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Crystallography remains, for mineralogy, one of the main sources of information on natural crystalline substances. A description of mineral species shape is carried out according to the principles of geometric crystallography; the crystal structure of minerals is determined using X-ray crystallography techniques, and physical crystallography approaches allow one to evaluate various properties of minerals, etc. However, the reverse comparison should not be forgotten as well: the crystallography science, in its current form, was born in the course of mineralogical research, long before preparative chemistry received such extensive development. It is worth noting that, even today, investigations of crystallographic characteristics of minerals regularly open up new horizons in materials science, because the possibilities of nature (fascinating chemical diversity; great variation of thermodynamic parameters; and, of course, almost endless processing time) are still not available for reproduction in any of the world's laboratories. This Special Issue is devoted to mineralogical crystallography, the oldest branch of crystallographic science, and aims to combine important surveys covering topics indicated in the keywords below.
Research & information: general --- galenobismutite --- high pressure --- single-crystal X-ray synchrotron diffraction --- equation of state --- calcium ferrite structure type --- lone electron pair --- vaterite --- calcium carbonate --- polymorph --- precipitation --- synthesis --- carbonation --- pathogen crystallization --- biomimetic synthesis --- renal stone --- calcium oxalate --- apatite --- brushite --- struvite --- octocalcium phosphate --- whitlockite --- Escherichia coli --- Klebsiella pneumoniae --- Pseudomonas aeruginosa --- Staphylococcus aureus --- uranyl --- selenite --- selenate --- crystal structure --- topology --- structural complexity --- demesmaekerite --- guillemenite --- haynesite --- coesite --- high-temperature Raman --- FTIR spectrum --- single crystal structure --- isobaric Grüneisen parameters --- OH-stretching modes --- strontium oxalate --- solid solutions --- ionic substitutions --- weddellite --- whewellite --- X-ray powder diffraction --- scanning electron microscopy --- EDX spectroscopy --- hydroxy-hydrate --- sulfate --- cesium --- schoepite --- krasnoshteinite --- zeolite-like borate --- hydrous aluminum chloroborate --- new mineral --- microporous crystalline material --- evaporitic salt rock --- Verkhnekamskoe potassium salt deposit --- Perm Krai --- anatomy --- Cactaceae --- oxalate --- silica --- stem --- stanfieldite --- phosphate --- merrillite --- meteorite --- pallasite --- mesosiderite --- luminophore --- bioceramics --- powder diffraction --- Raman spectroscopy --- Kamchatka --- hot springs --- pyrite --- complexity of crystal habits --- Mars --- mineral --- crystallography --- crystal chemistry --- X-ray diffraction --- crystal growth --- mineral evolution
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One last comment concerns the fundamental contributions of Fourier analysis to quantum physics: Quantum mechanics and quantum field theory.
self-electrorefining --- hedyphane group --- structural combinatorics --- CuFe2O4 --- Kamchatka --- Raman --- El Dragón --- apatite supergroup --- borate --- ariegilatite --- oyonite --- Tuscany --- gahnite --- magnesioferrite --- Szklary pegmatite --- aurihydrargyrumite --- Au6Hg5 phase --- Trentino --- Peru --- Germany --- cerromojonite --- sulfosalt --- pyrometamorphism --- Bellerberg volcano --- manganese --- gold --- spinel supergroup --- selenium --- CuAl2O4 --- clinokurchatovite --- sharyginite --- Poland --- copper --- kurchatovite --- copper oxide --- antimony --- nabimusaite group --- laachite --- lead --- thermaerogenite --- intercalated hexagonal antiperovskite --- placer --- Lower Silesia --- Eldfell --- Tolbachik volcano --- structural complexity --- nöggerathite-(Ce) --- Val di Fiemme --- Oyon district --- sanidinite --- cuprospinel --- sulfate --- fumarole sublimate --- Cretaio --- polymorphism --- polytypism --- tiberiobardiite --- fiemmeite --- stacking faults --- CO3-group --- Hatrurim Complex --- least-action principle --- phosphorus --- Laacher See --- new oxalate mineral --- Japan --- verneite --- alkaline volcanic rock --- arsenic --- Raman spectroscopy --- single-crystal investigation --- Rusinovite --- Eifel --- Lima department --- Italy --- barioferrite --- configurational entropy --- Hekla --- mercury --- Bolivia --- parafiniukite --- aluminofluoride --- new mineral --- Shadil-Khokh volcano --- Vesuvius --- bournonite group --- Ehime --- calcium --- lillianite homologous series --- chalcophyllite group --- sou?ekite --- silicate --- pyrometamorphic rocks --- crystal structure --- zirconolite --- bismuth
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One last comment concerns the fundamental contributions of Fourier analysis to quantum physics: Quantum mechanics and quantum field theory.
