By C. E. B. Conybeare
Read or Download Lithostratigraphic Analysis of Sedimentary Basins PDF
Similar analysis books
This booklet includes all invited contributions of an interdisciplinary workshop of the UNESCO operating team on structures research of the ecu and North American area entitled "Stochastic Phenomena and Chaotic Behaviour in complicated Systems". The assembly used to be held at lodge Winterthalerhof in Flattnitz, Karnten, Austria from June 6-10, 1983.
Das Arbeitsbuch Mathematik für Ingenieure richtet sich an Studierende der ingenieurwissenschaftlichen Fachrichtungen. Der erste Band behandelt Lineare Algebra sowie Differential- und Integralrechnung für Funktionen einer und mehrerer Veränderlicher bis hin zu Integralsätzen. Die einzelnen Kapitel sind so aufgebaut, dass nach einer Zusammenstellung der Definitionen und Sätze in ausführlichen Bemerkungen der Stoff ergänzend aufbereitet und erläutert wird.
- Arbeitsleistung, Identität und Markt: Eine Analyse marktförmiger Leistungssteuerung in Arbeitsorganisationen (German Edition)
- Analysis and Topology in Nonlinear Differential Equations: A Tribute to Bernhard Ruf on the Occasion of his 60th Birthday (Progress in Nonlinear Differential Equations and Their Applications)
- Analysis and Control System Techniques for Electric Power Systems Part 4 of 4: Advances in Theory and Applications
- Semiclassical Analysis
- Advances in Composite Materials-ecodesign and Analysis
- Topics in Functional Analysis over Valued Division Rings
Extra info for Lithostratigraphic Analysis of Sedimentary Basins
Seen 32 1. INTRODUCTION with different eyes and possibly with additional information, the previous interpretation will probably be modified. For although the data used in a study are accepted as valid and the methods of employment of this data are scientific, the interpretations arrived at by different geologists may not be the same. There is inevitably a certain element of subjective and imaginative thinking in the formulation of interpretations, and were it not so, the earth sciences would stagnate and the discovery of hydrocarbon and mineral deposits would be retarded.
The sequence of events that gave rise to the origin of the oceans and that shaped the development of landmasses can only be surmised, but it seems not unreasonable to assume, as Stewart (1972) has done, that during the Precambrian zones of tension within the crust produced widening fractures which were filled along their margins with wedges of sediment. A similar concept was expressed by Anhaeusser et al. (1969) to explain the origin of greenstone belts within Precambrian shields. Both concepts conceive the development of linear depressions in the crust formed by tensional rifts.
It is axiomatic that sedimentary basins develop where they do, not necessarily because they are filling topographic depressions but because the underlying basement is subsiding at a rate compatible with the rate of sedimentation and the degree of compaction of the sediments. To what extent the weight of the pile of sediments causes the basement to sink, commonly by means of faulting, is arguable. The fact is, the relationship CLASSIFICATION OF SEDIMENTARY BASINS 25 obtains, signifying the importance of structural framework to the growth of sedimentary basins.