SIMPLE MODEL FOR
OVERPRESSURE BUILD-UP 392 CONTENTS XI 12.5 HYDROFRACTURING 397 12.6
GIBSON S SOLUTION FOR OVERPRESSURE 401 12.7 GIBSON S SOLUTION FOR
POROSITY REDUCTION 405 12.8 OVERPRESSURE AND MECHANICAL COMPACTION 407
12.9 THE DIMENSIONLESS GIBSON SOLUTION 412 12.10 FURTHER READING 415 13
FLUID FLOW: BASIC EQUATIONS 417 13.1 CONSERVATION OF SOLID 417 13.2
CONSERVATION OF FLUID 420 13.3 POROELASTIC PRESSURE EQUATION 421 13.4
STORAGE COEFFICIENTS 422 13.5 STRESS, STRAIN AND POROELASTICITY 425 13.6
STRESS CAUSED BY OVERPRESSURE 428 13.7 THE RATE OF CHANGE OF POROSITY .
431 13.8 A GENERAL PRESSURE EQUATION 433 13.9 POTENTIAL FLOW 434 13.10 A
GENERAL EQUATION FOR THE FLUID FLOW POTENTIAL 437 13.11 SIMPLE PRESSURE
EQUATIONS 437 13.12 FURTHER READING 439 14 FLUID FLOW: BASIC EQUATIONS
440 14.1 UNCONFINED FLOW 440 14.2 METEORIC FLUID FLOW 442 14.3 DECAY OF
OVERPRESSURE AND PRESSURE SEALS 446 14.4 OVERPRESSURE DECAY IN CLAY 452
14.5 OVERPRESSURE BUILD-UP IN CLAY 454 14.6 THE GRAVITY NUMBER 457 14.7
OVERPRESSURE FROM THERMAL EXPANSION 459 14.8 SPECIAL CASES OF FLUID
EXPULSION AND MINERAL REACTIONS 463 14.9 OVERPRESSURE FROM QUARTZ
CEMENTATION 465 14.10 OVERPRESSURE FROM CEMENTATION OF PORE SPACE 465
14.11 FLUID EXPULSION AND MINERAL REACTIONS 472 14.12 OVERPRESSURE FROM
DEHYDRATION OF CLAY 473 14.13 WEAK (NON-RAYLEIGH) THERMAL CONVECTION 477
14.14 THERMAL CONVECTION 482 14.15 FURTHER READING 486 15 WELLS 488 15.1
STATIONARY PRESSURE FROM A WELL 488 15.2 WELLS AND STREAMLINES 491 15.3
THE SKIN FACTOR 493 15.4 TRANSIENT PRESSURE FROM A WELL 494 15.5 WELL
TESTING 499 CONTENTS APPENDIX: FOURIER SERIES, THE DISCRETE FOURIER
TRANSFORM AND THE FAST FOURIER TRANSFORM 502 A. 1 FOURIER SERIES 502 A.2
INTERPOLATION WITH FOURIER SERIES 503 A.3 THE DISCRETE FOURIER TRANSFORM
504 A.4 THE FAST FOURIER TRANSFORM 505 REFERENCES 513 INDEX 523
|
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| id | DE-604.BV036049132 |
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| indexdate | 2024-07-09T22:10:16Z |
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| isbn | 9780521761253 |
| language | English |
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| physical | XV, 527 S. Ill., graph. Darst. |
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| publisher | Cambridge Univ. Press |
| record_format | marc |
| spelling | Wangen, Magnus Verfasser aut Physical principles of sedimentary basin analysis Magnus Wangen 1. publ. Cambridge [u.a.] Cambridge Univ. Press 2010 XV, 527 S. Ill., graph. Darst. txt rdacontent n rdamedia nc rdacarrier "This book is based on lecture notes about the physical processes that govern sedimentary basins. The notes were the basis for a one-semester seminar named "Heat and fluid flow in sedimentary basins" offered by UNIK, an affiliate of the University of Oslo at Kjeller. As the title suggests, this book is about the physical principles of processes in sedimentary basins like for instance heat and fluid flow. The subject is approached by deriving the basic equations from fundamental principles like mass and energy conservation. The equations are then solved for simple problems that give insight into the processes.It should be possible to reproduce most of the solutions, calculations and plots presented in the book with a modest effort and a minimum of computer facilities"--Provided by publisher "Presenting a rigorous treatment of the physical and mechanical basis for the modelling of sedimentary basins, this book supplies geoscientists with practical tools for creating their own models. It begins with a thorough grounding in properties of porous media, linear elasticity, continuum mechanics and rock compressibility. Chapters on heat flow, subsidence, rheology, flexure and gravity consider sedimentary basins in the context of the Earth's lithosphere, and the book concludes with coverage of pore space cementation, compaction and fluid flow. The volume introduces basic, state-of-the-art models and demonstrates how to reproduce results using tools like MATLAB and Octave. Main equations are derived from first principles, and their basic solutions obtained and then applied. Separate notes sections supply more technical details, and the text is illustrated throughout with real-world examples, applications and test exercises. This is an accessible introduction to quantitative modelling of basins for graduate students, researchers and oil industry professionals"--Provided by publisher Fluid mechanics Rock mechanics Sedimentary basins Geomechanik (DE-588)4126903-2 gnd rswk-swf Sedimentationsbecken (DE-588)4180610-4 gnd rswk-swf Sedimentationsbecken (DE-588)4180610-4 s Geomechanik (DE-588)4126903-2 s DE-604 GBV Datenaustausch application/pdf http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=018940848&sequence=000001&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA Inhaltsverzeichnis |
| spellingShingle | Wangen, Magnus Physical principles of sedimentary basin analysis Fluid mechanics Rock mechanics Sedimentary basins Geomechanik (DE-588)4126903-2 gnd Sedimentationsbecken (DE-588)4180610-4 gnd |
| subject_GND | (DE-588)4126903-2 (DE-588)4180610-4 |
| title | Physical principles of sedimentary basin analysis |
| title_auth | Physical principles of sedimentary basin analysis |
| title_exact_search | Physical principles of sedimentary basin analysis |
| title_full | Physical principles of sedimentary basin analysis Magnus Wangen |
| title_fullStr | Physical principles of sedimentary basin analysis Magnus Wangen |
| title_full_unstemmed | Physical principles of sedimentary basin analysis Magnus Wangen |
| title_short | Physical principles of sedimentary basin analysis |
| title_sort | physical principles of sedimentary basin analysis |
| topic | Fluid mechanics Rock mechanics Sedimentary basins Geomechanik (DE-588)4126903-2 gnd Sedimentationsbecken (DE-588)4180610-4 gnd |
| topic_facet | Fluid mechanics Rock mechanics Sedimentary basins Geomechanik Sedimentationsbecken |
| url | http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=018940848&sequence=000001&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA |
| work_keys_str_mv | AT wangenmagnus physicalprinciplesofsedimentarybasinanalysis |