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Редактор(ы):Knipe R.J., Rutter E.H.
Издание:The Geological Society of London, 1990 г., 553 стр., ISBN: 0-803317-58-3
Язык(и)Английский
Deformation Mechanisms, Rheology and Tectonics. Special publication / Механика деформация, реология и тектоника. Специальный выпуск

It is my great pleasure to introduce this volume dedicated to my long-standing colleague and friend, Henk Zwart; the more so since I missed the opportunity of addressing him on the occasion of his retirement from the chair of structural and applied geology in the State University at Utrecht in 1988.

Редактор(ы):Brun J.P., Cobbold P.R., Gapais D.
Издание:The Geological Society of London, 2005 г., 326 стр., ISBN: 1-86239-176-9
Язык(и)Английский
Deformation mechanisms, rheology and tectonics: from minerals to the lithosphere / Механизмы деформации, реология и тектоника: от минералов до литосферы

This volume is derived from the 13th meeting on Deformation Mechanisms, Rheology and Tectonics (DRT2003). The meeting was held in St Malo (Brittany, France) in April 2003, and organized by an informal group from Gdosciences Rennes (UMR 6118 CNRS, Rennes University), including Michel Ballbvre, St6phane Bonnet, Arlette Falaise, Olivier Galland, Fr6d6ric Gueydan, Charles Gumiaux, Benjamin Le Bayon, Alain-Herv6 Le Gall, Monique Le Moigne, Sylvie Schueller, and C61ine Tirel. It was sponsored by the Centre National de la Recherche Scientifique, Rennes University, the ity of Rennes, the Conseil G6n6ral d'Ille et Vilaine, and the R6gion Bretagne. Forty-eight reviewers have worked hard to improve the papers. We thank these persons and institutions for their contributions.

Редактор(ы):Prior D.J., Rutter E.H., Tatham D.J.
Издание:The Geological Society of London, 2001 г., 355 стр., ISBN: 978-1-86239-338-7
Язык(и)Английский
Deformation mechanisms, rheology and tectonics: Microstructures, mechanics and anisotropy / Механизм деформации, реология и тектоника: Микроструктуры, механика и анизотропия

Martin Casey, who died on the 10 June 2008 after a short illness, was a structural geologist of world renown. He led numerical approaches to understanding rock deformation and the development of tectonic structures, pioneering the quantitative analysis of rock fabrics, textures and folds. These researches now underpin diverse areas of geology, such as quantifying the strength of rocks in the crust which leads to calibrations of the seismic properties of the minerals in continents and the prediction of the fine-scale structure of hydrocarbon reservoirs. This Special Publication is dedicated to his memory not only for his fundamental contribution to science but also as a mentor, colleague and friend. <...>

Редактор(ы):Hambrey M.J., Hubbard B., Maltman A.J.
Издание:The Geological Society of London, 2000 г., 354 стр., ISBN: 1-86239-072-X
Язык(и)Английский
Deformation of glacial materials / Деформации ледников

The flow of glacier ice can produce structures that are striking and beautiful. Associated sediments, too, can develop spectacular deformation structures and examples are remarkably well preserved in Quaternary deposits. Although such features have long been recognized, they are now the subject of new attention from glaciologists and glacial geologists. However, these workers are not always fully aware of the methods for unravelling deformation structures evolved in recent years by structural geologists, who themselves may not be fully aware of the opportunities offered by glacial materials. This book, and the conference from which it stemmed, were conceived of as a step towards bridging this apparent gap between groups of workers with potentially overlapping interests.

Редактор(ы):Jones M.E., Preston M.F.
Издание:Blackwell science Ltd, 1987 г., 345 стр., ISBN: 0-632-01733-3
Язык(и)Английский
Deformation of sediments and sedimentary rocks / Деформация отложений и осадочных пород

In recognition of the increasing interest in the subject of deformation of sediments and sedimentary rocks shown by Earth scientists in recent years, a major international conference with this theme was held at University College London in April 1985. This volume contains the texts of those contributions to the Conference that were submitted for publication.

Редактор(ы):Butler R.W.H., Graham R.H., Ries A.C.
Издание:The Geological Society of London, 2007 г., 596 стр., ISBN: 978-1-86239-215-1
Язык(и)Английский
Deformation of the Continental Crust: The Legacy of Mike Coward / Деформация континентальной коры: наследие Mike Coward

This Special Publication celebrates the life and times of one of the late 20th century's most influential structural geologists, Mike Coward. At various times Mike was H H Read Professor of Geology at Imperial College, Chair of the UK Tectonic Studies Group and Council Member of the Geological Society of London; but these official titles belie a deeply unconventional man who loved to challenge accepted wisdom and dogma. Mike's career was an eclectic mix of pure and applied research in structural geology that straddled continents and geological time. Normal chronological narratives can hardly do justice to a man who could step from theme to theme at times, seemingly to colleagues, almost on a daily basis. This brief biography attempts to draw together some of the strands, in rather the same way as the Special Publication itself, to offer a glimpse of a character who could be very much larger than life. <...>

