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  • 1
    Book
    Book
    Dordrecht [u. a.] :Kluwer,
    UID:
    almahu_BV024768897
    Format: VIII, 188 S. : , graph. Darst.
    ISBN: 0-7923-0972-3
    Language: English
    Subjects: Geography
    RVK:
    Keywords: Geologie ; Paläogeografie ; Einführung ; Einführung ; Einführung
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  • 2
    Book
    Book
    Boulder, Colorado : The Geological Society of America
    UID:
    gbv_325835063
    Format: XIV, 199 S. , graph. Darst., Kt.
    ISBN: 0813711290
    Series Statement: Memoir / The Geological Society of America 129
    Language: English
    Keywords: Große Antillen ; Karibik ; Geologie ; Stratigraphie ; Paläogeografie ; Haiti ; Dominikanische Republik ; Cayman Islands ; Kuba ; Jamaika ; Historische Geologie
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  • 3
    UID:
    almafu_BV011519651
    Format: IX, 69 S. : graph. Darst.
    ISBN: 0-8137-1189-4
    Series Statement: Geological Society of America: Memoir 189
    Language: English
    Keywords: Phanerozoikum ; Tiere ; Plattentektonik ; Phanerozoikum ; Pflanzen ; Plattentektonik
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  • 4
    UID:
    b3kat_BV011519651
    Format: IX, 69 S. , graph. Darst.
    ISBN: 0813711894
    Series Statement: Geological Society of America: Memoir 189
    Language: English
    Keywords: Phanerozoikum ; Tiere ; Plattentektonik ; Phanerozoikum ; Pflanzen ; Plattentektonik
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  • 5
    UID:
    b3kat_BV045178675
    Format: 1 Online-Ressource (XVIII, 326 p)
    ISBN: 9789400917385
    Series Statement: Solid Earth Sciences Library 9
    Content: TECTONlCS AND PHYSICS Geology, although rooted in the laws of physics, rarely has been taught in a manner designed to stress the relations between the laws and theorems of physics and the postulates of geology. The same is true of geophysics, whose specialties (seismology, gravimetIy, magnetics, magnetotellurics) deal only with the laws that govern them, and not with those that govern geology's postulates. The branch of geology and geophysics called tectonophysics is not a formalized discipline or subdiscipline, and, therefore, has no formal laws or theorems of its own. Although many recent books claim to be textbooks in tectonophysics, they are not; they are books designed to explain one hypothesis, just as the present book is designed to explain one hypothesis. The textbook that comes closest to being a textbook of tectonophysics is Peter 1. Wyllie's (1971) book, The Dynamic Earth. Teachers, students, and practitioners of geology since the very beginning of earth science teaching have avoided the development of a rigorous (but not rigid) scientific approach to tectonics, largely because we earth scientists have not fully understood the origin of the features with which we are dealing. This fact is not at all surprising when one considers that the database for hypotheses and theories of tectonics, particularly before 1960, has been limited to a small part of the exposed land area on the Earth's surface
    Additional Edition: Erscheint auch als Druck-Ausgabe ISBN 9789401072786
    Language: English
    Keywords: Geodynamik
    URL: Volltext  (URL des Erstveröffentlichers)
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  • 6
    UID:
    b3kat_BV045177210
    Format: 1 Online-Ressource (XI, 188 p)
    ISBN: 9789401137706
    Content: all such systems are important, the Proterozoic column This volume concerns the geology of China, and it examinesthat concern by expositionsofthe stratigraphy, possibly is unique in its continuous sedimentary devel the paleogeography,and the tectonics ofthat remarkable opment and in its reference section of global rank. In paleogeography, this volume describes and illustra country. In this sense, therefore, our aims and purposes are explicit in the title. The senior author and his tes first the broad distribution of Proterozoic deposits. colleagues, furthermore, do not have in mind any special Succeeding descriptions and illustrations trace the ebb and flow of shallow marine waters across China as or specific audience. This volume is quite simply for all geologists. By far the majority will be those whose Phanerozoic time of more than 600 million years elapses native tongue is English, or those who understand from the beginning of the Cambrian to the present. In structure, this volume emphasizes the importance English. Not to be overlooked, moreover, is the large number ofChinese geologists who not only read English of paraplatforms, platforms, geosynclines, and great but also who themselves write studies in English that east-west zones of fracture in the Precambian, also the appear in publications in both their homeland and effects of these early structural elements on structure abroad. in the ensuing Phanerozoic. In the Phanerozoic itself, north-south stress developed in the pre-Phanerozoic A constantly growing interest in the geology of China continued through much of the Paleozoic
    Additional Edition: Erscheint auch als Druck-Ausgabe ISBN 9789401056786
    Language: English
    Keywords: China ; Geologie ; China ; Paläogeografie ; Einführung
    URL: Volltext  (URL des Erstveröffentlichers)
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  • 7
    UID:
    b3kat_BV007182448
    Format: XIV, 199 S.
    Series Statement: Geological Society of America: Memoir 129
    Language: English
    Subjects: Geography
    RVK:
    Keywords: Große Antillen ; Geologie
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  • 8
    UID:
    almahu_9948600922202882
    Format: XI, 188 p. , online resource.
    Edition: 1st ed. 1991.
