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Поиск по книгам
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.

Автор(ы):Pollard L.D., Weaver C.
Издание:Elsevier, 1973 г., 221 стр., ISBN: 0-444-41043-0
Язык(и)Английский
Developments in sedimentology. Volume 15. The chemistry of clay minerals / Исследования в седиментологии. Том 15. Химия глинистых минералов

Clay minerals occur in all types of sediments and sedimentary rocks and are a common constituent of hydrothermal deposits. They are the most abundant minerals in sedimentary rocks perhaps comprising as much as 40% of the minerals in these rocks. Half or more of the clay minerals in the earth's crust are illites, followed, in order of relative abundance, by montmorillonite and mixed-layer illite-montmorillonite, chlorite and mixed-layer chlorite-montmorillonite, kaolinite and septachlorite, attapulgite and sepiolite. The clay minerals are fine-grained. They are built up of tetrahedrally (Si, A l , Fe3+) and octahedrally (Al, Fe3+, Fez+, Mg) coordinated cations organized to form either sheets or chains. All are hydrous. <...>

Издание:Debeersgroup, 31 стр.
Язык(и)Английский
Diamond Geology

Diamond deposits can be classified as primary (kimberlites and lamproites) and secondary (alluvial and marine). In 1995, their relative production contributions in South Africa were, primary (kimberlite) 8.63 million carats (89% of total), alluvial 960,000 carats (10%). and marine 90.000 carats (1%). The percentage of gems in kimberlites is highly variable. Published figures suggest approximately 40% for the Kimberley mines and 55% for Premier mine. The proportion of gems in the West Coast marine deposits is over 98%. The MIBA mine in the Congo and the Argyle mine in Australia have an average gem content of only 5%. The dispersal of diamonds from their primary sources into streams and rivers and ultimately to the sea is generally accompanied by an increase in average value per carat.| as flawed stones are progressively destroyed with greater and greater transport.

Источник:www.debeersgroup.com
Издание 2
Автор(ы):Manutchehr-Danai M.
Издание:Springer, 2005 г., 887 стр., ISBN: 3-540-23970-7
Язык(и)Английский
Dictionary of gems and gemology / Словарь драгоценных минералов и геммологии

The worldwide acceptance of the first edition of this book encouraged me to extensively revise and extend the second edition. The book was of value to readers of widely ranging interests as demonstrated by the letters received from scientists, students, mining engineers, editors of periodical papers and teachers.

This revision comes five years after the publication of the first edition. Many entries have been improved and now include new data. In total it includes about 25 000 entries, 1 500 graphic figures and 42 tables.

The first edition was criticized by readers who felt that some entries were not related to respective materials: but I would like to emphasize that many minerals are described in the form of references necessary for determining other gemstone materials.

In this edition chapters on light, color and colorant are dealt with in more depth, a large section introduces new terms applying to these areas.

If you have criticisms or suggestions please feel free to contact the author.

Издание 3
Автор(ы):Manutchehr-Danai M.
Издание:Springer, Verlag - Berlin - Heidelberg - New York, 2009 г., 1028 стр., ISBN: 978-3-540-72795-8
Язык(и)Английский
Dictionary of gems and gemology / Словарь драгоценных минералов и геммологии

This revision (third edition) is being published 4 years after the publication of the second edition. Many entries have been improved and circa 500 new terms have been added. It includes more than 27,000 entries, 1,500 graphic figures, and nearly 50 tables. New entries include notable sapphires (comprising blue sapphires, sapphires of other colors, engraved or carved sapphires), notable rubies (engraved or carved rubies), and corundums.

If you have criticism or suggestions, please feel free to contact the author.

Выпуск 29
Издание:Christian Weise Verlag Germany, Munich, 99 стр., ISBN: 0945-8492
Язык(и)Немецкий
Die schonsten mineralien. Rublands

Wer Steine sammelt, möchte am liebsten den ganzen Planeten bereisen. Jeder Flecken Erde kann interessant sein. Für echte Mineralien- und Edelsteinsammler gibt es deshalb keine Grenzen, schon gar keine politischen. Sinnvoll ist vielleicht eine Grenze, die zwischen Kalkgesteinen und Graniten verläuft: Auf der einen Seite findet man ein paar kleine Calcite, jenseits der Grenze aber winken herrliche Topase, Berylle, Apatite und Turmaline. Doch weil wir Menschen sind, erfinden wir eben auch unsinnige Grenzen, zum Beispiel jene zwischen Ost und West. Auch wenn Deutschland nicht so extrem im „Westen" liegt wie Amerika, und Rußland nicht so extrem im ..Osten" wie China, so empfinden wir im deutsch-russischen Verhältnis doch eine Art Ost-West-Konflikt. Die Ursachen dafür sind jüngeren Datums, und wer zwei- bis dreihundert Jahre zurückblickt, entdeckt, daß die Sammlerherzen älterer Zeiten weit verzweigte und fruchtbare Freundschaftsbande geknüpft und gepflegt haben.

