T HE C O M P L E TE ENCYCLOPEDIA OF M I N E R A LS Description of over 600 Minerals from around the world PETR lli®E£SMILAN NOVAK, T HE C O M P L E TE ENCYCLOPEDIA OF MINERALS T HE C O M P L E TE ENCYCLOPEDIA OF MINERALS T HE C O M P L E TE ENCYCLOPEDIA OF MINERALS T HE C O M P L E TE ENCYCLOPEDIA OF MINERALS Description of over 600 Minerals from around the world PETR KORBEL & MILAN NOVAK BOOKS* Explanation of the abbreviations used in the book c - color s - streak L - luster D - diaphaneity DE - density H - hardness CL - cleavage F - fracture M - morphology LU - luminescence R - remark X - crystal XX - crystals In the figure captions, the bigger dimension is always mentioned Scale of the frequency of the occurrence • - very rare • • - rare" • • • - uncommon • • • • . abundant • • • • • - common © 1999 Rebo International b.v., Lissc. the Netherlands ©2001 Grange Books PLC, United kingdom Text: Petr Korbel, Milan Novak Fptografie: Fotobanka Granit (100), Petr Korbel (220), Geza Kulcsar (16), Jeffry A. Scovil (331), Sandor Szakall (34) Production and layout: Granit Ltd., Praha ISBN 1 84013 404 6 All rights reserved. Copying of the entire book as well as of its parts in any way is forbidden by law without prior written consent of the publisher. Contents Introduction 7 1. Elements 9 2. Sulphides 19 3. Halides 67 4. Oxides 75 5. Carbonates 113 6. Borates 131 7. Sulfates 137 8. Phosphates 155 9. Silicates 193 10. Organic compounds 281 11. Rocks, meteorites and tektites 285 Recommended literature 291 Index 293 Introduction The ever increasing number of publications about meteorites); 2. sedimentary, when a mineral minerals reflects a growing interest in nature. crystallizes during a process of diagenesis or from Most of those publications though only deal with a hydrous solutions under normal temperature few dozen of the most common minerals or (clastic, organic and chemical sedimentary rocks); gemstones. This book fills the gap by also 3. mctamorphic, when a mineral crystallizes featuring less common and rare minerals. The during mctamorphic processes in a solid state at a authors describe over 600 mineral species and wide range of temperature and pressure (it varieties, illustrated with about 750 color includes regionally and contact metamorphosed photographs. In choosing illustrations of particular rocks and skarns); 4. hydrothermal, when minerals minerals, acsthctic criteria such as size of crystal crystallize from aqueous solutions and fluids and color played a role in addition to their under high to low temperatures (it includes ore and importance and distribution in nature. This book the Alpine-type veins, cavities in volcanic rocks, includes some rare minerals, known only from one minerals and rocks, hydrothermally altered under locality, because they form very attractive crystals high temperature, e.g. greisens). or aggregates. There are minerals known to Secondary minerals are divided into following humankind since prehistoric times such as quartz groups: 1. oxidation, when minerals result from and gold, but also minerals first described quite the oxidation (weathering) of the primary minerals recently like rossmanite. The photographs show in the oxidation zone of ore deposits and other well-formed and colorful crystals but many rocks (it includes the origin of malachite and aggregates, which are more common in nature, are azurite during the chalcopyrite oxidation, also the also included. The minerals in the book are listed origin of secondary phosphates in granitic according to the mineralogical system of Hugo pegmatites during the oxidation of primary Strunz, in his book Mineralogische Tabellen in phosphates); 2. cementation, when minerals result 1978. The chemical formulae of individual from the reduction of the primary minerals (the minerals follow the form of Glossary of Mineral origin of native copper and native silver under the Species 1995 by M. Fleischer and J.A. Mandarine. reduction conditions in the cementation zone of The information is complemented in both cases ore deposits). This classification is very much with the latest knowledge from scientific simplified of course, because in many cases we literature, such as new nomenclature of cannot readily determine a specific origin of a amphiboles, micas and zeolites. particular mineral. This relates to minerals that The mineral descriptions cover the basic physical crystallize under conditions which approximately and chemical data, including chemical formula represent a transition between separate phases of and crystal system. The data provided correspond the origin, such as the magmatic or hydrothermal mainly to the end-members. The less common origins of elbaite in the pegmatite cavities; the valence of the chemical elements is marked in the mctamorphic or hydrothermal origins of grossular chemical formula (Fc5. Mil", As", Mn4, Pb"). in skarns; the magmatic or mctamorphic origins of Where an element features in both valences in the cordierite in migmatites; and the hydrothermal or mineral, they are both marked (e.g. ilvaite, secondary origins of some phosphates in granitic braunite). pegmatites etc. The origin of individual minerals is described in With the localities for individual minerals we have detail. We chose for a relatively simplified scheme tried to list the most important worldwide because the normal complexity cannot be localities regardless of their recent production but described here in detail. Minerals can be we have also included recent discoveries since distinguished as either primary (resulting directly these may produce important mineral specimens. from a solidifying of magma, crystallizing of an Where a mineral has an important use this is listed aqueous solution or mctamorphism - re- at the end of mineral description. We would like to crystallization in a solid state) and secondary acknowledge all who contributed in any way to the (resulting from alteration of the original mineral, production of this book, particularly those private e.g. during its oxidation or reduction under low collectors and institutions which loaned minerals temperature and pressure close to the surface of for photography. We hope those fascinated in the the Earth). Primary minerals are divided into world of minerals and of nature will find this book following groups: 1. magmatic, when a mineral a fascinating source of information. crystallizes directly from a melt (it includes This book is dedicated to the memory of Dr. magmatic and effusive igneous rocks, including Jaroslav "venek, who was of extraordinary granitic and alkaline syenite pegmatites and influence to several generations of Czech and Slovak mineralogists and mineral collectors with his enthusiasm for mineralogy and attitude to life. Marcasite. 100 mm. Misburg. Germany 7
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