    ISBN: 9789401137706
    Content: all such systems are important, the Proterozoic column This volume concerns the geology of China, and it examinesthat concern by expositionsofthe stratigraphy, possibly is unique in its continuous sedimentary devel­ the paleogeography,and the tectonics ofthat remarkable opment and in its reference section of global rank. In paleogeography, this volume describes and illustra­ country. In this sense, therefore, our aims and purposes are explicit in the title. The senior author and his tes first the broad distribution of Proterozoic deposits. colleagues, furthermore, do not have in mind any special Succeeding descriptions and illustrations trace the ebb and flow of shallow marine waters across China as or specific audience. This volume is quite simply for all geologists. By far the majority will be those whose Phanerozoic time of more than 600 million years elapses native tongue is English, or those who understand from the beginning of the Cambrian to the present. In structure, this volume emphasizes the importance English. Not to be overlooked, moreover, is the large number ofChinese geologists who not only read English of paraplatforms, platforms, geosynclines, and great but also who themselves write studies in English that east-west zones of fracture in the Precambian, also the appear in publications in both their homeland and effects of these early structural elements on structure abroad. in the ensuing Phanerozoic. In the Phanerozoic itself, north-south stress developed in the pre-Phanerozoic A constantly growing interest in the geology of China continued through much of the Paleozoic.
    Note: I Introduction -- Physical Geography -- II Stratigraphy and Paleontology -- Pre-Sinian -- Sinian -- Paleozoic -- Cambrian System -- Ordovician System -- Silurian System -- Devonian System -- Carboniferous System -- Permian System -- Mesozoic -- Triassic System -- Jurassic System -- Cretaceous System -- Cenozoic -- Tertiary System -- Quarternary System -- III Tectonics and Structure of China.
    In: Springer Nature eBook
    Additional Edition: Printed edition: ISBN 9789401056786
    Additional Edition: Printed edition: ISBN 9780792309727
    Additional Edition: Printed edition: ISBN 9789401137713
    Language: English
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  • 9
    UID:
    almahu_9948601216902882
    Format: XVIII, 326 p. , online resource.
    Edition: 1st ed. 1996.
    ISBN: 9789400917385
    Series Statement: Solid Earth Sciences Library ; 9
    Content: TECTONlCS AND PHYSICS Geology, although rooted in the laws of physics, rarely has been taught in a manner designed to stress the relations between the laws and theorems of physics and the postulates of geology. The same is true of geophysics, whose specialties (seismology, gravimetIy, magnetics, magnetotellurics) deal only with the laws that govern them, and not with those that govern geology's postulates. The branch of geology and geophysics called tectonophysics is not a formalized discipline or subdiscipline, and, therefore, has no formal laws or theorems of its own. Although many recent books claim to be textbooks in tectonophysics, they are not; they are books designed to explain one hypothesis, just as the present book is designed to explain one hypothesis. The textbook that comes closest to being a textbook of tectonophysics is Peter 1. Wyllie's (1971) book, The Dynamic Earth. Teachers, students, and practitioners of geology since the very beginning of earth­ science teaching have avoided the development of a rigorous (but not rigid) scientific approach to tectonics, largely because we earth scientists have not fully understood the origin of the features with which we are dealing. This fact is not at all surprising when one considers that the database for hypotheses and theories of tectonics, particularly before 1960, has been limited to a small part of the exposed land area on the Earth's surface.
    Note: 1: Why a New Hypothesis? -- 1.1 Introduction -- 1.2 Former and Current Concepts of Earth Dynamics -- 1.3 Conclusion -- 2: Unraveling Earth History: Tectonic Data Sets -- 2.1 Data Availability -- 2.2 New Data Acquisition -- 2.3 Data Sets Unexplained in Current Tectonic Models: Foundation for a New Hypothesis -- 2.4 Conclusion -- Chapter3: Surge Tectonics -- 3.1 Introduction -- 3.2 Velocity Structure of the Earth's Outer Shells -- 3.3 Contraction -- 3.4 Contraction as an Explanation of Earth Dynamics -- 3.5 Review of Surge and Related Concepts in Earth-Dynamic Theory -- 3.6 Geotectonic Cycle of Surge Tectonics -- 3.7 Pascal's Law-the Core of Tectogenesis -- 3.8 Evidence for the Existence of Surge Channels -- 3.9 Geometry of Surge Channels -- 3.10 Demonstration of Tangential Flow in Surge Channels -- 3.11 Mechanism for Eastward Surge -- 3.12 Classification of Surge Channels -- 3.13 K Structures -- 3.14 Criteria for the Identification of Surge Channels -- 4: Examples of Surge Channels -- 4.1 Ocean-Basin Surge Channels -- 4.2 Surge Channels of Continental Margins -- 4.3 Continental Surge Channels -- 4.4 Surge Channels in Zones of Transtension-Transpression -- 5: The Tectonic Evolution of Southeast Asia-a Regional Application of the Surge-Tectonics Hypothesis -- 5.1 Surge Tectonic Framework -- 5.2 Surge-Tectonic History -- 6: Magma Floods, Flood Basalts, and Surge Tectonics -- 6.1 Introduction -- 6.2 Descriptions of Selected Continental Flood-Basalt Provinces -- 6.3 The Use of Geochemistry in Identifying Flood Basalts -- 6.4 Geochemical Comparisons among Basalts Erupted in Different Tectonic Settings -- 6.5 Duration of Individual Basalt Floods -- 6.6 Flood-Basalt Provinces and Frequency in Geologic Time -- 6.7 Non-Basalt Flood Volcanism in Flood-Basalt Provinces -- 6.8 Flood Basalts or Magma Floods? -- 6.9 Surge-Tectonics Origin of Magma Floods -- 7: Conclusions.
    In: Springer Nature eBook
    Additional Edition: Printed edition: ISBN 9789401072786
    Additional Edition: Printed edition: ISBN 9780792341567
    Additional Edition: Printed edition: ISBN 9789400917392
    Language: English
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  • 10
    UID:
    almafu_BV026236862
    Format: XIV, 199 S.
    Series Statement: Memoir / Geological Society of America 129
    Language: English
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