Автор(ы):Rickwood P.C.
Издание:Elsevier, 1989 г., 17 стр.
Boundary lines within petrologic diagrams which use oxides of major and minor elements / Граничные линии на петрологических схемах, в которых используются оксиды как основные и второстепенные элементы

Use of some petrologic diagrams applied to analyses of volcanic rocks is unnecessarily difficult due to lack of data for construction of discriminant lines between rock series. Coordinates are provided for sufficient points to enable accurate plotting of the boundary lines within seven diagrams, viz.: ( 1 ) TAS - total alkalies (Na20+K20) vs. SIO2; (2) K20 vs. SiO2; (3) AFM; (4) Jensen; (5) KTP - K20-TiO~-P205; (6)FMS- (FeO*/MgO) vs. SIO2; and (7) TAKTIP- K20/(Na20+K20) vs. TiOz/P2Os. Different versions of these boundaries are collated to indicate their variable position, and it is demonstrated that inter-laboratory analytical precision suffices to account for almost all of their spread on the TAS and K20 vs. SiO2 diagrams.

Редактор(ы):Kool T.W., Muller K.A.
Издание:World Scientific Publishing Co. Pte. Ltd., Singapore, 2010 г., 582 стр., ISBN: 978-981-4293-35-8
Properties of perovskites and other oxides / Свойства перовскитов и других оксидов

On the occasion of the 65th birthday of K Alex Muller (KAM), the IBM Zurich Research Laboratory in Ruschlikon, with the help of J. Georg Bednorz, offered a compilation of almost all the publications he had authored or co-authored. Those two volumes encompass thewritings until 1992. They are very useful to access KAM's earlier work, with the more than 300 papers arranged in chronological order. When KAM turned seventy, Prof. KK Phua, chairman of World Scientific, suggested to collect relevant original work in a volume to be published by this well-established house. After some reflection, Muller thought this might be a reasonable undertaking, and selected, from the then more than 400 original publications, those he considered the relevant ones. The result is this book with its eleven chapters, arranged in topological rather than chronological order. In each chapter the pertinent publications in one specific area of investigations are grouped together. Therefore it should be easy for the reader to find a paper of interest to him or her. To bring this work up to date, it also includes KAM's articles on the topics in this book published after 1992 and publications by Tom Kool, the second author, who worked in the field of oxide perovskites as well and kept helping to realize and edit the present volume <...>

МеткиОксиды, Перовскит
Автор(ы):Булах А.Г., Золотарев А.А.
Издание:Санкт-Петербург, 1998 г., 24 стр.
Атлас структур минералов - оксидов, гидроксидов

Атлас подготовлен преподавателями каф. минералогии геологического ф-та СПбГУ. В него вошли изображения кристаллических структур оксидов и гидроксидов, которые принципиально важны для понимания общих закономерностей кристаллического строения минералов и обычно используются преподавателями для объяснения зависимостей между структурой и составом, с одной стороны, и морфологией кристаллов и их свойствами - с другой

Издание 2
Автор(ы):Deer W.A., Howie R.A., Zussman J.
Издание:Geology Society, London, 2011 г., 920 стр., ISBN: 978-1-86239-315-8
Rock-forming minerals. Non-silicates. Oxides, hydroxides and sulphides / Породообразующие минералы. Несиликаты. Оксиды, гидроксиды и сульфиды

Tt is 50 years since the publication of the first edition of this volume of Rock-forming Minerals. The intervening years have seen a vast growth in the range and quantity of published work on 'non-silicate" rock-forming minerals, a growth that has justified dividing the topics of the first edition into two volumes (sulphates, carbonates, phosphates and halides have already been covered; see Chang, Howie and Zussman, Rock-forming Minerals, Vol. 5B, 2nd edn. The Geological Society, 1996). Here, we discuss the oxides, hydroxides and sulphides. This growth in published information on oxide, hydroxide and sulphide minerals has resulted partly from the availability of new techniques for the chemical and structural analysis of these materials and the characterization of their physical and chemical properties. It has also been the result of the opening-up of entirely new fields of investigation where these minerals play a key role. The list of minerals discussed in this new edition has expanded somewhat compared with the first edition; although the same five sulphide minerals are considered "rock-forming', the hydroxides have gained several new iron hydroxide phases (akaga-neitc. ferrihydrite and feroxyhyte), while losing limonite. These developmenb are largely due to better characterization of poorly crystalline ultrafine particle phases using new techniques. The list of oxides has also expanded with additions including quandilite. pseudonitile and armalcolite, the last a lunar mineral and a legacy of the Apollo missions which occurred seven years after publication of the first edition.

Автор(ы):Кудрявцева Г.П.
Издание:Недра, Москва, 1988 г., 232 стр., УДК: 538.7+550.382.3, ISBN: 5-247-00284-9
Ферримагнетизм природных оксидов

Рассмотрены основы ферримагнетизма, кристаллохимия природных ферримагнитных оксидов с различными типами кристаллических структур, рациональная методика изучения природных ферримагнитных минералов. Описана простейшая, аппаратура для исследования магнитных свойств минералов, даны оригинальные схемы установок для термомагнитного анализа и термомагнитной сепарации, собранных с использованием выпускаемых узлов. Рассмотрены особенности состава и магнитных свойств ферримагнитных минералов, слагающих промышленные типы месторождений железных, титановых и марганцевых руд. Показана высокая информативность разнообразных магнитных характеристик для решения ряда теоретических и прикладных задач.

Для минералогов, геологов-рудников и геофизиков. 

МеткиКристаллохимия, Магнитные свойства минералов, Оксиды, Термомагнетизм, Ферримагнетизм, Ферримагнитные осадки
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