self-electrorefining --- hedyphane group --- structural combinatorics --- CuFe2O4 --- Kamchatka --- Raman --- El Dragón --- apatite supergroup --- borate --- ariegilatite --- oyonite --- Tuscany --- gahnite --- magnesioferrite --- Szklary pegmatite --- aurihydrargyrumite --- Au6Hg5 phase --- Trentino --- Peru --- Germany --- cerromojonite --- sulfosalt --- pyrometamorphism --- Bellerberg volcano --- manganese --- gold --- spinel supergroup --- selenium --- CuAl2O4 --- clinokurchatovite --- sharyginite --- Poland --- copper --- kurchatovite --- copper oxide --- antimony --- nabimusaite group --- laachite --- lead --- thermaerogenite --- intercalated hexagonal antiperovskite --- placer --- Lower Silesia --- Eldfell --- Tolbachik volcano --- structural complexity --- nöggerathite-(Ce) --- Val di Fiemme --- Oyon district --- sanidinite --- cuprospinel --- sulfate --- fumarole sublimate --- Cretaio --- polymorphism --- polytypism --- tiberiobardiite --- fiemmeite --- stacking faults --- CO3-group --- Hatrurim Complex --- least-action principle --- phosphorus --- Laacher See --- new oxalate mineral --- Japan --- verneite --- alkaline volcanic rock --- arsenic --- Raman spectroscopy --- single-crystal investigation --- Rusinovite --- Eifel --- Lima department --- Italy --- barioferrite --- configurational entropy --- Hekla --- mercury --- Bolivia --- parafiniukite --- aluminofluoride --- new mineral --- Shadil-Khokh volcano --- Vesuvius --- bournonite group --- Ehime --- calcium --- lillianite homologous series --- chalcophyllite group --- sou?ekite --- silicate --- pyrometamorphic rocks --- crystal structure --- zirconolite --- bismuth
Choose an application
Crystallography remains, for mineralogy, one of the main sources of information on natural crystalline substances. A description of mineral species shape is carried out according to the principles of geometric crystallography; the crystal structure of minerals is determined using X-ray crystallography techniques, and physical crystallography approaches allow one to evaluate various properties of minerals, etc. However, the reverse comparison should not be forgotten as well: the crystallography science, in its current form, was born in the course of mineralogical research, long before preparative chemistry received such extensive development. It is worth noting that, even today, investigations of crystallographic characteristics of minerals regularly open up new horizons in materials science, because the possibilities of nature (fascinating chemical diversity; great variation of thermodynamic parameters; and, of course, almost endless processing time) are still not available for reproduction in any of the world's laboratories. This Special Issue is devoted to mineralogical crystallography, the oldest branch of crystallographic science, and aims to combine important surveys covering topics indicated in the keywords below.
