The Continental Permain in Central, West, and South Europe
The Continental Permain in Central, West, and South Europe

Author: H. Falke

Publisher: Springer Science & Business Media

Published: 1976-08-31

Total Pages: 370

ISBN-13: 9789027706645

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Geological research on the continental Permian in West Central and South Europe has been neglected in l l former days. Nevertheless, interest in it increased in the last twenty years and became important owing to the problems connected with continental sedimentation and also because of the important discoveries of oill gas and uranium deposits. Therefore, detailed inves l tigations in all countries where continental Permian appears have been made with the help of boreholes. These investigations included sedimentation basins in which the above-mentioned deposits are not expected. Consequently, the numerous results received in connec tion with still unanswered questions led to the idea to invite the specialists to a meeting. The first meeting was held in Pisa 1966 and a further one in 1 Vienna 1969. Both conferences exclusively dealed with the deposits of the Verrucano province, both in the Alps and Apennines. With respect to the importance of such meetings a further one was intended to be arranged in Mainz dealing with the whole continental Permian in West Central, and South Europe. With financial help l of the,NATO Scientific Affairs Division this meeting could be arranged as a NATO Advanced Study Institute.

Eolian Sediments and Processes
Eolian Sediments and Processes

Author: M.E. Brookfield

Publisher: Elsevier

Published: 2000-04-01

Total Pages: 671

ISBN-13: 0080869521

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Papers cover the entire spectrum of eolian investigations, ranging from the microscopic level to regional synthesis as well as ancient eolian deposits and their interpretation.

Geology of Gas and Oil under the Netherlands
Geology of Gas and Oil under the Netherlands

Author: H.E. Rondeel

Publisher: Springer Science & Business Media

Published: 2012-12-06

Total Pages: 322

ISBN-13: 9400901216

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Contains 21 papers on the petroleum geology of the Netherlands, combining work by the industry, the Geological Survey and universities. The wide range of topics presented includes reservoir characterization through 3D seismic and borehole log evaluation of single oil and gas fields, as well as reviews of the hydrocarbon habitat in the West Netherlands Basin and of the regional Rotliegend facies distribution. Published in association with the Royal Geological and Mining Society of the Netherlands (KNGMG), which hosted the 1993 International Conference in the Hague of the American Association of Petroleum Geologists. The papers were prepared for this conference. Audience: Staff engaged in hydrocarbon exploration and production in the North Sea area. Others who need to know about the results of this exploration and production in the Netherlands.

The Carboniferous Timescale
The Carboniferous Timescale

Author: S.G. Lucas

Publisher: Geological Society of London

Published: 2022-04-26

Total Pages: 1012

ISBN-13: 1786205424

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The print edition is published as 2 hardback volumes, parts A and B, and sold as a set. The Carboniferous was the time of the assembly of Pangaea by the collision of the Gondwanan and Larussian supercontinents, and the principal interval of the late Paleozoic ice ages. These tectonic and climatic events caused dramatic sea-level fluctuations and climate changes and produced a Carboniferous world that was diverse topographically and climatologically, perhaps only rivalled in that diversity by the late Cenozoic world. Furthermore, the Carboniferous was a time of the accumulation of vast coal deposits of great economic and societal significance. The temporal ordering of geological and biotic events during Carboniferous time thus is critical to the interpretation of some unique and pivotal events in Earth history. This temporal ordering is based on the Carboniferous timescale, which has been developed and refined for nearly two centuries. This book reviews the history of the development of the Carboniferous chronostratigraphic scale and includes comprehensive analyses of Carboniferous radioisotopic ages, magnetostratigraphy, isotope-based correlations, cyclostratigraphy and timescale-relevant marine and non-marine biostratigraphy and biochronology.

The British Seas
The British Seas

Author: Jack Hardisty

Publisher: Taylor & Francis

Published: 2024-04-03

Total Pages: 289

ISBN-13: 1040014739

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Originally published in 1990 and designed as a student text, The British Seas is a clear introduction to the oceanography and resources of the region. It is unique in providing a detailed review of the resources of the north-west European continental shelf together with a comprehensive description of the environment. Introducing the shelf region as if it were a new country, Jack Hardisty explores first its physical environment and then summarizes the distribution and exploitation of resources from the environment. Part 1 – on the oceanography - covers the shape of the shelf, its geological history and its wave and tidal regimes. Part 2 – on the resources – looks at trade and shipping, and the hydrocarbon, fishing and seabed mining industries. It goes on to discuss wave and tidal power, and to consider the problem of pollution in terms of resource utilization. The industrial technology and the environmental potential of each resource are examined, and the economic and legislative restrictions are analysed.

The Permian of Northern Pangea
The Permian of Northern Pangea

Author: Peter A. Scholle

Publisher: Springer Science & Business Media

Published: 2012-12-06

Total Pages: 263

ISBN-13: 364278593X

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The Permian was a remarkable time period. It represents the maximum stage of Pangean continental assembly, includes a major global climatic shift from glacial to nonglacial conditions (icehouse-greenhouse transition), and is ter minated by one of the most profound faunal/floral extinction events in the Earth's history. In addition, Permian oceans, although poorly understood, must have had some quite unique characteristics. Permian seas reached the most extreme values of carbon, sulfur, and strontium isotopic ratios ever achieved in Phanerozoic time, and the isotopic ratios of all three elements abruptly returned to more "normal" values at, or very close to, the Permo Triassic boundary. Finally, the Permian is marked by an abundance of important sedimentary mineral resources. It has large fossil fuel concentra tions (coal, oil, and natural gas), enormous phosphate reserves, and very extensive evaporite deposits, including gypsum, anhydrite, and halite, as well as a variety of potash salts. Study of the Permian has been hampered, however, by a number of factors. These include a scattered geologic literature (presented in a variety of languages), a confusing regional and global stratigraphic framework (based, in part, on inadequate type sections), and largely provincial, often poorly correlatable faunas. All have contributed to the sparsity and inadequacy of overviews of this critical geological interval. The two volumes attempts to bring together some of the widely scattered observations about these fascinating rocks, at least for the northern (pre dominantly nonglacial) parts of Pangea.

Pre-Mesozoic Geology in the Alps
Pre-Mesozoic Geology in the Alps

Author: J.F.v. Raumer

Publisher: Springer Science & Business Media

Published: 2012-12-06

Total Pages: 1001

ISBN-13: 3642846408

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The Alps are an arched mountain chain stretching 1500 km between Vienna and Graz in Austria and Genova in Italy. They resulted from the collision of the African and Laurasian plates during Mesozoic and Tertiary times. The high standard of knowledge attained over the last 30 years by the working groups on "Alpine Metamorphism" is well known and helped considerably to recognize pre-Mesozoic elements in the Alps. In Part I of this book the subdivision of the major Alpine units and pre-Mesozoic pal inspastic reconstructions are covered before discussion of the pre-Mesozoic geology in Parts II, III and IV It is understood that the Mesozoic and later events overprinted pre-existing structures veiling the earlier history and the nature of protoliths. Although the Alpine overprint does not facilitate the recognition of older struc tures, pre-Mesozoic basement units were recognized during the first beginnings of geological observations in the Alps, about 200 years ago. Fifty percent of the Alpine domain is underlain by basement units that have been unconformably covered since Permian and Mesozoic times. This basement appears today in a complex pattern among the Alpine structures. The history of their discovery and explanation, parallel with a growing sophistication of research methods, are the subject of the introductory chapter of Part II.