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  • 1
    Keywords: Tectonics ; Konferenzschrift 1991 ; Aufsatzsammlung ; Konferenzschrift ; Tektonik ; Mechanische Spannung ; Bruchtektonik ; Klufttektonik ; Tektonik ; Tektonik ; Mechanische Spannung ; Bruchtektonik ; Klufttektonik ; Tektonik
    Type of Medium: Book
    Pages: 194 S , Ill
    ISBN: 0521428580 , 085403448X
    DDC: 551.1
    RVK:
    Language: English
    Note: First publ. in Philosophical transactions of the Royal Society of London, series A, vol. 337 (no. 1645)
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  • 2
    Online Resource
    Online Resource
    San Diego :Elsevier,
    Keywords: Continental margins -- Congresses. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (319 pages)
    Edition: 1st ed.
    ISBN: 9781483257259
    Language: English
    Note: Front Cover -- Sedimentary Basins of Continental Margins and Cratons -- Copyright Page -- Table of Contents -- Chapter 1. MECHANISMS OF BASIN SUBSIDENCE - AN INTRODUCTORY REVIEW -- INTRODUCTION -- HYPOTHESES OF BASIN SUBSIDENCE MECHANISM -- TESTING THE HYPOTHESES -- ACKNOWLEDGEMENT -- REFERENCES -- Chapter 2. RHEOLOGY OF THE LITHOSPHERE - EXPERIMENTAL INDICATIONS -- ABSTRACT -- INTRODUCTION -- STRUCTURE, COMPOSITION AND TEMPERATURE OF THE LITHOSPHERE -- ELASTIC PROPERTIES AND FLEXURAL RIGIDITY OF THE LITHOSPHERE -- 'VISCOUS' PROPERTIES OF THE LITHOSPHERE -- CHOICE OF CREEP PARAMETERS -- MODELS OF LITHOSPHERE RHEOLOGY -- RHEOLOGY OF YOUNG CONTINENTAL MARGINS -- ACKNOWLEDGMENTS -- REFERENCES -- Chapter 3. FLEXURE OF THE LITHOSPHERE AND CONTINENTAL MARGIN BASINS -- ABSTRACT -- INTRODUCTION -- SEDIMENT LOADING AT A CONTINENTAL MARGIN -- 25 M.Y. GULF OF LION MARGIN -- DISCUSSION -- ACKNOWLEDGEMENTS -- REFERENCES -- Chapter 4. PLATFORM SUBSIDENCE MECHANISMS AND "EUSTATIC" SEA-LEVEL CHANGES -- ABSTRACT -- INTRODUCTION -- CALCULATION OF EUSTATIC EFFECTS -- EUSTATIC CHANGE AMPLITUDE -- CONCLUSIONS -- ACKNOWLEDGMENTS -- REFERENCES -- Chapter 5. THERMAL AND MECHANICAL EVOLUTION OF THE MICHIGAN BASIN -- ABSTRACT -- INTRODUCTION -- RHEOLOGICAL CONSIDERATIONS -- AXISYMMETRIC BENDING OF A LITHOSPHERIC PLATE -- GRAVITY -- THERMAL EVOLUTION OF THE BASIN -- BASIN FORMATION MODEL -- ACKNOWLEDGMENTS -- REFERENCES -- Chapter 6. FORMATION OF SEDIMENTARY BASINS OF GRABEN TYPE BY EXTENSION OF THE CONTINENTAL CRUST -- ABSTRACT -- INTRODUCTION -- OUTLINE OF PROPOSED MECHANISM -- PREDICTED WIDTH OF THE GRABEN -- ENERGY BUDGET OF WEDGE SUBSIDENCE MECHANISM -- DISCUSSION -- REFERENCES -- Chapter 7. MAJOR SYNCHRONOUS EVENTS IN CONTINENTAL SHELVES -- ABSTRACT -- INTRODUCTION -- INCEPTION OF SHELF DEVELOPMENT (PERMIAN) -- TAPHROGENIC SUBSIDENCE (TRIASSIC TO EARLY CRETACEOUS). , THE MID-CRETACEOUS CHANGE (APTIAN/ALBIAN) -- INTER CRATONIC BASIN AL SUBSIDENCE (LATE CRETACEOUS AND TERTIARY) -- SUMMARY -- REFERENCES -- Chapter 8. DEVELOPMENT OF GRABEN ASSOCIATED WITH THE INITIAL RUPTURES OF THE ATLANTIC OCEAN -- ABSTRACT -- INTRODUCTION -- CENTRAL ATLANTIC GRABEN -- SOUTH ATLANTIC GRABEN -- GRABEN OF THE BENUE TROUGH COMPLEX -- GRABEN OF THE GULF OF GUINEA AND THE NORTH COAST OF BRAZIL -- GRABEN BETWEEN IBERIA, ARMORICA AND THE GRAND BANKS -- LABRADOR SEA AND BAFFIN BAY GRABEN -- GRABEN OF NORTHWESTERN EUROPE -- GRABEN OF THE NORWEGIAN-GREENLAND SEA -- ORIGIN AND DEVELOPMENT OF MARGINAL GRABEN -- CONCLUSIONS -- REFERENCES -- Chapter 9. SEDIMENTARY BASINS OF THE ATLANTIC MARGIN OF NORTH AMERICA -- ABSTRACT -- INTRODUCTION -- MECHANICS OF BASIN FORMATION -- EVOLUTION OF U.S. ATLANTIC MARGIN BASINS -- ACKNOWLEDGMENTS -- REFERENCES -- Chapter 10. GEODYNAMIC SIGNIFICANCE OF SPASMODIC, CRETACEOUS, RAPID SUBSIDENCE RATES, CONTINENTAL SHELF, U.S.A. -- ABSTRACT -- INTRODUCTION -- NEW RESULTS -- POSSIBLE SOURCES OF ERROR IN THE DATA BASE -- SIGNIFICANCE -- ACKNOWLEDGMENT -- REFERENCES -- Chapter 11. OBSERVATIONS ON THE PROCESSES OF SEDIMENTARY BASIN FORMATION