Автор(ы):Coleman J.M., Prior D.B.
Издание:AAPG, 1980 г., 171 стр.
Язык(и)Английский
Deltaic sand bodies / Песчаные дельтовые массивы

Deltaic depositional facies result from interacting dynamic physical processes (wave energy, tidal action, climate, etc.) which modify and disperse riverborne elastics. Since ancient times, river deltas have been of fundamental importance to civilization. Owing to their early significance as agricultural lands, deltas received considerable attention from scholars such as Homer, Herodotus, Plato, and Aristotle. More recently, subsurface deltaic facies have played a paramount role in accommodating the world's energy needs; ancient deltaic sediments have provided source beds and reservoirs for a large percentage of the known petroleum reserves. The facies relationships and mechanisms responsible for development and distribution of deltaic sand bodies must be understood before they can be explored efficiently. <...>

Редактор(ы):Pickering K.T., Whateley M.K.G.
Издание:The Geological Society of London, 1989 г., 358 стр., ISBN: 0-632-02385-6
Язык(и)Английский
Deltasю Sites and Traps for Fossil Fuels / Дельты. Площадки и ловушки для ископаемого топлива

Deltas, with their economic, political and scientific importance, have long fascinated and attracted Man's attention. The term 'delta' was coined by Herodotus in approximately 450 Bc for the triangular-shaped sedimentary body at the mouth of the River Nile. Today, the concept of a delta, its morphology and its controlling processes, are almost as numerous as the people who work on such systems.
This volume, of 23 papers on many aspects of modern and ancient deltaic sedimentary systems, will be useful to researchers as well as teachers and students alike. The well-balanced content of the book should prove particularly attractive.to those who seek a detailed state-of-the-science overview of this large and ever-expanding subject area. <...>

Редактор(ы):Fabbri A.G., Gaal G., McCammon R.B.
Издание:Springer, 2002 г., 532 стр., ISBN: 978-1-4020-0990-7
Язык(и)Английский
Deposit and geoenvironmental models for resource exploitation and environmental security / Модели месторождений и геоэкологические модели для изучения ресурсов и экологической безопасности

This volume contains the edited papers prepared by lecturers and participants of the NATO Advanced Study Institute (ASI) on "Deposit and Geoenvironmental Deposit Models for Resource Exploitation and Environmental Security" held in Matrahaza, Hungary, September 6-19, 1998.

Выпуск 93
Издание:Economic geology, 1998 г., 15 стр.
Язык(и)Английский
Deposition of gold in carlin-type deposits: the role of sulfidation and decarbonation at Twin Creeks, Nevada

We report here an investigation of the distribution of Au, As, Sb, Hg, carbonates, K-Al silicates, and pyrite in the Twin Creeks Carlin-type gold deposit. The main objective of the study was to determine the nature and degree of correlation among these variables and use them to identify the process(es) that deposited gold. The study focused on deposit-scale variations in these parameters and was based, in part, on data from two large geochemical databases that were prepared by mine staff.

Country rocks at Twin Creeks include Ordovician-age interlayered calcareous shales and mafic igneous rocks, the overlying Leviathan allochthon, and the Pennsylvanian-Permian Etchart Formation that was deposited unconformably over these rocks. Most gold values are found in calcareous shales in the Ordovician sequence and in limestones in the Etchart Formation, although not all layers contain the same amount of gold. Strongest gold mineralization is not adjacent to faults but its general form and distribution suggest that gold-bearing solutions gained access to favorable layers along the faults. In the Ordovician sequence, gold values are highest in shales that have undergone maximum dissolution of carbonate minerals. Petrographic study shows that some gold is associated with adularia, but deposit-scale comparisons do not show a consistent relation between K/Al ratios and gold values. The distribution of antimony is similar to that of gold, whereas mercury is more concentrated than gold, and arsenic is more widely dispersed than gold.

The relation between gold, iron, and sulfide sulfur values shows that mineralization is concentrated in rocks that have gained sulfur, but not iron, to form gold-bearing arsenian pyrite. Thus, these rocks have undergone sulfidation rather than pyritization. The iron that underwent sulfidation came largely from preore, diagenetic(P) ferroan dolomite and was released into solution by decarbonation, a common form of alteration associated with Carlin-type deposits. The results of this study suggest that wall-rock iron content and decarbonation processes which liberate this iron are the most important factors controlling formation of Carlin-type gold deposits. New deposits should be sought where stratigraphic units containing abundant ferroan dolomite are cut by favorable structures.

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