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  • 1
    Call number: 9/M 09.0155
    Description / Table of Contents: 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. - Characteristics of complex intracontinental sedimentary basins.- The Central European Basin System.- Strain and temperature in space and time.- Basin fill.- Salt dynamics.- Fluid systems.
    Type of Medium: Monograph available for loan
    Pages: XXIV, 520 S. + 1 CD-ROM , 49 schw.-w. Ill., 334 farb. Ill., 24 schw.-w. Tab., 1 schw.-w. Fotos, 23 farb. Fotos, 48 schw.-w. graph. Darst., 311 farb. graph. Darst.
    ISBN: 9783540850847
    detail.hit.classification_display:
    A.3.16.
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Call number: AR 97/12
    detail.hit.classification_display:
    A.3.5.
    Language: English
    Branch Library: GFZ Library
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  • 3
    Call number: AR 97/16
    detail.hit.classification_display:
    A.3.16.
    Language: English
    Branch Library: GFZ Library
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  • 4
    In: Terra nostra
    Pages: Vol. 1-2
    Series Statement: Terra Nostra
    detail.hit.classification_display:
    A.3.1.
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  • 5
    Call number: S 99.0056(2005, 5)
    In: Terra nostra
    Type of Medium: Series available for loan
    Pages: VIII, 135 S.
    Series Statement: Terra nostra 2005, 05
    Location: Lower compact magazine
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  • 6
    Call number: S 97.0506(577-2/1)
    In: Forschungsbericht
    Type of Medium: Series available for loan
    Pages: 139 S. : Ill., graph. Darst.
    ISBN: 9783936418910
    Series Statement: DGMK research report 577-2/1
    detail.hit.classification_display:
    A.3.16.
    Location: Lower compact magazine
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  • 7
    Call number: S 99.0056(99/3)
    In: Terra nostra
    Type of Medium: Series available for loan
    Pages: 45 S.
    Series Statement: Terra nostra 99/3
    detail.hit.classification_display:
    A.3.3.
    Location: Lower compact magazine
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  • 8
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 4/M 04.0355
    In: Lecture notes in earth sciences
    Type of Medium: Monograph available for loan
    Pages: VII, 229 S. , graph. Darst
    ISBN: 3540139834
    Series Statement: Lecture notes in earth sciences 2
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  • 9
    Unknown
    Berlin ; Heidelberg : Springer
    Description / Table of Contents: INTRODUCTION Theoretical modelling and the use of mathematical methods are presently gaining in importance since progress in both geology and mathematics offers new possibilities to combine both fields. Most geological problems are inherently geometrical and morphological, and, therefore, amenable to a classification of forms from a "Gestalt point of view". Geometrical objects have to possess an inherent stability in order to preserve their essential quality under slight deformations. Otherwise, we could hardly conceive of them or describe them, and today's observation would not reproduce yesterday's result (DANGELMAYR & GÜTTINGER, 1982). This principle has become known as "structural stability" (THOM, 1975), i.e. the persistence of a phenomenon under all allowed perturbations. Stability is also, of course, an assumption of classical Newtonian physics, which is essentially the theory of various kinds of smooth behavior (POSTON &STEWART, 1978). However, things sometimes "jump". A new species with a different morphology appears suddenly in the paleontological record (EI.DREDGE & GOULD, 1972), a fault develops, a landslide moves, a computer program becomes unstable with a certain data configuration, etc. It is, surprisingly, the topological approach which permits the study of a broad range of such phenomena in a coherent manner (POSTON & STEWART, 1978; LU, 1976; STEWART, 1982). The universal singularities and bifurcation processes derived from the concept of structural stabiIity determine the spontaneous formation of qualitatively similar spatio-temporal structures in systems of various geneses exhibiting critical behavior (DANGELMAYR & GÜTTINGER, 1982; THOM, 1975; POSTON & STEWART, 1978; GÜTTINGER & EIKEMEIER, t979; STEWART, 1981). In addition, this return to a "geometrization of phenomena"-- after decades of algorithmization-- comes much closer to the geologist's intuitive geometric reasoning. It is the aim of this study to elucidate, by examples, how the qualitative geometrical approach allows one to classify forms and to control the behavior of complex computer algorithms...
    Pages: Online-Ressource (229 Seiten)
    ISBN: 9783540139836
    Language: English
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  • 10
    Unknown
    Berlin ; Heidelberg : Springer
    Description / Table of Contents: INTRODUCTION In the context of evolutionary studies, it is the privilege of paleontologists to trace the actual course of evolutionary change over time spans that are adequate for such a slow process. At the same time it is their crux that they can not always hope to do this with the resolution necessary to reveal the causal relationships involved. The Tübingen Sonderforschungsbereich 53, "Palökologie", was primarily geared to study the interrelationships between organisms and environments in the fossil record. As is pointed out in this volume, such an approach will necessarily emphasize the static aspect of this relationship, all the more since this is what we need for the practical purposes of facies recognition. This was clone during a time interval of thirteen years at the level of individual species and taxonomic groups ("Konstruktions-Morphologie"), of characteristic facies complexes ("Fossil-Lagerstätten") and of assemblages ("Fossil- VergeseIlschaftungen") with the aim to recognize general patterns that persist in spite of the historical and evolutionary changes in the biosphere. But as our project came closer to its end, the possible causal relationships between physical and evolutionary changes became more tangible. This trend is expressed by symposia devoted to the biological effects of long term tectonic changes (KULLMANN & SCHÖNENBERG, eds., 1983) and of short term physical events (EINSELE & SEILACHER, eds., 1982). But in retrospect it appears that the time scales of the environmental changes chosen were either too large or too small to reveal the mechanisms of evolutionary response. The present volume is the outcome of a symposium of the projects B 20 ("Bankungsrhythmen in sedimentologischer, ökologischer und diagenetischer Sicht", directed by U. BAYER), D 40 ("Analoge Gehäuse-Aberrationen bei Ammonoideen", directed by J. WIEDMANN) and D 60 ("Substratwechsel im marinen Benthos", directed by A. SEILACHER) in September, 1983. tt addresses environmental changes at time scales large enough to produce more than a local ecological response and short enough to observe evolutionary and/or migratory changes at the species and genus levels. It also focusses on basins which by various degrees of isolation provided suitable sites for "evolutionary experiments", such as lakes and marginal epicontinental basins. In a way, this book is a successor of the previous one on "Cyclic and event stratification" (EINSELE & SEILACHER, eds., 1982). Small scale cycles and events are the 'primitives' of a sedimentary sequence, the lowermost scale from which it can be deciphered. However, medium and long term physical cycles commonly impress sedimentological and lithological trends on the stratigraphic column which are accompanied by faunal replacements and cycles. But since sedimentation is controlled both by physical and biological processes, which are intercorrelated in complicated ways, we also need to decode the stratigraphic text. In this effort, paleontological and sedimentological interpretation must go hand in hand. On the 'megascale' of global sea-level changes faunal and species evolution is triggered by opening and closing of migration pathways, sometimes providing us with malor biostratigraphic boundaries. As it turns out, however, integrated research and the choice of suitable scales do not free us from problems of resolution. Thus our inability to distinguish local speciation from ecophenotypic modification and from immigration in the fossil record excludes definite evolutionary answers even in well studied cases. Nevertheless we hope that this approach opens a fruitful discussion, in which stratigraphy, systematic paleontology and paleoecology will be reconciled in a concerted effort to eventually understand the evolutionary mechanisms of our biosphere.
    Pages: Online-Ressource (465 Seiten)
    ISBN: 9783540139829
    Language: English
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