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Books > Science & Mathematics > Chemistry > Mineralogy > General
Mining is a capital-intensive industry, and involves long lead
times to develop projects that demand a structured approach, from
mine exploration to exit. This book provides mine developers,
investors, owners, shareholders, and mineral policymakers a
comprehensive game plan to raise capital for the development of new
mining projects or to bolster operational mines. The author, an
experienced mining capital consultant, shows how mine developers
and mine owners can secure capital in any phase of the commodity
price cycle, at any site, and at any project stage. The book
follows a proven and structured approach that enables mine
developers and owners to successfully raise capital for their
projects. With the aid of case studies and practical methods, the
reader will learn the essentials on topics ranging from developing
and marketing a business case for investment, to the types and
sources of mining capital for different project stages, as well as
the structure and significance of due diligence. The author
presents actual mining projects and their funding plans,
transaction structures and term sheets for capital. The mining
projects discussed represent various project stages, commodities,
and parts of the globe, offering a comprehensive reference guide
for mine developers, investors and promoters alike.
'Hurray for Mackenzie and Guilford for at last we have a pictorial
guide to the rock-forming minerals! . . . such feasts of colour in
mineralogy books are rare . . . an admirable guide' New Scientist
The first edition of this book was published in 1965 and its French
translation in 1966. The revised second edition followed in 1967
and its Russian translation became available in 1969. Since then,
many new petrographic observations and experimental data elucidat-
ing reactions in metamorphic rocks have made a new approach in the
study of metamorphic transformation desirable and possible. It is
felt that this new approach, attempted in this book, leads to a
better unders- tanding of rock metamorphism. The concept of
metamorphic facies and subfacies considers asso- ciations of
mineral assemblages from diverse bulk compositions as
characteristic of a certain pressure-temperature range. As new
petrographic observations accumulated, it became increasingly
difficult to accommodate this information within a manageable
framework of metamorphic facies and subfacies. Instead, it turned
out that mineral assemblages due to reactions in common rocks of a
particular composi- tion provide suitable indicators of metamorphic
conditions. Metamorphic zones, defined on the basis of mineral
reactions, very effectively display the evolution of metamorphic
rocks. Thus the im- portance of reactions in metamorphic rocks is
emphasized. Experimen- tal calibration of mineral reactions makes
it possible to distinguish reac- tions which are of petrogenetic
significance from those which are not. This distinction provides
guidance in petrographic investigations un- dertaken with the
object of deducing the physical conditions of metamorphism.
Das Motiv fur die Veranstaltung dieses Symposiums uber die
Beziehungen zwischen metallogenetischen und geochemischen Provinzen
war ein egoistisches Informationsbedurfnis des Organisators. Als
ich 1967 an dem Manuskript uber Erzprovinzen und Kontinentaldrift
arbeitete, ergab sich die Frage, ob die Metalle der Lagerstatten in
den wandernden Kontinentalschollen beheimatet sind oder ob sie aus
dem wechselnden Substratum des oberen Mantels und der daraus ge-
speisten ozeanischen Kruste stammen. Es galt also, das Material zu
uberprufen, das die Beziehungen der Erzlagerstatten zur Geochemie
ihrer kontinentalen Um- gebung oder zur Geochemie des Ozeanbodens
zeigt. Dies kann zugleich auch Bei- trage ergeben zu dem Problem
der modernen Iateralsekretionaren Lagerstatten- bildung. Die
wirkungsvollste Art, sich bei der heutigen grossen Menge von
Literatur uber ein komplexes Thema zu informieren, ist, kompetente
Leute zusammenzu- bitten, damit sie daruber vortragen und
diskutieren. Ich darf sagen, dass meinem Bedurfnis voll Genuge
geleistet wurde und ich habe dafur all den lieben Kolle- gen, die
zum Teil von sehr weit nach Leoben gekommen sind, herzlichen Dank
zu sagen. Alle Vortrage behandeln, ja man kann fast sagen, klaren
in ihrer Gesamt- heit das aufgeworfene Problem. Ich mochte aber
doch glauben und hoffen, dass nicht nur der Veranstalter, son- dern
auch die Teilnehmer von den Vortragen und Diskussionen Nutzen
hatten. Ein intensiver Gedankenaustausch war moglich, da die
Teilnehmerzahl mit Ab- sicht klein gehalten und auf spezielle
Sad1kenner beschrankt war und da das Programm im Gegensatz zu
vielen Kongressen weite Lucken fur Diskussionen liess.
