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Author: A.S. Marfunin
Publisher: Springer
ISBN:
Category : Science
Languages : en
Pages : 362
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Book Description
The physics of minerals in a broad sense implies the fundamental aspects of understanding mineral matter: the electronic structure of atoms related to their behavior in geochemical processes; the atomic and electronic structures of minerals; the properties of minerals, with their genetic, geophysical, and technical significance, and their pressure and temperature dependence; the mechanisms of phenomena and reactions in mineral formation and transformation processes; the physical me thods applied in mineralogical, geochemical and petrological studies, and to a great extent in geological surveys and prospecting. In a narrower sense, it is a branch lying in the border area between mineralogy and solid-state physics, dealing with those aspects of mine ralogy which require, for their understanding and investigation, special knowledge in contemporary physics and chemistry of solids. The physics of minerals accounts for the third crucial change within this century in the conceptual foundations of mineralogy: after physi cochemical mineralogy, from experimental studies of phase relations to parage netic analyses, and crystal chemistry of minerals, there followed solid-state physics, which has evolved to its present state over the past 25 years. The task of mineralogy has expanded greatly. In addition to the identification and description of minerals, it is becoming necessary to establish the relationships between structure, composition and properties of minerals and their genesis, their distribution within geological regions, magmatic, metamorphic and sedimentary formations and types of ore deposits. The development of new methods of investigation requires an understanding of the physical meaning of the parameters under evaluation.
Author: A.S. Marfunin
Publisher: Springer
ISBN:
Category : Science
Languages : en
Pages : 362
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Book Description
The physics of minerals in a broad sense implies the fundamental aspects of understanding mineral matter: the electronic structure of atoms related to their behavior in geochemical processes; the atomic and electronic structures of minerals; the properties of minerals, with their genetic, geophysical, and technical significance, and their pressure and temperature dependence; the mechanisms of phenomena and reactions in mineral formation and transformation processes; the physical me thods applied in mineralogical, geochemical and petrological studies, and to a great extent in geological surveys and prospecting. In a narrower sense, it is a branch lying in the border area between mineralogy and solid-state physics, dealing with those aspects of mine ralogy which require, for their understanding and investigation, special knowledge in contemporary physics and chemistry of solids. The physics of minerals accounts for the third crucial change within this century in the conceptual foundations of mineralogy: after physi cochemical mineralogy, from experimental studies of phase relations to parage netic analyses, and crystal chemistry of minerals, there followed solid-state physics, which has evolved to its present state over the past 25 years. The task of mineralogy has expanded greatly. In addition to the identification and description of minerals, it is becoming necessary to establish the relationships between structure, composition and properties of minerals and their genesis, their distribution within geological regions, magmatic, metamorphic and sedimentary formations and types of ore deposits. The development of new methods of investigation requires an understanding of the physical meaning of the parameters under evaluation.
Author: A.S. Marfunin
Publisher: Springer
ISBN: 9783642670442
Category : Science
Languages : en
Pages : 0
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Book Description
The physics of minerals in a broad sense implies the fundamental aspects of understanding mineral matter: the electronic structure of atoms related to their behavior in geochemical processes; the atomic and electronic structures of minerals; the properties of minerals, with their genetic, geophysical, and technical significance, and their pressure and temperature dependence; the mechanisms of phenomena and reactions in mineral formation and transformation processes; the physical me thods applied in mineralogical, geochemical and petrological studies, and to a great extent in geological surveys and prospecting. In a narrower sense, it is a branch lying in the border area between mineralogy and solid-state physics, dealing with those aspects of mine ralogy which require, for their understanding and investigation, special knowledge in contemporary physics and chemistry of solids. The physics of minerals accounts for the third crucial change within this century in the conceptual foundations of mineralogy: after physi cochemical mineralogy, from experimental studies of phase relations to parage netic analyses, and crystal chemistry of minerals, there followed solid-state physics, which has evolved to its present state over the past 25 years. The task of mineralogy has expanded greatly. In addition to the identification and description of minerals, it is becoming necessary to establish the relationships between structure, composition and properties of minerals and their genesis, their distribution within geological regions, magmatic, metamorphic and sedimentary formations and types of ore deposits. The development of new methods of investigation requires an understanding of the physical meaning of the parameters under evaluation.
Author: Arnold S. Marfuin
Publisher:
ISBN:
Category :
Languages : en
Pages :
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Book Description
Author: Arnolʹd Sergeevich Marfunin
Publisher: Springer
ISBN:
Category : Science
Languages : en
Pages : 362
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Book Description
Author: Miner Hamlin Paddock
Publisher:
ISBN:
Category : Mineralogy
Languages : en
Pages : 176
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Book Description
Author: Annemarie Meike
Publisher: Springer Science & Business Media
ISBN: 1461512050
Category : Science
Languages : en
Pages : 512
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Book Description
The triennial International Alloy Conferences (lACs) aim at the identification and promotion of the common elements developed in the study, either experimental, phenomenological, or theoretical and computational, of materials properties across materials types, from metals to minerals. To accomplish this goal, the lACs bring together scientists from a wide spectrum of materials science including experiment, theory, modeling, and computation, incorporating a broad range of materials properties. The first lAC, lAC-I, took place in Athens, Greece, June 16-21, 1996. The present volume of proceedings contains the papers presented at IAC-2, that took place in Davos, Switzerland, August 8-13, 1999. The topics in this book fall into several themes, which suggest a number of different classification schemes. We have chosen a scheme that classifies the papers in the volume into the categories Microstructural Properties; Ordering, Kinetics and Diffusion; Magnetic Properties and Elastic Properties. We have juxtaposed apparently disparate of revealing the dynamic character approaches to similar physical processes, in the hope of the processes under consideration. We hope this will invigorate new kinds of discussion and reveal challenges and new avenues to the description and prediction of properties of materials in the solid state and the conditions that produce them.
