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Издание:British Geological Survey, 1999 г., 6 стр.
Язык(и)Английский
Minerals in Britain. Past production...  Future potential. Gemstones / Полезные ископаемые в Великобритании. Добыча в прошлом... Потенциал в будущем. Драгоценные камни

Although Britain is a major gemstone trader, it currently produces little from indigenous sources. There are, however, records of a wide variety of gem material, particularly in Scotland. In addition to sapphire, ruby and possible diamond, the country has yielded topaz, beryl, and many varieties of semi-precious stones including cairngorm, amethyst, garnet, tourmaline, agate, zircon, ‘Blue John’ flourite and jet. There is also an unconfirmed report of Scottish emerald. Most of these gemstones were found by amateur geologists and gemmologists but recent discoveries, particularly of iamond indicator minerals in Scandinavia and Ireland, have raised commercial interest in the potential of Britain as a source of precious stones. <...>0

Редактор(ы):Szakall S.
Издание:Granit, Prague, 2002 г., 480 стр., ISBN: 80-7296-014-8
Язык(и)Английский
Minerals of the Carpathians / Минералы Карпат

Geologically, the Carpathian Range is the continuation of the Eastern Alps towards the East forming an arching bow-shaped mountain chain of 1,500 km in length that extends through several countries, (i.e. the Czech Republic. Slovakia, Poland. Hungary, Ukraine, and Romania). From a mineralogical viewpoint, the Carpathians, with its more than 1,000 mineral species, is an extremely interesting area. Its geological formations vary in ages and compositions. The structural evolution is highly complicated. It has also been a traditional mining area since prehistoric times. More than fifty valid mineral species were first described from this region (karpatite. koktaite, libethenite, native tellurium, pilsenite, rozenite. rhodochrosite.  etc.). Some very rare species, originally discovered in other parts of the world, also occur here (cymrite, hetaerolite. nambulite, segnitite, capgaronnite, etc.). <...>

Редактор(ы):Putirka K.D., Tepley F.J.
Издание:2008 г., 677 стр.
Язык(и)Английский
Minerals, inclusions and volcanic processes / Вулканические минералы, включения и процессы

Minerals are intrinsically resistant to the processes that homogenize silicate liquids—their compositions thus yield an archive of volcanic and magmatic processes that are invisible at the whole rock scale. Minerals and their inclusions record diverse magma compositions, the depths and temperatures of magma storage, the nature of open system processes, and the rates at which magmas ascend.

Издание:The Hamlyn Publishing Group Limited, 1980 г., 320 стр.
Язык(и)Английский
Minerals, rocks and fossils / Минералы, горные породы и ископаемые остатки

This field guide is divided into three sections, namely minerals, rocks (including meteorites and tektites) and fossils. Each section comprises an introductory part, which is illustrated by line drawings, and a descriptive part, which is illustrated by line drawings and colour photographs. The introductory sections include the minimum basic information required to follow the descriptive sections adequately, while the descriptive sections, for ease of reference, are always arranged so that photographs and accompanying text are opposite one another.

Автор(ы):Wenk H.-R., Булах А.Г.
Издание:Cambridge University Press, 2003 г., 671 стр., ISBN: 978-0-521-82238-1
Язык(и)Английский
Minerals. Their constitution and origin / Минералы. Их строение и происхождение

Minerals: Their Constitution and Origin is an introduction to mineralogy for undergraduate and graduate students in the fields of geology, materials science, and environmental science. It has been designed as a textbook for use on a semester course and covers all aspects of mineralogy in a thoroughly modern and integrated way.

Редактор(ы):Мщенфлщм Ыюб Лшыудумф Вюб Пкщлрщмылн Мюб Ысрфзщмф Ню
Издание:Springer, 2020 г., 288 стр., ISBN: 978-3-030-00924-3
Язык(и)Английский
Minerals: structure, properties, methods of investigation / Минералы: структура, свойства, методы исследования

Zoned Olivines of Bronze Age Metallurgical Slags of Southern Urals According to LA-ICP-MS Mapping Maxim N. Ankushev, Dmitry A. Artemyev and Ivan A. Blinov

Modern Urban Sediments: Identification of the Cosmic Spherules Irina A. Danilenko, Elena M. Baglaeva, Evgeniya V. Petrova, Andrian A. Seleznev and Grigoriy A. Yakovlev

Zircon Thermometry of the Yarot Granite Massif (The Subpolar Urals) Yulia V. Denisova and Anna N. Vikhot
New Carbonaceous Chondrite from Northwest Africa Kseniya A. Dugushkina and Stepan V. Berzin Scanning Electron Microscopy of Pyrite from Brown Coal (Mugun Coal Deposit, Irkutsk Basin)
Narine R. Dzhumayan and Aleksey V. Nastavkin Dimensions of Atoms in a Crystal: Delusions Versus Reality Nikolai N. Eremin

Редактор(ы):D'Arco P., Silvi B.
Издание:Kluwer Academic Publishers, 2002 г., 351 стр., ISBN: 0-306-46933-2
Язык(и)Английский
Modeling of minerals and silicated materials / Моделирование минералов и силикатных материалов

The Structural Properties of Silica Using Classical and Quantum Interatomic Forces

High Pressure Studies of Mantle Minerals by Ab initio Variable Cell Shape Molecular Dynamics

Calculation of Mineral Properties with the Electron Gas Model

Издание 2
Автор(ы):Gaft M., Pznczer G., Reisfeld R.
Издание:Springer, 2015 г., 619 стр., ISBN: 978-3-319-24763-2
Язык(и)Английский
Modern luminescence spectroscopy of minerals and materials / Современная люминесцентная спектроскопия минералов и материалов

Spectroscopy is the study of the interaction of electromagnetic radiation with the matter. There are three aspects of the spectroscopic measurement: irradiation of a sample with electromagnetic radiation; measurement of the absorption, spontaneous emission and scattering (Rayleigh elastic scattering, Raman inelastic scattering) from the sample; and analysis and interpretation of these measurements. The main subject of our book is spontaneous luminescence of natural minerals. We have used the term luminescence, which is the general term of the phenomenon. Luminescence may be subdivided to the fast fluorescence with spin-allowed transition and slow phosphorescence with spin-forbidden transition. Afterglow may be added, which is related to emission after trapping of an electron elsewhere. <...>

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