Author: K.H. Olsen
Publisher: Elsevier
ISBN: 0080529836
Category : Science
Languages : en
Pages : 511
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Book Description
This multi-author book has been prepared by an international group of geoscientists that have been active in rift research since the late 1960s. In 1984, an informal, grass-roots study group was initiated to compare individual research results and to explore in greater depth the apparent differences and similarities in the interpretations from various rift systems. The group became known as the CREST working group, an acronym of Continental Rifts: Evolution, Structure and Tectonics, which not surprisingly became the title of this book.Continental Rifts: Evolution, Structure, Tectonics presents an overview of the present state of understanding and knowledge of the processes of continental rifting from a multidisciplinary, lithospheric scale perspective. The chapters have been structured on each rift system in approximately the same synoptic sequence, so as to facilitate comparisons of rifts by the reader. The book complements its predecessors by presenting a more unified picture. It succeeds in presenting the status of a representative majority of the continental rift systems that have been at the forefront of recent research. For students and experienced researchers alike, this book will be of significant value in assessing the current state of knowledge and in serving as a framework for future research.
Author: Achyuta Ayan Misra
Publisher: Springer
ISBN: 3319205765
Category : Science
Languages : en
Pages : 97
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Book Description
This work reviews the mechanism of rifting with a focus on pre-existing tectonic weaknesses in pre-rift and/or basement rocks, i.e., on tectonic inheritance. The passive margins that are studied in this book are the Norwegian Continental Shelf, the Eastern North America and the East and West Indian Continental Margins. The continental rifts that have been analysed are the East African Rift System, the Brazilian Continental Rift Systems and the European Cenozoic Rift System. It states how rifts and passive margins serve as valuable locations for hydrocarbon exploration. Tectonic inheritance/heritage examines the influence of pre-existing/pre-rift elements on the geometry, genesis and propagation of rift-related faults. Such elements include anisotropies in the shallow crustal levels, as well as the rheology of the lithosphere. Inheritance greatly influences the architecture of rifted passive margins including the attitude of faults and geometry of horsts, (half-) grabens, transfer zones etc. Inheritance is also a determining factor in the width of rifts and rift shoulder topography.
Author: E.R. Neumann
Publisher: Springer Science & Business Media
ISBN: 9400998031
Category : Science
Languages : en
Pages : 314
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Book Description
Proceedings of the NATO Advanced Study Institute, Oslo, Norway, July 27-August 5, 1977
Author: Albert Mathieson Quennell
Publisher: Van Nostrand Reinhold Company
ISBN:
Category : Science
Languages : en
Pages : 376
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Book Description
Author: P. Morgan
Publisher: Elsevier
ISBN: 1483289826
Category : Science
Languages : en
Pages : 685
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Book Description
Selected papers from the Lunar and Planetary Institute Topical Conference, St. Helena, CA, USA, 3-5 Dec. 1981
Author: I.B. Ramberg
Publisher: Springer Science & Business Media
ISBN: 9400998066
Category : Science
Languages : en
Pages : 444
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Book Description
Proceedings of the NATO Advanced Study Institute, Oslo, Norway, July 27-August 5, 1977
Author: Garry D. Karner
Publisher: Columbia University Press
ISBN: 9780231127387
Category : Nature
Languages : en
Pages : 376
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Book Description
Traditionally, investigations of the rheology and deformation of the lithosphere (the rigid or mechanically strong outer layer of the Earth, which contains the crust and the uppermost part of the mantle) have taken place at one scale in the laboratory and at an entirely different scale in the field. Laboratory experiments are generally restricted to centimeter-sized samples and day- or year-length times, while geological processes occur over tens to hundreds of kilometers and millions of years. The application of laboratory results to geological systems necessitates extensive extrapolation in both temporal and spatial scales, as well as a detailed understanding of the dominant physical mechanisms. The development of an understanding of large-scale processes requires an integrated approach. This book explores the current cutting-edge interdisciplinary research in lithospheric rheology and provides a broad summary of the rheology and deformation of the continental lithosphere in both extensional and compressional settings. Individual chapters explore contemporary research resulting from laboratory, observational, and theoretical experiments.
Author: Michal Nemčok
Publisher: Cambridge University Press
ISBN: 1107025834
Category : Science
Languages : en
Pages : 619
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Book Description
This is a comprehensive synthesis of state-of-the-art information on vitally important hydrocarbon habitats for advanced geology students and researchers, exploration geoscientists, and petroleum managers.
Author: A.V. Razvalyaev
Publisher: Routledge
ISBN: 1351458094
Category : Science
Languages : en
Pages : 212
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Book Description
Translation of the Russian edition of 1988 on peculiarities of the Arabian-Nubian Shield in the Precambrian, prerift magmatism in the Red Sea Rift zone, evolution of the crust in rift forming zones.
Author: Geological Society of London
Publisher: Geological Society of London
ISBN: 9781862390911
Category : Science
Languages : en
Pages : 598
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Book Description
Non-continental margins lack thick lavas that are generated as continental crust thins immediately prior to the onset of seafloor spreading. They may form up to 30 per cent of passive margins around the world. This volume contains papers examining an active margin, fossil margins that border present day oceans, and remnants of margins exposed today in the Alps. The papers present evidence across a range of scales, from individual mineral grains, through borelide cores and outcrop, to whole margins at the crustal scale.
