Precambrian Banded-Iron-Formations

Precambrian Banded-Iron-Formations
Author: Y.P. Mel'nik
Publisher: Elsevier
Total Pages: 323
Release: 1982-01-01
Genre: Science
ISBN: 0080869041

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Precambrian Banded-Iron-Formations

Precambrian Banded Iron-formations

Precambrian Banded Iron-formations
Author: I︠U︡. P. Melʹnyk
Publisher:
Total Pages: 310
Release: 1982
Genre: Geology, Stratigraphic
ISBN: 9780444419347

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Ancient Banded Iron Formations

Ancient Banded Iron Formations
Author: J. J. Chauvel
Publisher:
Total Pages: 480
Release: 1990
Genre: Formations (Geology)
ISBN:

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Precambrian Iron-formations

Precambrian Iron-formations
Author: Peter W. Uitterdijk Appel
Publisher:
Total Pages: 696
Release: 1987
Genre: Geology, Stratigraphic
ISBN:

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Iron-Formation: Facts and Problems

Iron-Formation: Facts and Problems
Author: A.F. Trendall
Publisher: Elsevier
Total Pages: 559
Release: 2000-04-01
Genre: Science
ISBN: 008086905X

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Iron-Formation: Facts and Problems

Banded Iron Formations to Iron Ore

Banded Iron Formations to Iron Ore
Author: Desmond Fitzgerald Lascelles
Publisher: Nova Science Publishers
Total Pages: 0
Release: 2017-06
Genre: Iron
ISBN: 9781536109719

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From the first attempts to understand the origin of giant iron ore deposits, numerous false assumptions have been used as the basis of genesis models that have become standard and unquestioned, with later research generally seeking to find evidence supporting the existing models and ignoring contrary evidence. Many models were constructed based on extremely rare features, and their absence in the global abundance of iron formations was not considered important since there was no understanding of the major sedimentary structures, i.e. laminations and banding. Inconsistencies within the hypothetical models are either ignored or excused by proposing special circumstances, but no one considers that the models might be wrong or have only limited application. Many hypotheses regarding Earths history have been postulated from the difference between Phanerozoic and Precambrian iron-formations. In particular, the development of an oxygenated atmosphere has been deduced from the supposed evolution of iron-formations. The subject has provided a fertile field for research and models of Earths history, but without clear knowledge of the sedimentation, diagenesis and metamorphism of BIFs (branded iron formations), such models are speculative or even irrelevant. Since these models on the genesis and distribution of BIF were used as proxies to answer questions regarding the composition of the early oceans and atmosphere, weathering and transport conditions on early land surface, volcanism and continental development in the Archean eon, and as they affect exploration for the largest volume and most basic of industrial metals, they have an importance beyond academic sedimentary and stratigraphic interest. The aim of this book is to present a model for the origin of BIFs and derived high-grade iron ore deposits with global applications that are still subject to correction and change as new information becomes available and are free of illogical assumptions which do not conflict with either field observations or basic chemistry and physics.

Precambrian Sedimentary Environments

Precambrian Sedimentary Environments
Author: Wladyslaw Altermann
Publisher: Blackwell Publishing
Total Pages: 450
Release: 2002-03-12
Genre: Science
ISBN: 9780632064151

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The motivation for this volume came from the idea that the Precambrian is the key, both to the present, and to the understanding of the Earth as a whole. The Precambrian constitutes about 85% of Earth's history, and of that, about 3.75 billion years of Precambrian time, represented by rocks, are accessible to geoscientists. Ancient atmospheric and environmental conditions can be traced back to the time when the Earth was only about 250 million years old. Precambrian rocks supply almost 75% of important mineral resources such as Fe, Mn, Au, Pt and Cr. Many of these elements are associated with sedimentary rocks and some important hydrocarbon, coal and graphite deposits are also hosted by Precambrian rocks. This volume is aimed at geoscientists interested in Precambrian sedimentary rocks and at students of Earth history. It contains review articles discussing Precambrian conditions and case studies from Precambrian shields and successions of North and South America, Australia, Africa, Europe, Asia and India. The introductory papers, written by experts on Precambrian environments, treat comprehensively the application of actualism to the Precambrian, the evolution and influence of life on the sedimentary rock record, the genesis of Banded Iron Formations, the Precambrian sulphur cycle and the significance of Precambrian chemical carbonate precipitates. The case studies include depositional settings and processes in Archean terranes, in Paleoproterozoic sequences, with some emphasis on the lack of vegetation and weathering, and in late Proterozoic sequences, with some emphasis on glacial deposits. The contributions demonstrate that Precambrian sedimentary deposits are commonly similar to their Phanerozoic counterparts in terms of composition, sedimentary processes, and depositional setting, but may differ significantly as a result of lack of vegetation, climatic and biological constraints, composition and circulation of seawater, and the secular involvement of continental crust. Contains review articles discussing Precambrian conditions and case studies from Precambrian shields and successions of North and South America, Australia, Africa, Europe, Asia and India. The introductory papers, written by experts on Precambrian environments, treat comprehensively the application of actualism to the Precambrian, the evolution and influence of life on the sedimentary rock record, the genesis of Banded Iron Formations, the Precambrian sulphur cycle and the significance of Precambrian chemical carbonate precipitates. Detailed case studies include depositional settings and processes in Archean terranes, in Paleoproterozoic sequences, with some emphasis on the lack of vegetation and weathering, and in late Proterozoic sequences, with some emphasis on glacial deposits. Written for geoscientists interested in Precambrian sedimentary rocks and students of Earth history. If you are a member of the International Association of Sedimentologists (IAS), for purchasing details, please see: http://www.iasnet.org/publications/details.asp?code=SP33

Phanerozoic Ironstones

Phanerozoic Ironstones
Author: Timothy Peter Young
Publisher: Geological Society Publishing House
Total Pages: 290
Release: 1989
Genre: Science
ISBN:

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