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1996 | Buch

Surge Tectonics: A New Hypothesis of Global Geodynamics

verfasst von: Arthur A. Meyerhoff, Irfan Taner, A. E. L. Morris, W. B. Agocs, M. Kamen-Kaye, M. I. Bhat, N. C. Smoot, Dong R. Choi

herausgegeben von: Donna Meyerhoff Hull

Verlag: Springer Netherlands

Buchreihe : Solid Earth Sciences Library

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Über dieses Buch

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.

Inhaltsverzeichnis

Frontmatter
Chapter 1. Why a New Hypothesis?
Abstract
Before 1962, the year in which H.H. Hess revived and revised Arthur Holmes’s (1931) concept of seafloor spreading (which also was proposed by Ampferer [1941]), the geology and geophysics departments of the world taught several geodynamics hypotheses. These hypotheses stimulated lively discussions and resulted in the publication of a highly diversified spectrum of ideas. After Hess’s version of seafloor spreading was published, diversity in geodynamics thinking began to wane, and outside of Asia and Eastern Europe, had all but vanished by the end of 1963. Most of these earlier and now contrary concepts are no longer taught or are presented briefly as old, outdated ideas in light of the new hypothesis of plate tectonics. This fact should generate concern among all scientists, for historically the rigorous testing of ideas effectively ceases in intellectual environments dominated by a single concept. Furthermore, it is the belief of these authors that as intensive geotectonic research has vastly increased the database for Earth-dynamic studies, plate tectonics has not adequately and completely explained the geology of many regions of the world.
Arthur A. Meyerhoff, Irfan Taner, A. E. L. Morris, W. B. Agocs, M. Kamen-Kaye, M. I. Bhat, N. C. Smoot, Dong R. Choi, Donna Meyerhoff Hull
Chapter 2. Unraveling Earth History: Tectonic Data Sets
Abstract
In this chapter, we discuss types of data sets available for discerning Earth tectonics todays that we feel have not been adequately explained by current tectonic hypotheses.
Arthur A. Meyerhoff, Irfan Taner, A. E. L. Morris, W. B. Agocs, M. Kamen-Kaye, M. I. Bhat, N. C. Smoot, Dong R. Choi, Donna Meyerhoff Hull
Chapter 3. Surge Tectonics
Abstract
Surge tectonics is a new hypothesis quite unlike previously proposed hypotheses, although many of its component parts are based on ideas long known. We believe the hypothesis provides a comprehensive and internally consistent explanation of all tectonic phenomena without the necessity of making unsupported assumptions or ad hoc explanations. We have found nothing that surge tectonics cannot explain in a simpler way than other tectonic hypotheses. Surge tectonics draws on well-known physical laws, especially those related to Newton’s laws of motion and gravity. Fluid dynamics plays an important role in surge tectonics. (For more information on the laws we utilize, those mentioned in the text are defined in the Appendix; those wishing more detail are referred to two standard physics textbooks by Sears et al. [1974] and Blatt [1983]. An excellent state-of-the-art fluid-dynamics text is that by Tritton [1988]).
Arthur A. Meyerhoff, Irfan Taner, A. E. L. Morris, W. B. Agocs, M. Kamen-Kaye, M. I. Bhat, N. C. Smoot, Dong R. Choi, Donna Meyerhoff Hull
Chapter 4. Examples of Surge Channels
Abstract
In this chapter, we present actual examples of the major types of surge channels, following the outline of Table 3.2 and Figure 3.39. We also discuss the criteria for recognizing the different types of surge channels, listed on Table 3.3.
Arthur A. Meyerhoff, Irfan Taner, A. E. L. Morris, W. B. Agocs, M. Kamen-Kaye, M. I. Bhat, N. C. Smoot, Dong R. Choi, Donna Meyerhoff Hull
Chapter 5. The Tectonic Evolution of Southeast Asia—A Regional Application of the Surge-Tectonics Hypothesis
Abstract
In this chapter, we give a surge-tectonic interpretation of the geological evolution of southeastern Asia. This part of the book should be treated as interpretative and not as an attempt at a definitive statement on the tectonic history of southeastern Asia (Fig. 5.1). We also present a series of paleotectonic surge-channel maps to illustrate our interpretation. These maps (Figs. 5.2, 5.3, 5.6, 5.8–5.12 and 5.17–5.18) portray the major stable areas (massifs and platforms) and paleogeothermal phenomena (surge channels) of southeastern Asia from the beginning of Sinian time (850 Ma) through the present. Insofar as possible, we identified both former and still active surge channels on the basis of the criteria for the identification of surge channels that were listed in Chapter 3. The literature sources used for these maps are listed in the bibliography: an asterisk appears before each source used.
Arthur A. Meyerhoff, Irfan Taner, A. E. L. Morris, W. B. Agocs, M. Kamen-Kaye, M. I. Bhat, N. C. Smoot, Dong R. Choi, Donna Meyerhoff Hull
Chapter 6. Magma Floods, Flood Basalts, and Surge Tectonics
Abstract
Tyrrell (1937) brought into the literature the term “flood basalts,” to give substance to a concept that he felt would improve the understanding of the effusion and flow of basaltic lavas. Tyrell was dissatisfied with the term “plateau basalt,” which had been current for more than a half century because it “… merely refers to an accidental and inessential feature resulting from levelling-up, erosion or Eaith movement.” Tyrrell was aware, however, that his predecessor by more than a half century, Sir Archibald Geikie, understood fully the dynamics and the framework of “plateau basalt” (Geikie, 1887), for he noted: “Sir A. Geikie actually mentions the word ‘flooded’ …” However, Tyrrell then commented “…I hold that ‘flood basalt’ is a much more fitting designation for this colossal type of basalt accumulation….”
Arthur A. Meyerhoff, Irfan Taner, A. E. L. Morris, W. B. Agocs, M. Kamen-Kaye, M. I. Bhat, N. C. Smoot, Dong R. Choi, Donna Meyerhoff Hull
Chapter 7. Conclusions
Abstract
We have proposed a new hypothesis of global tectonics in this book, one that is different and will be considered unorthodox by many scientists and non-scientists alike. However, we believe that current tectonic hypotheses cannot adequately explain the increasing volume of data being collected by both old and new technologies. We believe that the hypothesis of surge tectonics does explain these data sets, in a way that is simple and more accurate.
Arthur A. Meyerhoff, Irfan Taner, A. E. L. Morris, W. B. Agocs, M. Kamen-Kaye, M. I. Bhat, N. C. Smoot, Dong R. Choi, Donna Meyerhoff Hull
Backmatter
Metadaten
Titel
Surge Tectonics: A New Hypothesis of Global Geodynamics
verfasst von
Arthur A. Meyerhoff
Irfan Taner
A. E. L. Morris
W. B. Agocs
M. Kamen-Kaye
M. I. Bhat
N. C. Smoot
Dong R. Choi
herausgegeben von
Donna Meyerhoff Hull
Copyright-Jahr
1996
Verlag
Springer Netherlands
Electronic ISBN
978-94-009-1738-5
Print ISBN
978-94-010-7278-6
DOI
https://doi.org/10.1007/978-94-009-1738-5