galenobismutite --- high pressure --- single-crystal X-ray synchrotron diffraction --- equation of state --- calcium ferrite structure type --- lone electron pair --- vaterite --- calcium carbonate --- polymorph --- precipitation --- synthesis --- carbonation --- pathogen crystallization --- biomimetic synthesis --- renal stone --- calcium oxalate --- apatite --- brushite --- struvite --- octocalcium phosphate --- whitlockite --- Escherichia coli --- Klebsiella pneumoniae --- Pseudomonas aeruginosa --- Staphylococcus aureus --- uranyl --- selenite --- selenate --- crystal structure --- topology --- structural complexity --- demesmaekerite --- guillemenite --- haynesite --- coesite --- high-temperature Raman --- FTIR spectrum --- single crystal structure --- isobaric Grüneisen parameters --- OH-stretching modes --- strontium oxalate --- solid solutions --- ionic substitutions --- weddellite --- whewellite --- X-ray powder diffraction --- scanning electron microscopy --- EDX spectroscopy --- hydroxy-hydrate --- sulfate --- cesium --- schoepite --- krasnoshteinite --- zeolite-like borate --- hydrous aluminum chloroborate --- new mineral --- microporous crystalline material --- evaporitic salt rock --- Verkhnekamskoe potassium salt deposit --- Perm Krai --- anatomy --- Cactaceae --- oxalate --- silica --- stem --- stanfieldite --- phosphate --- merrillite --- meteorite --- pallasite --- mesosiderite --- luminophore --- bioceramics --- powder diffraction --- Raman spectroscopy --- Kamchatka --- hot springs --- pyrite --- complexity of crystal habits --- Mars --- mineral --- crystallography --- crystal chemistry --- X-ray diffraction --- crystal growth --- mineral evolution
Choose an application
Crystallography remains, for mineralogy, one of the main sources of information on natural crystalline substances. A description of mineral species shape is carried out according to the principles of geometric crystallography; the crystal structure of minerals is determined using X-ray crystallography techniques, and physical crystallography approaches allow one to evaluate various properties of minerals, etc. However, the reverse comparison should not be forgotten as well: the crystallography science, in its current form, was born in the course of mineralogical research, long before preparative chemistry received such extensive development. It is worth noting that, even today, investigations of crystallographic characteristics of minerals regularly open up new horizons in materials science, because the possibilities of nature (fascinating chemical diversity; great variation of thermodynamic parameters; and, of course, almost endless processing time) are still not available for reproduction in any of the world's laboratories. This Special Issue is devoted to mineralogical crystallography, the oldest branch of crystallographic science, and aims to combine important surveys covering topics indicated in the keywords below.
Research & information: general --- galenobismutite --- high pressure --- single-crystal X-ray synchrotron diffraction --- equation of state --- calcium ferrite structure type --- lone electron pair --- vaterite --- calcium carbonate --- polymorph --- precipitation --- synthesis --- carbonation --- pathogen crystallization --- biomimetic synthesis --- renal stone --- calcium oxalate --- apatite --- brushite --- struvite --- octocalcium phosphate --- whitlockite --- Escherichia coli --- Klebsiella pneumoniae --- Pseudomonas aeruginosa --- Staphylococcus aureus --- uranyl --- selenite --- selenate --- crystal structure --- topology --- structural complexity --- demesmaekerite --- guillemenite --- haynesite --- coesite --- high-temperature Raman --- FTIR spectrum --- single crystal structure --- isobaric Grüneisen parameters --- OH-stretching modes --- strontium oxalate --- solid solutions --- ionic substitutions --- weddellite --- whewellite --- X-ray powder diffraction --- scanning electron microscopy --- EDX spectroscopy --- hydroxy-hydrate --- sulfate --- cesium --- schoepite --- krasnoshteinite --- zeolite-like borate --- hydrous aluminum chloroborate --- new mineral --- microporous crystalline material --- evaporitic salt rock --- Verkhnekamskoe potassium salt deposit --- Perm Krai --- anatomy --- Cactaceae --- oxalate --- silica --- stem --- stanfieldite --- phosphate --- merrillite --- meteorite --- pallasite --- mesosiderite --- luminophore --- bioceramics --- powder diffraction --- Raman spectroscopy --- Kamchatka --- hot springs --- pyrite --- complexity of crystal habits --- Mars --- mineral --- crystallography --- crystal chemistry --- X-ray diffraction --- crystal growth --- mineral evolution --- galenobismutite --- high pressure --- single-crystal X-ray synchrotron diffraction --- equation of state --- calcium ferrite structure type --- lone electron pair --- vaterite --- calcium carbonate --- polymorph --- precipitation --- synthesis --- carbonation --- pathogen crystallization --- biomimetic synthesis --- renal stone --- calcium oxalate --- apatite --- brushite --- struvite --- octocalcium phosphate --- whitlockite --- Escherichia coli --- Klebsiella pneumoniae --- Pseudomonas aeruginosa --- Staphylococcus aureus --- uranyl --- selenite --- selenate --- crystal structure --- topology --- structural complexity --- demesmaekerite --- guillemenite --- haynesite --- coesite --- high-temperature Raman --- FTIR spectrum --- single crystal structure --- isobaric Grüneisen parameters --- OH-stretching modes --- strontium oxalate --- solid solutions --- ionic substitutions --- weddellite --- whewellite --- X-ray powder diffraction --- scanning electron microscopy --- EDX spectroscopy --- hydroxy-hydrate --- sulfate --- cesium --- schoepite --- krasnoshteinite --- zeolite-like borate --- hydrous aluminum chloroborate --- new mineral --- microporous crystalline material --- evaporitic salt rock --- Verkhnekamskoe potassium salt deposit --- Perm Krai --- anatomy --- Cactaceae --- oxalate --- silica --- stem --- stanfieldite --- phosphate --- merrillite --- meteorite --- pallasite --- mesosiderite --- luminophore --- bioceramics --- powder diffraction --- Raman spectroscopy --- Kamchatka --- hot springs --- pyrite --- complexity of crystal habits --- Mars --- mineral --- crystallography --- crystal chemistry --- X-ray diffraction --- crystal growth --- mineral evolution
Choose an application
One last comment concerns the fundamental contributions of Fourier analysis to quantum physics: Quantum mechanics and quantum field theory.
