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

Поиск по книгам
Автор(ы):Papanikolaou D.I.
Издание:Springer, 2021 г., 388 стр., ISBN: 978-3-030-60730-2
Язык(и)Английский
The geology of Greece / Геология Греции

The Geology of Greece was my major teaching responsibility and research focus for about 40 years in the Department of Geology at the National and Kapodistrian University of Athens. My first book regarding the Geology of Greece published in 1986 (Eptalofos Publ. Co., Athens, 240 p., in greek) was focused in assisting the students of Geology to refine the basic aspects about the geology of Greece, incorporating the «theoretical» part together with the description of the geological formations and the overall geodynamic and paleogeographic evolution. It should be noted that the Geology of Greece is a complex and rather challenging task, incorporating a Late Paleozoic—Early Cenozoic orogenic history of a Tethyan segment and an active subduction and orogenic arc in the Eastern Mediterranean.

Редактор(ы):Oliveira J.T., Quesada C.
Издание:Springer, 2019 г., 559 стр., ISBN: 978-3-030-10518-1
Язык(и)Английский
The geology of Iberia: A geodynamic approach. Volume 2: The variscan cycle / Геология Иберии (Испании): геодинамический подход. Том 2: Варисциды (герциниды)

The geology of the Iberian Peninsula and its continental shelves is complex and varied despite its relatively small size. With some 590,000 km2 inland (Iberian Peninsula, the Balearic and other small Atlantic and Mediterranean islands) and some additional 200,000 km2 making up the continental shelves, the record exposed spans for nearly the last 600 Ma of Earth’s history. The geological record is not only long but also deep: from surficial to upper mantle, segments are exposed both inland and under the sea.

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 / Геология медно-цинкового месторождения Антамина, Перу, Южная Америка

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.

937.3