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Выпуск 3
Автор(ы):Марфунин А.С.
Издание:Springer, 1998 г., 342 стр., ISBN: 978-3-642-62108-6
Advanced mineralogy. Mineral matter in space, mantle, ocean floor, biosphere, environmental management, and jewelry. Vol 3. /  Продвинутая минералогия. Минеральные вещества в космосе, мантии, океане, биосфере, природопользовании и ювелирном деле. Часть 3

This volume of Advanced Mineralogy encompasses six different areas having two features in common: they are related to one of the largest enterprises of the second half of this century; and represent the ultimate and final extension of the concept of mineral matter.

- Understanding mineral matter in Space is one of the principal purposes of cosmic exploration. This includes the results of comparative planetology, lunar epopee, sophisticated meteorite studies (now more than 500 meteorite minerals), discovery of the interstellar mineral dust forming some 60 trillion of earth masses in the Galaxy, and terrestrial impact crater studies. It is possible now to speak of mineralogy of the Universum, and the mineralogical type of the states of matter in the Universe. 

Автор(ы):Xiuli Wang
Издание:Gulf Publishing Company, Houston, 2009 г., 415 стр.
Advanced natural gas engineering

The role of natural gas in meeting the world energy demand has been increasing because of its abundance, versatility, and clean burning nature. As a result, new gas exploration, field development, and production activities are under way. This is especially true in places where natural gas was (until recently) labeled as “stranded.” Because a significant portion of natural gas reserves worldwide are located across bodies of water, gas transportation becomes an issue. We are dealing with many unique issues and facing many challenges in the entire “food chain” (upstream to midstream and downstream) of natural gas engineering.

Редактор(ы):Sammonds P.R., Thompson J.M.T.
Издание:Imperial College Press, London, 2007 г., 342 стр., ISBN: 978-1-86094-761-2
Advances in Earth Science From Earthquakes to Global Warming / Достижения в области наук о Земле От землетрясений до глобального потепления

This welcome volume is a collection of articles principally adapted from articles published in the Philosophical Transactions triennial issue. It very largely reflects the views of younger scientists, and highlights how the Earth Sciences continue to delight us with new ideas and controversies. Many of the authors are research fellows, or former research fellows, of the Royal Society, and the editors have successfully assembled an entertainingly eclectic mix. The book is divided into three sections covering Environmental Change, the Dynamics of the Earth, and Applied Earth Science, and the topics range from costing climate change, to the properties of the Earth’s core and objectively optimised Earth observation

Автор(ы):Cooke D.R., Holliday J.R.
Издание:Ore deposit and exploration technology, 2007 г., 19 стр.
Advances in Geological Models and Exploration Methods for Copper ± Gold Porphyry Deposits

This paper focuses on the relationships between the geological model and exploration techniques for porphyry Cu ± Au deposits, with reference to the discovery record and exploration practices over the past fifteen years. The porphyry model is built on a long record of study dating back to the 1960s which has been gradually refined to encompass differences and complexities in mineralization and hydrothermal alteration assemblages resulting from varying intrusion (‘porphyry’) chemistries, differing wallrock geochemical and structural controls, the upwards zonation into the lithocap environment, and the overprinting effects of deep weathering.

Автор(ы):Adams M.D.
Редактор(ы):Wills B.A.
Издание:Elsevier, 2005 г., 1076 стр., ISBN: 0-444-51730-8, 0067-4528
Advances in gold ore processing / Достижения в переработке золотых руд

The gold-processing industry is experiencing change. As free-milling and oxide ores become depleted, more complex polymetallic and refractory ores are being processed, coupled with increasing pressure for stricter environmental compliance. Recent years have also seen a steady reduction in mineral processing and metallurgy graduates and a gradual loss of older operating experience. A contribution to documenting current and future best practice <...>

Редактор(ы):Gosso G., Marotta A.M., Spalla M.I.
Издание:The Geological Society of London, 2010 г., 235 стр., ISBN: 978-1-86239-295-3
Advances in interpretation of geological processes. Refinement of multi-scale data and integration in numerical modeling / Достижения в интерпретации геологических процессов. Оптимизация разномасштабных данных в численном моделировании

This Special Publication deals with some of the themes treated during the XVI Deformation Rheology and Tectonics Conference, held in Milano on 27–29 September 2007, and analysed in depth during the workshop, held in Oropa-Biella on 29 September–2 October 2007. A preconference excursion was held on the Monviso metaophiolites and Dora–Maira UHP continental crust (23–26 September 2007).

