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GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Southern Africa
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elements, isotopes
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stable isotopes
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Al-27/Al-26 (1)
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Mg-26/Mg-24 (1)
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Nd-144/Nd-143 (1)
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Rb-87/Sr-86 (1)
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metals
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alkali metals
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potassium (1)
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rubidium
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alkaline earth metals
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barium (2)
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calcium (2)
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magnesium
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Mg-26/Mg-24 (1)
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strontium
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Rb-87/Sr-86 (1)
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Sr-87/Sr-86 (1)
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aluminum
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chromium (1)
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cobalt (1)
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iron (1)
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nickel (1)
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rare earths
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neodymium
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Sm-147/Nd-144 (1)
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samarium
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titanium (2)
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zinc (3)
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oxygen (3)
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Mesozoic
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Paleozoic
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igneous rocks
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lamprophyres (3)
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volcanic rocks
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carbonates
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silicates
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pyroxene group
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diopside (4)
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wollastonite group
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celsian (2)
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barium feldspar
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plagioclase
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leucite (3)
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nepheline group
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silica minerals
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sodalite group
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zeolite group
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orthosilicates
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sorosilicates
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sheet silicates
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tellurides
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calaverite (1)
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Primary terms
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Africa
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East Africa
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Laetoli (1)
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Southern Africa
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South Africa
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Asia
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Far East
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Cenozoic
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Tertiary
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Paleogene
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Wasatch Formation (1)
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crystal chemistry (7)
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Romania
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Western Europe
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United Kingdom
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Hebrides
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Inner Hebrides
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Highland region Scotland
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Inverness-shire Scotland
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Moine thrust zone (1)
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geochemistry (6)
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igneous rocks
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feldspathoid rocks (1)
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lamproite (1)
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lamprophyres (3)
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volcanic rocks
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flood basalts (1)
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basanite (1)
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glasses (2)
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phonolites (2)
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stable isotopes
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Mesozoic
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Cretaceous
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alkaline earth metals
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magnesium
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Mg-26/Mg-24 (1)
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strontium
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Rb-87/Sr-86 (1)
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aluminum
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rare earths
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Sm-147/Nd-144 (1)
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samarium
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Sm-147/Nd-144 (1)
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titanium (2)
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zinc (3)
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metamorphic rocks
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metasomatic rocks
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skarn (5)
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metamorphism (4)
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metasomatism (2)
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meteorites
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Acfer Meteorites (1)
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iron meteorites
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carbonaceous chondrites
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mineral deposits, genesis (2)
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Paleozoic
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Devonian
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sediments
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spectroscopy (1)
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USSR (1)
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weathering (2)
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sedimentary rocks
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sedimentary rocks
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sedimentary structures
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sediments
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clastic sediments
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-
melilite
Cristobalite Clinker and Paralavas of Ferroan and Melilite–Nepheline Types in the Khamaryn-Khural–Khiid Combustion Methamorphic Complex, East Mongolia: Formation Conditions and Processes
Crystallisation of Ca-bearing nepheline in basanites from Kajishiyama, Tsuyama Basin, Southwest Japan
Crystal chemistry and Raman spectroscopy study of bennesherite, Ba 2 Fe 2+ Si 2 O 7 , and rare accessory Ba minerals from Caspar quarry, Bellerberg volcano, Germany
Crystal chemistry of K-rich nepheline in nephelinite from Hamada, Shimane Prefecture, Japan
High-Grade Contact Metamorphism in the Kochumdek River Valley (Podkamennaya Tunguska Basin, East Siberia): Evidence for Magma Flow
Thermodynamic properties of natural melilites
Nuwaite (Ni 6 GeS 2 ) and butianite (Ni 6 SnS 2 ), two new minerals from the Allende meteorite: Alteration products in the early solar system
Addibischoffite, Ca 2 Al 6 Al 6 O 20 , a new calcium aluminate mineral from the Acfer 214 CH carbonaceous chondrite: A new refractory phase from the solar nebula
The three-dimensional periodic nature of crystalline structures was so strongly anchored in the minds of scientists that the numerous indications that seemed to question this model struggled to acquire the status of validity. The discovery of aperiodic crystals, a generic term including modulated, composite and quasicrystal structures, started in the 1970s with the discovery of incommensurately modulated structures and the presence of satellite reflections surrounding the main reflections in the diffraction patterns. The need to use additional integers to index such diffractograms was soon adopted and theoretical considerations showed that any crystal structure requiring more than three integers to index its diffraction pattern could be described as a periodic object in a higher dimensional space, i.e. superspace, with dimension equal to the number of required integers. The structure observed in physical space is thus a three-dimensional intersection of the structure described as periodic in superspace. Once the symmetry properties of aperiodic crystals were established, the superspace theory was soon adopted in order to describe numerous examples of incommensurate crystal structures from natural and synthetic organic and inorganic compounds even to proteins. Aperiodic crystals thus exhibit perfect atomic structures with long-range order, but without any three-dimensional translational symmetry. The discovery of modulated structures was soon followed by the discovery of composite structures consisting of structural entities with partly independent translations and finally by the discovery of quasicrystals. In recent years, the use of CCD and imaging plate systems improved considerably the sensitivity of data collection for aperiodic structures and in particular modulated structures and, therefore, there was a need for further improvement of the methods. Today, several computer programs are able to solve and refine incommensurately modulated structures using the superspace approach. In nature, it is uncommon to find minerals which have strong and sharp incommensurate satellites that could be used for a higher dimensional refinement. Here we describe several cases of aperiodic minerals (natrite, calaverite, melilite, fresnoite, pearceite–polybasite, cylindrite) including the first examples of natural and stable quasicrystalline structures (icosahedrite and decagonite) which settle beyond doubt any questions which remain about the long-term stability of quasicrystals.