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index of alteration - Übersetzung nach russisch
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![[[Diamond]]s have a very high refractive index of 2.417.](https://commons.wikimedia.org/wiki/Special:FilePath/Brillanten.jpg?width=200 "[[Diamond]]s have a very high refractive index of 2.417.")
![A [[calcite]] crystal laid upon a paper with some letters showing [[double refraction]]](https://commons.wikimedia.org/wiki/Special:FilePath/Calcite.jpg?width=200 "A [[calcite]] crystal laid upon a paper with some letters showing [[double refraction]]")
![power]] of a [[magnifying glass]] is determined by the shape and refractive index of the lens.](https://commons.wikimedia.org/wiki/Special:FilePath/Lupa.na.encyklopedii.jpg?width=200 "power]] of a [[magnifying glass]] is determined by the shape and refractive index of the lens.")
![Birefringent materials can give rise to colors when placed between crossed polarizers. This is the basis for [[photoelasticity]].](https://commons.wikimedia.org/wiki/Special:FilePath/Plastic Protractor Polarized 05375.jpg?width=200 "Birefringent materials can give rise to colors when placed between crossed polarizers. This is the basis for [[photoelasticity]].")
![[[Refraction]] of light at the interface between two media of different refractive indices, with ''n''<sub>2</sub> > ''n''<sub>1</sub>. Since the [[phase velocity]] is lower in the second medium (''v''<sub>2</sub> < ''v''<sub>1</sub>), the angle of refraction ''θ''<sub>2</sub> is less than the angle of incidence ''θ''<sub>1</sub>; that is, the ray in the higher-index medium is closer to the normal.](https://commons.wikimedia.org/wiki/Special:FilePath/Snells law.svg?width=200 "[[Refraction]] of light at the interface between two media of different refractive indices, with ''n''<sub>2</sub> > ''n''<sub>1</sub>. Since the [[phase velocity]] is lower in the second medium (''v''<sub>2</sub> < ''v''<sub>1</sub>), the angle of refraction ''θ''<sub>2</sub> is less than the angle of incidence ''θ''<sub>1</sub>; that is, the ray in the higher-index medium is closer to the normal.")
![The colors of a [[soap bubble]] are determined by the [[optical path length]] through the thin soap film in a phenomenon called [[thin-film interference]].](https://commons.wikimedia.org/wiki/Special:FilePath/Soap bubble sky.jpg?width=200 "The colors of a [[soap bubble]] are determined by the [[optical path length]] through the thin soap film in a phenomenon called [[thin-film interference]].")
![A [[split-ring resonator]] array arranged to produce a negative index of refraction for [[microwaves]]](https://commons.wikimedia.org/wiki/Special:FilePath/Split-ring resonator array 10K sq nm.jpg?width=200 "A [[split-ring resonator]] array arranged to produce a negative index of refraction for [[microwaves]]")
![In [[optical mineralogy]], [[thin section]]s are used to study rocks. The method is based on the distinct refractive indices of different [[mineral]]s.](https://commons.wikimedia.org/wiki/Special:FilePath/Thin section scan crossed polarizers Siilinjärvi R636-105.90.jpg?width=200 "In [[optical mineralogy]], [[thin section]]s are used to study rocks. The method is based on the distinct refractive indices of different [[mineral]]s.")
![Thomas Young]] coined the term ''index of refraction''.](https://commons.wikimedia.org/wiki/Special:FilePath/Thomas Young (scientist).jpg?width=200 "Thomas Young]] coined the term ''index of refraction''.")
![[[Total internal reflection]] can be seen at the air-water boundary.](https://commons.wikimedia.org/wiki/Special:FilePath/Total internal reflection of Chelonia mydas.jpg?width=200 "[[Total internal reflection]] can be seen at the air-water boundary.")
![Light of different colors has slightly different refractive indices in water and therefore shows up at different positions in the [[rainbow]].](https://commons.wikimedia.org/wiki/Special:FilePath/WhereRainbowRises.jpg?width=200 "Light of different colors has slightly different refractive indices in water and therefore shows up at different positions in the [[rainbow]].")
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Definition
Wikipedia
The Conodont Alteration Index (CAI) is used to estimate the maximum temperature reached by a sedimentary rock using thermal alteration of conodont fossils. Conodonts in fossiliferous carbonates are prepared by dissolving the matrix with weak acid, since the conodonts are composed of apatite and thus do not dissolve as readily as carbonate. The fossils are then compared to the index under a microscope. The index was first developed by Anita Epstein and colleagues at the United States Geological Survey.
The CAI ranges from 1 to 6, as follows:
The CAI is commonly used by paleontologists due to its ease of measurement and the abundance of Conodonta throughout marine carbonates of the Paleozoic. However, the organism disappears from the fossil record after the Triassic period, so the CAI is not available to analyze rocks younger than 200 million years. Additionally, the index can be positively skewed in regions of hydrothermal alteration.