Westliche Fürsten und östliche Zaren tauschten nicht nur Waren, Kunst und Technik miteinander aus, sie förderten auch den Ost-West-Dialog der Wissenschaften. So schickten sie kistenweise Mineralien, Edelsteine und Fossilien hin und her, Sammler und Wissenschaftler pendelten zwischen Ost und West, zahlreiche Publikationen wurden ausgetauscht, es wurde lebhaft geforscht und diskutiert - alles in allem war es ein fruchtbarer Boden, auf dem auch mineralogisch sehr viel wachsen konnte.

Und wie sieht es heute aus? Was bringt uns das viel gepriesene Kommunikations-Zeitalter? Die Grenzen sind heute zwar wieder offener denn je, nicht nur elektronisch. Blickt man aber zurück in die Geschichte, scheint in der Ost-West-Mineralogie früher mehr los gewesen zu sein. Grund genug, erneut in Richtung Rußland zu blicken. Nicht misstrauisch, sondern mit der Freude, Reise- und Entdeckerlust, mit der dies z. B. im 19. Jahrhundert geschah. Das vorliegende extraLapis möge dazu beitragen: Noch nie gab es in deutscher Sprache einen so komprimierten Überblick über die russische Landesmineralogie, einen praxisorientierten Leitfaden zu diesem Sammelgebiet.

Und schließlich: Wenn wir als Sammler, ob in Ost oder West, die wir alle eine gemeinsame Liebe teilen - die kristallisierten Schätze der Erde - wenn wir es nicht schaffen, in Freundschaft alte Grenzen zu überwinden, wer soll es dann? Doch schauen wir erst einmal kurz nach Osten: Wo liegt Rußland überhaupt?

Редактор(ы):Cherniak D.J., Zhang Y.
Издание:Mineralogical Society of America, 2010 г., 1055 стр., ISBN: 978-0-939950-86-7
Язык(и)Английский
Diffusion in minerals and melts / Диффузия в минералах и расплавах

Geologists often need to apply diffusion theory and data to understand the degree of mass transfer, infer temperature-time histories, and address a wide range of geological problems. The aim of this volume is to provide practitioners the necessary background and data for such applications. We have made efforts to present a comprehensive overview, with discussion and assessment of diffusion data in a broad range of rock-forming minerals and all geologically relevant melts. Extensive data tables are provided as online supplements (as well as at websites maintained by individual authors), both for general usage by readers, and for experimentalists and theoreticians in the field to develop greater understanding of diffusion and plan future research directions.

Автор(ы):Klein C., Philpotts A.R.
Издание:Cambridge University Press, 2013 г., 1253 стр., ISBN: 978-0-521-76115-4; 978-0-521-14521-3
Язык(и)Английский
Earth materials. Introduction to mineralogy and petrology / Состав Земли. Введение в минералогию и петрологию

The fundamental concepts of mineralogy and petrology are explained in this highly illustrated, full-color textbook, to create a concise overview for students studying Earth materials. The relationship between minerals and rocks and how they relate to the broader Earth, materials, and environmental sciences is interwoven throughout. Beautiful photos of specimens and CrystalViewer’s three-dimensional illustrations allow students to easily visualize minerals, rocks, and crystal structures.

Издание 2
Автор(ы):Klein C., Philpotts A.R.
Издание:Cambridge University Press, 2017 г., 1924 стр., ISBN: 978-1-107-15540-4
Язык(и)Английский
Earth materials. Introduction to mineralogy and petrology / Состав Земли. Введение в минералогию и петрологию

Over the past two decades, many curriculum changes have occurred in geology, Earth science, and environmental science programs in universities. Many of these have involved the compression of separate one-semester courses in mineralogy, optical mineralogy, and petrology into a singlesemester offering that combines mineralogy and petrology, commonly called Earth Materials. Such a course is a challenge to the instructor (or a team of instructors) and the students. This is especially so when few, if any, textbooks for such a one-semester course have been available.

Автор(ы):Klein C., Philpotts A.R.
Издание:Cambridge, 2012 г., 549 стр.
Язык(и)Английский
Earth materials. Introduction to mineralogy and petrology / Состав Земли. Введение в минералогию и петрологию

Over the past two decades, many curriculum changes have occurred in geology, Earth science, and environmental science programs in universities. Many of these have involved the compression of separate one-semester courses in mineralogy, optical mineralogy, and petrology into a single-semester offering that combines mineralogy and petrology, commonly called Earth Materials.

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