Добрый день, Коллеги. Важное сообщение, просьба принять участие. Музей Ферсмана ищет помощь для реставрационных работ в помещении. Подробности по ссылке

Поиск по книгам
Редактор(ы):El-Barkooky A., El-Rahman Y.A., Frias J.M., Fritz H., Hamimi Z.
Издание:Springer, 2020 г., 725 стр., ISBN: 978-3-030-15264-2
Язык(и)Английский
The Geology of Egypt / Геология Египта

The passion to understand the Geology of Egypt could be traced back to 1150 BC. In this year, the oldest geological map in the world was prepared to illustrate the geology of the Hammamat-Fawakhir area in the central part of the Eastern Desert of Egypt.

Издание 4
Автор(ы):Miall A.D.
Издание:Springer, Berlin, 2006 г., 586 стр., ISBN: 978-3-642-08211-5
Язык(и)Английский
The geology of fluvial deposits. Sedimentary facies, basin analysis, and petroleum geology / Геология речных отложений. Осадочные фации, бассейновый анализ, нефтегазовая геология

Fluvial deposits represent the preserved record of one of the major nonmarine environments. They accumulate in large and small intermontane valleys, in the broad valleys of trunk rivers, in the wedges of alluvial fans flanking areas of uplift, in the outwash plains fronting melting glaciers, and in coastal plains. The nature of alluvial assemblages - their lithofacies composition, vertical stratigraphic record, and architecture - reflect an interplay of many processes, from the wandering of individual channels across a floodplain, to the long-term effects of uplift and subsidence. Fluvial deposits are a sensitive indicator of tectonic processes, and also carry subtle signatures of the climate at the time of deposition. They are the hosts for many petroleum and mineral deposits. This book is about all these subjects.

Автор(ы):Ghorbani M.
Издание:Springer, 2021 г., 450 стр., ISBN: 978-3-030-71108-5
Язык(и)Английский
The geology of Iran: tectonic, magmatism and metamorphism / Геология Ирана: тектоника, магматизм и метаморфизм

The beginning of any scientific, economic, investigational, and executive achievement depends on the proper knowledge of basic information. The application of geosciences to meet the needs of each country is related to the level of knowledge of the geologists.

Редактор(ы):Abd el-aziz Khairy Abd el-aal, Ali Al-Dousari, Jasem Mohammed Al-Awadhi
Издание:Springer, 2023 г., 249 стр., ISBN: 978-3-031-16726-3
Язык(и)Английский
The Geology of Kuwait / Геология Кувейта

This chapter represents a comprehensive review of Kuwait’s surface geology and stratigraphy from previous works accomplished by numerous geoscience researchers in the past decades. The surface of Kuwait is characterized by nearly flat topography, featureless to gently undulating, apart from a few tens of meters of escarpments in the north and south, and flat low to moderately elevated hills and ridges.

Редактор(ы):Salvador A.
Издание:The Geological Society of America, 1991 г., 577 стр., ISBN: 0-8137-5216-7
Язык(и)Английский
The geology of North America. Volume J. The gulf of Mexico basin / Геология Северной Америки. Том J. Залив Мексиканского бассейна

The Geology of North America series has been prepared to mark the Centennial of The Geological Society of America. It represents the cooperative efforts of more than 1,000 individuals from academia, state and federal agencies of many countries, and industry to prepare syntheses that are as current and authoritative as possible about the geology of the North American continent and adjacent oceanic regions.

Том 1-2
Издание:London, 1845 г.
Язык(и)Английский
The geology of Russia in Europe and the Ural mountains. Vol 1-2 / Геология России в Европе и Уральских горах. Том 1-2

ALTHOUGH the physical geography, mineralogy and natural history of the distant and mountainous parts of Russia have been well illustrated, from the days of Pallas and Hermann to those of Humboldt and Rose, the true geological structure of the country, particularly of her great flat regions, has never yet been adequately developed. We need not now enumerate all those persons who have recently offered contributions towards this object;

Связанные материалы:
Издание 2
Автор(ы):Miall A.D.
Издание:Springer, 2010 г., 531 стр., ISBN: 978-3-642-05026-8
Язык(и)Английский
The geology of stratigraphic sequences / Геология стратифированных толщ

The first chapter of the book provides some essential historical background to the modern story of sequence stratigraphy. The history of the study of stratigraphy includes two parallel but largely independent strands of research that have been underway since at least the early twentieth century. They are characterized by some profound differences in underlying principles, references and research methods, one research method being essentially empirical and inductive in approach, while another groups of researchers has attempted to develop deductive, theoretical models for understanding Earth history. Chapter 1 is based largely on four papers which explored this history (Miall and Miall, 2001, 2002, 2004; Miall, 2004). It is to be hoped that readers will not skip this chapter, because experience suggests that students of geology do not learn enough about the history, philosophy, or methodology of their science.<...>

Автор(ы):Harland W.B.
Издание:The Geological Society of London, 1997 г., 538 стр., ISBN: 1-897799-93-4
Язык(и)Английский
The Geology of Svalbard / Геология Шпицбергена

This work attempts to present the geology of Svalbard in some detail, arranged systematically as a definitive study and so reflecting the present conjuncture of research. It may thus meet the needs of specialists with information on related fields or of any geoscientist wanting an indication of what is known about this key region. Spitsbergen (peaked mountains), the name earlier referred to the whole archipelago. It is now replaced by the name Svalbard (cold coasts), within which Spitsbergen is the principal landmass. Spitsbergen alone is about the size of Switzerland and the whole archipelago a little less than the area of Scotland.

Автор(ы):Lipten E.J., Smith S.W.
Издание:PGS Publishing, Linden Park, 2005 г., 15 стр.
Язык(и)Английский
The Geology of the Antamina Copper-Zinc Deposit, Peru, South America

Antamina is the largest known copper-zinc skarn (>3000 Mt @ 1.1% Cu and 1.3% Zinc) in the world. It is located in the Northern Andes in Peru, 270 km north of Lima. The deposit formed at approximately 10 Ma by the emplacement of quartz monzonite intrusions into Mid to Late Cretaceous limestones of the Celendin and Jumasha Formations. Mineralisation is hosted as a series of zoned green and brown garnet endoskarns and exoskarns in the form of chalcopyrite, bornite and sphalerite. Elements present within the deposit of significant quantities to affect concentrate value are Cu, Zn, Mo, Ag, Bi and Pb. Antamina produces four concentrates, namely, copper (chalcopyrite and bornite), zinc (sphalerite), molybdenum and lead-silver-bismuth.

Редактор(ы):Abdelsalam M.G., Collins A., El-Wahed M.A., Fowler A.-R., Hamimi Z., Liegeois J.-P.
Издание:Springer, 2021 г., 785 стр., ISBN: 978-3-030-72994-3
Язык(и)Английский
The geology of the Arabian-Nubian shield / Геология Аравийско-Нубийского щита

The Arabian–Nubian Shield (ANS) is a vast and exceptionally well-preserved expanse of crust and underlying sub-continental lithospheric mantle that was largely produced during the Neoproterozoic, with only restricted contribution from older lithospheric components, except in the extreme north-eastern part of the shield. With an exposed area of nearly 2 million km², and an additional 1 million km² buried beneath the great Cenozoic East African Rift System and its associated volcanic rocks, the shield represents one of the best-preserved Neoproterozoic orogenic belts on the planet and the largest preserved expanse of new Neoproterozoic lithosphere in Earth’s geological history.

722.32