AT THE MARGINS OF SOUTHERN AFRICA -- ABSTRACT -- INTRODUCTION -- EVOLUTION OF THE SEDIMENTARY BASINS -- REGIONAL EVENTS -- REFERENCES -- Chapter 12. THE GEOSYNCLINAL PAIR AT THE CONTINENTAL MARGIN OF PERU -- ABSTRACT -- INTRODUCTION -- THE OLDER FRAMEWORK -- THE MESOZOIC SEQUENCE -- CONDITIONS OF BASIN FORMATION -- THE INTRUSIVES -- THE GEOTECTONIC CYCLE IN PERU -- DISCUSSION -- CONCLUSION -- REFERENCES -- Chapter 13. SEDIMENTARY FACIES AND THE ORIGINS OF BASIN SUBSIDENCE ALONG THE NORTHERN MARGIN OF THE SUPPOSED HERCYNIAN OCEAN -- ABSTRACT -- INTRODUCTION -- GENERAL ACCOUNT -- BRITISH AND IRISH BASINS -- MARITIME CANADIAN BASINS -- PREVIOUS HYPOTHESES FOR BASIN ORIGINS. , ORIGIN OF BRITISH/IRISH BASINS -- ORIGIN OF CANADIAN BASINS -- CONCLUSIONS -- ACKNOWLEDGEMENTS -- REFERENCES -- Chapter 14. EVOLUTION OF THE SVERDRUP BASIN, ARCTIC CANADA -- ABSTRACT -- INTRODUCTION -- GEOLOGICAL SETTING -- DATA SOURCES -- RESULTS -- SUMMARY AND GENERALIZATION OF SUBSIDENCE HISTORY -- INTERPRETATION -- ACKNOWLEDGEMENTS -- REFERENCES -- Chapter 15. THE CHAD BASIN: AN ACTIVE INTRA-CONTINENTAL BASIN -- ABSTRACT -- INTRODUCTION -- THE CHAD BASIN -- SEDIMENTS OF THE CHAD BASIN -- HIGH GROUND AND VOLCANIC ACTIVITY ON THE CHAD WATERSHED -- HYPOTHESIS OF ORIGIN AND HISTORY OF THE CHAD BASIN -- THE LITHOSPHERE OF THE CHAD BASIN -- POSSIBLE ANALOGY WITH THE MICHIGAN BASIN -- CONCLUSION -- REFERENCES -- Chapter 16. DEVONIAN BASINS OF WESTERN NORWAY - SEDIMENTARY RESPONSE TO TECTONISM AND TO VARYING TECTONIC CONTEXT -- ABSTRACT -- INTRODUCTION -- TECTONISM - THE FUNDAMENTAL CONTROL ON SEDIMENTATION -- COARSENING-UPWARDS SEQUENCE - THE BASIC RESPONSE TO AN EPISODE OF VERTICAL TECTONIC MOVEMENT -- CYCLIC SEDIMENTATION IN HORNELEN AND SOLUND BASINS -- SIGNS OF VARYING TECTONIC CONTEXT -- CONCLUSIONS -- ACKNOWLEDGEMENTS -- REFERENCES -- Chapter 17. GEOPHYSICAL STUDIES OF THE MAJOR SEDIMENTARY BASINS OF THE INDIAN CRATON, THEIR DEEP STRUCTURAL FEATURES AND EVOLUTION -- ABSTRACT -- INTRODUCTION -- CUDDAPAH BASIN -- VINDHYAN BASIN -- OTHER INTRA-CRATONIC BASINS -- CONCLUSION -- ACKNOWLEDGEMENT -- REFERENCES -- Chapter 18. DYNAMICS OF THE DEVELOPMENT OF THE RUSSIAN PLATFORM STRUCTURES -- ABSTRACT -- INTRODUCTION -- HISTORY OF TECTONIC MOVEMENTS -- TYPES OF BASINS AND DOWNWARPING RATES -- COMPARISON WITH THE M-DISCONTINUITY TOPOGRAPHY -- CONCLUSIONS -- ACKNOWLEDGEMENTS -- REFERENCES -- Chapter 19. THE REGIONAL STRUCTURE OF THE TURANIAN PLATFORM AND ITS DEVELOPMENT -- ABSTRACT. , INTRODUCTION, METHODS, TECHNIQUES, MATERIALS STUDIED AND AREA DESCRIPTIONS -- RESULTS -- CONCLUSION -- REFERENCES -- Chapter 20. THE HISTORY AND THE DYNAMICS OF THE DEVELOPMENT OF THE WEST SIBERIAN PLATFORM -- ABSTRACT -- INTRODUCTION -- STAGES OF TECTONIC DEVELOPMENT -- SOME FEATURES OF THE DEVELOPMENT OF PLATFORM UPLIFTS -- CONCLUSION -- ACKNOWLEDGEMENT -- REFERENCES -- Chapter 21. DEVELOPMENT OF MAIN STRUCTURES OF THE SIBERIAN PLATFORM: HISTORY AND DYNAMICS -- ABSTRACT -- INTRODUCTION -- METHODS OF INVESTIGATION -- RESULTS OF INVESTIGATIONS -- CONCLUSIONS -- ACKNOWLEDGMENTS -- REFERENCES -- Chapter 22. SEDIMENTARY BASINS OF THE EAST ANTARCTIC CRATON FROM GEOPHYSICAL EVIDENCE -- ABSTRACT -- INTRODUCTION -- TOPOGRAPHIC IDENTIFICATION OF BASINS -- EVIDENCE FOR SEDIMENTS -- BASIN STRUCTURE AND SEDIMENT AGE -- CONCLUSIONS -- ACKNOWLEDGMENTS -- REFERENCES.
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  • 3
    Publication Date: 2023-05-12
    Keywords: Area/locality; Conductivity, average; Depth, bottom/max; Depth, top/min; ELEVATION; Heat flow; Heat production, average; LATITUDE; LONGITUDE; Method comment; Number; Number of conductivity measurements; Number of heat production measurements; Number of temperature data; Sample, optional label/labor no; Temperature gradient
    Type: Dataset
    Format: text/tab-separated-values, 21 data points
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  • 4