Автор(ы):Dohmen R., Magna T., Tomascak P.B.
Издание:Springer, 2016 г., 204 стр., ISBN: 978-3-319-01430-2
Advances in lithium isitope geochemistry / Достижения в литиевой изотопной геохимии

In this book we decided to attach the permil sign (‰) to all Li isotopic quantities. One way of viewing stable isotopes denoted by δ is that the arithmetic sets the results as being part-per-thousand quantities, so to place the ‰ on a value is redundant. However, this implies a certain familiarity from the reader. Our decision regarding the ‰ in this volume was guided by the potential that the audience may include those not so steeped in the thinking of stable isotopes. This calls to mind a historical note regarding Li isotopes. Readers of the early literature on the subject (beginning with Chan in 1987) will find papers that use δ6Li. Prior to 2000, using the now-accepted δ7Li notation was viewed as an unwanted usurpation by at least one prominent geochemist. Nevertheless, being clear is important, and although δ7Li was not the first notation employed, it follows stable isotope convention. We find that students have a hard enough time understanding isotope geochemistry, so to oppose the notation used in virtually all systems (positive values are isotopically heavier than negative values) invites confusion. Hence, our use of the ‰ is a further step to make this compilation clear for all.

Выпуск 2
Редактор(ы):Saxena S.K.
Издание:Springer, 1982 г., 354 стр., ISBN: 978-1-4612-5685-4
Advances in Physical Geochemistry. Volume 2 / Достижения в физической геохимии. Выпуск 2

The second volume of this series consists of three parts. Part I focuses on the research on intracrystalline reactions. This work, which began nearly two decades ago, is critically reviewed by Ghose and Ganguly in Chapter 1. Besides the review, the authors include some of their previously unpublished work to demonstrate how future research could aid in obtaining data on thermodynamics of solid solutions and in understanding the cooling history of igneous and metamorphic rocks. The latter is also the theme adopted by Kretz in the second chapter, which examines the redistribution of Fe and Mg in coexisting silicates during cooling. Chapter 3 contains new data on Fe-Mg distribution in clinopyroxenes. Dal Negro and his co-authors have selected a series of clinopyroxenes from volcanic rocks and present site occupancy data on several clinopyroxenes of intermediate compositions. The data set has not been published before and is the first of its kind.

Редактор(ы):Rubie D.C., Thompson A.B.
Издание:Springer-Verlag, 1985 г., 300 стр., ISBN: 978-1-4612-9548-8
Advances in physical geochemistry. Volume 4. Metamorphic reactions. Kinetics, textures and deformation / Успехи физической геохимии. Выпуск 4. Метаморфические реакции. Кинетика, текстуры и деформация

It is very common to find that in mineral synthesis experiments the crystals that form first have disordered cations, even when the synthesis conditions are well within the stability field of the ordered state. Some examples are the crystallization of albite from glass starting material (MacKenzie, 1957) or a flux (Woensdregt, 1983), cordierite from glass (Schreyer and Schairer, 1961; Putnis, 1980a), and plagioclase from glass (Eberhard, 1967; Kroll and Muller, 1980).

Автор(ы):Arp G., Queric N.-V., Reitner J.
Издание:Springer, 2011 г., 572 стр., ISBN: 0930-0317, 978-3-642-10415-2
Advances in stromatolite geobiology / Достижения в геобиологии строматолитов

Stromatolites are the most intriguing geobiological structures of the entire history of the earth since the early beginning of the fossil record in the Archaean. Traditionally, stromatolites and related microbial sediments are interpreted as biosedimentological remains of biofilms and microbial mats.
Stromatolites are important environmental and evolutionary archives that give us plenty of information about ancient habitats, biodiversity, evolution of complex benthic biosystems, and generally of Global Change. However, many aspects of the formation, biology, and geobiology of these structures are still cryptic and poorly understood. <...>