The new edition of this popular textbook, once again, provides an
indispensable guide for the next generation of mineralogists.
Designed for use on one- or two-semester courses, this second
edition has been thoughtfully reorganised, making it more
accessible to students, whilst still being suitable for an advanced
mineralogy course. Additions include expanded introductions to many
chapters, a new introductory chapter on crystal chemistry, revised
figures, and an extended plates section containing beautiful colour
photographs. Text boxes include historical background and case
studies to engage students, and end-of-chapter questions help them
reinforce concepts. With new online resources to support learning
and teaching, including laboratory exercises, PowerPoint slides,
useful web links and mineral identification tables, this is a sound
investment for students in the fields of geology, materials science
and environmental science, and a valuable reference for
researchers, collectors and anyone interested in minerals.
This student-oriented text is written in a casual, jargon-free
style to present a modern introduction to mineralogy. It emphasizes
real-world applications and the history and human side of
mineralogy. This book approaches the subject by explaining the
larger, understandable topics first, and then explaining why the
"little things" are important for understanding the larger picture.
A fascinating exploration of exquisite images captured from natural
materials, and of their applications in fashion, environmental
design, and apps that anticipate a new era of digitally-driven
individual creativity. Data From Nature begins with the chance
encounter between an ammonite and a digital scanner and goes on to
relate the author's growing immersion in the micro-scale beauty of
minerals and--thanks to new digital means of production--their
applications in wide areas of design. These include an
award-winning range of silk scarves for Liberty of London (also
sold in Saks Fifth Avenue); "frocks from rocks"; a striking
architectural facade in London, and the transformation of his own
house and garden using the latest digital techniques. Along the way
we learn about how minerals form in the Earth; ways they have been
admired and imagined from ancient civilizations to the dawn of
Modernity; and discover how the inlaid surfaces of Renaissance
cabinets of curiosity could inspire creative coloring and design
apps intended to equip children and adults alike to participate
creatively in the Digital Revolution. And as if all this weren't
enough, the book ends as improbably as it started with a short
biography of a "lost" (for which read "fictional")
seventeenth-century artist, Carlo Alcite, whose "works" reveal
powers of invention and draftsmanship worthy of a baroque master.
Building upon the award-winning second edition, this comprehensive
textbook provides a fundamental understanding of the formative
processes of igneous and metamorphic rocks. Encouraging a deeper
comprehension of the subject by explaining the petrologic
principles, and assuming knowledge of only introductory
college-level courses in physics, chemistry, and calculus, it
lucidly outlines mathematical derivations fully and at an
elementary level, making this the ideal resource for intermediate
and advanced courses in igneous and metamorphic petrology. With
over 500 illustrations, many in color, this revised edition
contains valuable new material and strengthened pedagogy, including
boxed mathematical derivations allowing for a more accessible
explanation of concepts, and more qualitative end-of-chapter
questions to encourage discussion. With a new introductory chapter
outlining the "bigger picture," this fully updated resource will
guide students to an even greater mastery of petrology.
Wasser". Dieser MeBfiihler wird nun irgendwo in der Natur
installiert, der Beob- achter befindet sich weit entfemt, vor einem
Bildschirm sitzend, auf den die MeB- signale iibertragen werden. Es
solI festgestellt werden, ob es regnet oder nicht. 1st nun das
MeBintervall zu groB eingesteIlt, etwa alle 12 Stunden ein Signal,
so kann der Beobachter bei der Information, Nicht-Wasser" keine
Aussage dariiber treffen, ob es regnet oder nicht. Da Regen fUr
einen konkreten Raurn betrachtet ein Wechsel von "Wasser" und,
Nicht-Wasser", eben die diskreten Regentropfen, darsteIlt, ist die
Information, Nicht-Wasser" ebenso fiir Regen wie fUr schOnes Wetter
richtig, bei Regen eben nur weniger oft. Nach dieser Erfahrung wird
das MeBintervaIl nun verkleinert, alle paar Sekun- den erhiUt nun
der Beobachter eine Information iiber "Wasser" und, Nicht- Wasser".
