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Редактор(ы):Osborne D.
Издание:Woodhead Publishing Limited, 2013 г., 779 стр., ISBN: 78-0-85709-422-3
Язык(и)Английский
The coal handbook. Towards cleaner production / Справочник по углю. На пути к более чистому производству

There are few places in the developed world where the coal industry does not feel that it faces major challenges. Climate change, safety, and a variety of other environmental issues are just some of the concerns. In many cases, such concerns are justifi ed, and certainly in the developing world much more needs to be done to address them. Equally, the industry is working hard to respond. I know this to be true, after 25 years in the industry working with international organizations such as the World Coal Association and
Coal Industry Advisory Board of the International Energy Agency. These organisations, assisted by regional and other specialist industry bodies, as well as far-sighted coal companies, are all working constructively to improve the performance of the coal industry across a wide front. <...>

Автор(ы):Korbel P., Novak M.
Издание:Grange books, Praha, 2001 г., 299 стр., ISBN: 1-84013-404-6
Язык(и)Английский
The complete encyclopedia of minerals. Description of over 600 minerals from around the world / Полная энциклопедия минералов. Описание более 600 минералов со всего мира

The ever increasing number of publications about minerals reflects a growing interest in nature. Most of those publications though only deal with a few dozen of the most common minerals or gemstones. This book fills the gap by also featuring less common and rare minerals. The authors describe over 600 mineral species and varieties, illustrated with about 750 color photographs. In choosing illustrations of particular minerals, aesthetic criteria such as size of crystal and color played a role in addition to their importance and distribution in nature. This book includes some rare minerals, known only from one locality, because they form very attractive crystals or aggregates. There are minerals known to humankind since prehistoric times such as quartz and gold, but also minerals first described quite recently like rossmanite. The photographs show well-formed and colorful crystals but many-aggregates, which are more common in nature, are also included. The minerals in the book are listed according to the mincralogical system of Hugo Strunz, in his book Mineralogische Tabellen in 1978. The chemical formulae of individual minerals follow the form of Glossary of Mineral Species 1995 by M. Fleischer and J.A. Mandarine The information is complemented in both cases with the latest knowledge from scientific literature, such as new nomenclature of amphiboles, micas and zeolites. The mineral descriptions cover the basic physical and chemical data, including chemical formula and crystal system. The data provided correspond mainly to the end-members. The less common valence of the chemical elements is marked in the chemical formula (FeJ, Mn", As", Mn4", Pb'). Where an element features in both valences in the mineral, they are both marked (e.g. ilvaite, braunite).

Автор(ы):McDonough W.F., Sun S.-s.
Издание:1994 г., 31 стр.
Язык(и)Английский
The composition of the Earth / Состав Земли

Compositional models of the Earth are critically dependent on three main sources of information: the seismic profile of the Earth and its interpretation, comparisons between primitive meteorites and the solar nebula composition, and chemical and petrological models of peridotite-basalt melting relationships. Whereas a family of compositional models for the Earth are permissible based on these methods, the model that is most consistent with the seismological and geodynamic structure of the Earth comprises an upper and lower mantle of similar composition, an Fe-Ni core having between 5% and 15% of a low-atomic-weight element, and a mantle which, when compared to Cl carbonaceous chondrites, is depleted in Mg and Si relative to the refractory lithophile elements.

Редактор(ы):Войтеховский Ю.Л.
Издание:Кольский научный центр РАН, Апатиты, 2013 г., 56 стр., УДК: 552.311+553.491 (470.21)
Язык(и)Английский
The Cu-Ni-PGE and Cr deposits of the Monchegorsk area, Kola Peninsula, Russia. Guidebook for geological excursions / Месторождения Cu-Ni-МПГ и Cr в Мончегорском районе, Кольский полуостров, Россия. Путеводитель для геологических экскурсий

The geology, tectonics and stratigraphy of the Monchegorsk region (Kola Peninsula, Russia) is briefly described in the guidebook. The geological structure, ore localization and mineralogy of Cu-Ni-PGE and Cr occurrences in the major layered intrusions (Monchepluton, Imandra lopolith, Monchetundra intrusion) are presented in more detail.

Автор(ы):Anderson S.J., Harmon J.E.
Издание:John Wiley & Sons INC, 2003 г., 273 стр., ISBN: 0-471-20488-9
Язык(и)Английский
The design and implementation of geographic information systems / Разработка и внедрение географических информационных систем

IS is an extremely collaborative activity. Almost at the drop of a hat, GIS professionals will organize a conference, set up a Web-based list server, pull people together for discounts on training, establish a networking group, and generally do what they can to move the community forward.The standards for GIS certification in the United States, which are being worked out as we complete the manuscript for this book, explicitly include points for participating in and organizing events that benefit the entire community.

Издание:Pergamon Press, 1982 г., 412 стр.
Язык(и)Английский
The development potential of precambrian mineral deposits / Потенциал освоения докембрийских месторождений полезных ископаемых

It gives me great pleasure to bring the greetings and good wishes for the success of this meeting from the United Nations Under-Secretary-General for Technical Co-operation for Development, Mr. Bi Jilong, and it is my personal pleasure to respond to Academician Sidorenko is words of welcome.

Автор(ы):Garasic M.
Издание:Springer, 2021 г., 454 стр., ISBN: 978-3-030-80586-9
Язык(и)Английский
The Dinaric karst system of Croatia. Speleology and cave exploration / Динарская карстовая система Хорватии. Спелеология и исследование пещер

The Dinaric Karst of Croatia was formed in a tectonically active area, where several geotectonic plates of variable size are in direct contact. The African tectonic plate, with its smaller Adriatic plate, extends northwards towards the Alps. The Adriatic plate subducts under the Dinaric plate, which is the base part of the Dinaric Mountains. Therefore, this is a seismically palaeo and neotectonically active area with many earthquakes. Since these area is composed mainly of soluble carbonate rocks (mostly Mesozoic and Cenozoic ages) that are up to 8 km thick in this area, with favourable hydrogeological conditions, the karstification processes are very prominent. A brief overview of the geology of Croatia also indicates the complexity of hydrogeological processes in this area. <...>

Издание 2
Автор(ы):Trewartha G.T.
Издание:The University of Wisconsin Press, 1981 г., 383 стр., ISBN: 0-299-08230-Х
Язык(и)Английский
The Earth's problem climates / Проблема изменения климата на Земле
Автор(ы):Ghorbani M.
Издание:Springer, 2013 г., 580 стр., ISBN: 978-94-007-5624-3
Язык(и)Английский
The economic Geology of Iran. Mineral deposits and natural resources / Экономическая геология Ирана. Месторождения полезных ископаемых и минеральные ресурсы

 Iran is positioned on the southwest of Asia forming a bridge connecting three continents of Asia, Europe, and Africa. It is bordered by Azerbaijan, Armenia, Turkmenistan, and the Caspian Sea on the north, Afghanistan and Pakistan on the east, Oman Sea and Persian Gulf on the south, and Turkey and Iraq on the west (Road Atlas of Iran 2004 ) . The country is part of the Iranian Plateau that constitutes a vast and high terrane, which is bordered by the Caspian Sea on the north, Amu Darya, Syr Darya, and Kora River plains on the northeast, Sindh and Punjab Rivers plain on the southeast, the Oman Sea and the Persian Gulf on the south, and the Tigris river plain on the southwest (Comprehensive Geography of Iran 1987 ) <...>

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