self-electrorefining --- hedyphane group --- structural combinatorics --- CuFe2O4 --- Kamchatka --- Raman --- El Dragón --- apatite supergroup --- borate --- ariegilatite --- oyonite --- Tuscany --- gahnite --- magnesioferrite --- Szklary pegmatite --- aurihydrargyrumite --- Au6Hg5 phase --- Trentino --- Peru --- Germany --- cerromojonite --- sulfosalt --- pyrometamorphism --- Bellerberg volcano --- manganese --- gold --- spinel supergroup --- selenium --- CuAl2O4 --- clinokurchatovite --- sharyginite --- Poland --- copper --- kurchatovite --- copper oxide --- antimony --- nabimusaite group --- laachite --- lead --- thermaerogenite --- intercalated hexagonal antiperovskite --- placer --- Lower Silesia --- Eldfell --- Tolbachik volcano --- structural complexity --- nöggerathite-(Ce) --- Val di Fiemme --- Oyon district --- sanidinite --- cuprospinel --- sulfate --- fumarole sublimate --- Cretaio --- polymorphism --- polytypism --- tiberiobardiite --- fiemmeite --- stacking faults --- CO3-group --- Hatrurim Complex --- least-action principle --- phosphorus --- Laacher See --- new oxalate mineral --- Japan --- verneite --- alkaline volcanic rock --- arsenic --- Raman spectroscopy --- single-crystal investigation --- Rusinovite --- Eifel --- Lima department --- Italy --- barioferrite --- configurational entropy --- Hekla --- mercury --- Bolivia --- parafiniukite --- aluminofluoride --- new mineral --- Shadil-Khokh volcano --- Vesuvius --- bournonite group --- Ehime --- calcium --- lillianite homologous series --- chalcophyllite group --- sou?ekite --- silicate --- pyrometamorphic rocks --- crystal structure --- zirconolite --- bismuth --- self-electrorefining --- hedyphane group --- structural combinatorics --- CuFe2O4 --- Kamchatka --- Raman --- El Dragón --- apatite supergroup --- borate --- ariegilatite --- oyonite --- Tuscany --- gahnite --- magnesioferrite --- Szklary pegmatite --- aurihydrargyrumite --- Au6Hg5 phase --- Trentino --- Peru --- Germany --- cerromojonite --- sulfosalt --- pyrometamorphism --- Bellerberg volcano --- manganese --- gold --- spinel supergroup --- selenium --- CuAl2O4 --- clinokurchatovite --- sharyginite --- Poland --- copper --- kurchatovite --- copper oxide --- antimony --- nabimusaite group --- laachite --- lead --- thermaerogenite --- intercalated hexagonal antiperovskite --- placer --- Lower Silesia --- Eldfell --- Tolbachik volcano --- structural complexity --- nöggerathite-(Ce) --- Val di Fiemme --- Oyon district --- sanidinite --- cuprospinel --- sulfate --- fumarole sublimate --- Cretaio --- polymorphism --- polytypism --- tiberiobardiite --- fiemmeite --- stacking faults --- CO3-group --- Hatrurim Complex --- least-action principle --- phosphorus --- Laacher See --- new oxalate mineral --- Japan --- verneite --- alkaline volcanic rock --- arsenic --- Raman spectroscopy --- single-crystal investigation --- Rusinovite --- Eifel --- Lima department --- Italy --- barioferrite --- configurational entropy --- Hekla --- mercury --- Bolivia --- parafiniukite --- aluminofluoride --- new mineral --- Shadil-Khokh volcano --- Vesuvius --- bournonite group --- Ehime --- calcium --- lillianite homologous series --- chalcophyllite group --- sou?ekite --- silicate --- pyrometamorphic rocks --- crystal structure --- zirconolite --- bismuth
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