Und jeden Abend urn halb Sieben bis Sieben Uhr regnet es,
zurnindest meldet der Fiihler abwechselnd "Wasser" und,
Nicht-Wasser". Des Ratsels Lo- sung: Jeden Abend wird der Garten
gesprengt, in dem sich der MeBfiihler befindet. Der Raurn, der vom
MeBfiihler erfaBt wird, ist zu klein, urn eindeutig zwischen
natiirlichem Regen und anderen sporadischen
Wassertropfenereignissen unter- scheiden zu konnen. Fiir einen an
den Bildschirm verbannten Beobachter ist die Feststellung, ob es
regnet, nur gegeben, wenn mehrere MeBfiihler iiber einen hin-
reichend groBen Raum verteilt in entsprechend kurzen Intervallen
eine Information dariiber liefem, ob sie gerade vom Wasser oder von
Luft umgeben sind. MeBraurn und MeBzeit bestimmen also die durch
die Messungen gewonnene Aussage.
This book is the first systematic treatise of available data and
view-points obtained from geological and geochemical studies of the
Mo deposits in Qinling Orogen, China. Qinling Orogen has a minimum
reserve of 8.7 Mt Mo, ranking the largest molybdenum province both
in China and the world. Incorporating all known Mo deposit types in
the world, it presents extensive studies of Mo deposits of
world-class and unusual types within tectonic settings. The Qinling
Orogen was finally formed during continental collision between
Yangtze and North China cratons, following the Triassic closure of
the northernmost paleo-Tethys. It hosts 49 Mo deposits formed in
seven mineralization events since 1850 Ma, with all the world-class
deposits being formed during 160-105 Ma, coeval with collisional
orogeny. These deposits are assigned to magmatic and metamorphic
hydrothermal classes. The magmatic hydrothermal class includes
porphyries, skarns, and intrusion-related veins (carbonatite,
fluorite and quartz). The porphyry Mo systems in Qinling Orogen are
predominated by Dabie-type formed in continental collision setting,
followed by Endako- and Climax-types formed in continental arcs and
rifts, respectively. The metamorphic hydrothermal Mo deposits are
only reported in Qinling Orogen, and thus a new crustal continuum
model for the orogenic class mineral systems is proposed. A
scientific linkage between ore geology and fluid inclusions is
introduced and verified both by theory and case studies. This is
the first research book comprehensively displaying continental
collision metallogeny. This literature will benefit both Western
and Chinese mineral explorers and miners, as well as research
scientists and students.
Granites are emblematic rocks developed from a magma that
crystallized in the Earth's crust. They ultimately outcrop at the
surface of every continent. This book - translated, edited, and
updated from the original French edition Petrologie des Granites
published by Vuibert in 2011 - gives a modern presentation of
granitic rocks, or granites, from magma genesis to their
emplacement into the crust and their crystallization.
Mineralogical, petrological, physical, and economical aspects are
developed in a succession of 14 chapters. Special 'info boxes'
discuss topics for those wishing to deepen their knowledge of the
subject. Also included is a glossary, a comprehensive bibliography,
as well as descriptions of modern techniques. Granites are
considered in their geological spatial and temporal frame, in
relation with Plate Tectonics and Earth History, and assisted by a
large number of high quality illustrations.
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Epidotes
(Paperback)
Axel Liebscher, Gerhard Franz
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R1,271
Discovery Miles 12 710
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Ships in 12 - 19 working days
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This text is a compilation of practical information on the analysis
of mineral type materials and products by the fused, cast bead
method. It discusses the necessary equipment and its use; the
processes involved in loss of ignition and decomposition by fusion
and their chemistry. The book is also concerned with spectrometric
parameters and the analytical procedures for a wide range of
materials which, together with tables in the appendices, aim to
allow easy reference to the parameters to be adopted to follow a
defined procedure for most types of sample. The overall aim of the
work is to help towards standardizing procedures, equipment and
software, which should help to reduce costs and make for a better
inter-laboratory comparison of results.
This is the seventh edition of a book which has been for years the
'bible' of professional and amateur gemmologists, as well as retail
jewellers. Originally written by Robert Webster, an expert who
dedicated most of his life to the subject and who worked in the
London Gem Testing Laboratory for twenty-five years, this edition
has been completely revised and updated by E. Alan Jobbins, Keeper
of Minerals and Gemstones at the Geological Museum in London for
thirty-five years. The first part of the book is a comprehensive
glossary on all aspects of gemstones and the terms associated with
them. The second part includes sections on manufactured gems, the
enhancement of gem materials and on the precautions necessary for
avoiding damage to gemstones and jewellery during manufacturing,
repairs and cleaning. There are comprehensive sets of tables of the
physical constraints needed for gem testing, of the sources of gem
materials and the cuts used to demonstrate their beauty. Fifteen
pages of colour photographs will assist in the identification of
inclusions and there are many useful conversion tables.
Acknowledged as one of the most useful reference books available,
this should be the vade mecum of all gemmologists.
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