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical prospecting 7 (1959), S. 0 
    ISSN: 1365-2478
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences , Physics
    Notes: A method is described in which the major part of gravimetric terrain corrections may be estimated by digital computing methods.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical prospecting 6 (1958), S. 0 
    ISSN: 1365-2478
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences , Physics
    Notes: Some new formulae for the rapid estimation from the gravity field of the maximum possible depth to the top surface of gravitating bodies of positive mass are stated, discussed and proved.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical prospecting 11 (1963), S. 0 
    ISSN: 1365-2478
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences , Physics
    Notes: Two methods applicable to computers are described which are designed to evaluate the vertical, horizontal and total intensity magnetic anomalies due to finite three-dimensional bodies of uniform polarisation contrast. The direction of polarisation need not be co-linear with the Earth's field, thus allowing for a remanent component; and the calculation may be performed for a given model for several different directions of polarisation concurrently. The first programme depends on the transformation from a volume integral to a surface integral and the approximate representation of the surface by a series of plane polygonal faces. The second programme is based on an extension of Vacquier's graphical method.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 126 (1996), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Thin-plate flexure theory has previously assumed unconstrained end loading to model the flexure associated with a fault cutting a strong upper crust above an inviscid substratum. This assumption implies that fault planes are not parallel when the density differential across the plate differs on upthrown and downthrown sides, as in the development of a sediment-filled half-graben. A downward-widening extension crack would develop during planar normal faulting, which conflicts with the geological experience that such cracks are closed by overburden pressure below a few hundred metres depth. A new analytical solution is presented, in which the fault planes are constrained to be parallel and in contact. The new theory gives a substantially larger ratio of upthrow to downthrow, and a significantly wider half-graben and narrower uplift.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 243 (1973), S. 339-341 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Fig. 1 Two-dimensional model of the lithosphere overlying the asthenosphere, with linear and quadratic velocity-depth distributions shown at the right side. Our theoretical model consists of a horizontal two-dimensional elastic plate of length L, thickness d and Young's modulus E representing a ...
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 227 (1970), S. 268-269 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Flinn has suggested a new line for the Great Glen fault which does not cross gravity "high" A north of the Shet-lands. This raises a problem which needs to be recognized. To quote Allen5, "probably the most impressive feature of thoroughgoing transcurrent faults is their extreme linearity over ...
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 225 (1970), S. 265-268 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The regional rise in Bouguer anomaly across the shelf towards the continental margin is shown in Fig. 2. This is attributed to the thinning of the crust beneath the slope, from a continental type beneath the shelf to a thinner crust beneath the Shetland?Faroe channel, in quantitative agreement with ...
    Type of Medium: Electronic Resource
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