Author: Miner Hamlin Paddock
Publisher: Rarebooksclub.com
ISBN: 9781230068527
Category :
Languages : en
Pages : 30
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Book Description
This historic book may have numerous typos and missing text. Purchasers can usually download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1911 edition. Excerpt: ..."fool's gold" but may actually contain gold. USES.--For ornaments; source of sulphur; source of SO; fo_r sulphuric acid; somewhat as source of iron and iron compounds, but sulphur is diflicultly removed. NATURAL HISTORY.--Pyrite is found widely disseminated, sometimes in huge crystals, sometimes in extensive ledges. Hundreds of thousands of tons are mined annually, sources of sulphur and sulphuric acid. It is generally associated with copper, gold, and other metals. It is an unstable Inineral, and, breaking up into oxides of iron and sulphuric acid, is a great disintegrator of rocks and former of new minerals. No stone containing pyrite is suitable for architectural purposes. Pyrite is from pur, meaning fire, and means firestone. HALITE FORM.--Sometimes massive; often in cubic crystals of the isometric system. SPECIFIC GRAVITY.----2.1. CHEMICAL PROPERTIES.--In closed tube, decrepitates, melts; in o. t., the same. Soluble in water, saline taste. B. B., fuses, colors the flame bright yellow, --sign of sodium. With H2SO4 gives HCl acid. CIIARACTERISTIC TESTS.--Hardness, form, taste. VARIETIES.----Halite. USES.----Food; preservative; source of sodium and sodium compounds; of chlorine and chlorine compounds; (formerly employed as money among eastern peoples). NATURAL HIsToRY.--Found in sea water, in mines_ as rock salt, and as brine in the rocks. Estimated that if the salt of the ocean were extracted it would equal fourteen continents of the size of Europe above ocean level. Physiographically, beds of salt indicate ancient salt marshes, lagoons of the ocean, and also extensive interior drainage regions. Observe the great interior drainage area of Eurasia, 4000 miles long, receiving immense rivers into interior salt oceans. The...
Author: Kate Wright
Publisher: Springer Science & Business Media
ISBN: 9780792359814
Category : Science
Languages : en
Pages : 670
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Book Description
One of the major developments in Earth Sciences in general, and mineralogy in particular, has been the growth of our understanding of the microscopic behaviour of the complex materials that make up the Earth. This has been made possible by advances in our ability to probe minerals at the atomic level, over a large range of pressure and temperature conditions. New experimental techniques include the use of scanning probe microscopies to investigate mineral surfaces, as well as the use of neutron scattering, nuclear spectroscopies and synchrotron radiation to investigate the bonding and structure of minerals. In addition, there have been major developments in computational methods so that it is now possible to calculate the electronic structure of many rock forming materials. The aim of this volume is to give a coherent survey of the latest developments in experimental and theoretical approaches to the study of microscopic propertie~ and processes in minerals. Chapters in the book cover a number of key themes in the mineral sciences such as the behaviour of minerals at extremes of pressure and temperature, ordering in complex silicates, mechanisms of water incorporation in mantle phases, the importance of reactions occurring at the mineral surface, and the ability of computational methods to provide useful, qualitative information on the bulk and surface properties of minerals. The background to several experimental techniques is covered in some detail with examples of relevance to the issues cited above.
Author: Robert Cooper Liebermann
Publisher: MDPI
ISBN: 303936541X
Category : Science
Languages : en
Pages : 627
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Book Description
This Special Issue contains original scientific papers in the field of mineral physics (and also rock physics). These papers are grouped into four categories: Reviews, Experimental Science, Theoretical Science and Technological Developments. These papers include those from first authors covering 5 generations of mineral physicists, including contemporaries of Orson [e.g., William Bassett, Frank Stacey], the next generation of leaders in mineral physics throughout the world [e.g., Michael Brown, Eiji Ohtani], current leaders in this field [e.g., Agnes Dewaele, Jun Tsuchiya], senior graduate students [e.g., Jan Borgomano, Vasilije Dobrosavlijevic, Francesca Miozzi], and an undergraduate student [e.g., Tyler Perez]. Mineral physics is the study of mineralogical problems through the application of condensed matter physics. In reality, mineral physicists use not only physics, but also solid-state chemistry; they study not only minerals, but all materials related to natural minerals (e.g., structural analogs, but also glasses, melts and fluids). Mineral and rock physics is intimately connected to many other geoscience disciplines including seismology, planetary science, petrology, geochemistry, geomagnetism, and geodynamics, and even materials and climate science. This book is dedicated to Orson Anderson who died in June 2019 at the age of 94.
Author:
Publisher:
ISBN:
Category : Mineralogy
Languages : en
Pages :
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