词汇 | schist |
释义 | schist noun[ U ] geology specializeduk /ʃɪst/ us /ʃɪst/ a type of rock that breaks easily into thin layers, formed of mica or other minerals片岩(容易裂成薄层的一种岩石,由云母或其他矿物质形成) Dorling Kindersley: Richard Leeney/GettyImages Geology: types of rock agglomerate arenaceous arenite asthenosphere asthenospheric emery flinty gneiss haematite indurated intrusive lahar limestone lodestone magma marcasite marl marmoreal obsidian sandstone Examples of schistschist A method for calculating effective bulk composition modification due to crystal fractionation in garnet-bearing schist: implications for isopleth thermobarometry. The lower part of the formation is often metamorphosed and deformed into strongly magnetic mica schists. The magnetization in the schist and the sandstone is interpreted to be a chemical remanant magnetization caused by the same fluids that precipitated the veins. Metasedimentary samples from the southeastern portion are represented by graphite schist and metapelite. The most common type is garnet-biotite schist consisting of biotite, garnet, feldspar and accessory zircon. The schist is composed mainly of biotite, plagioclase and quartz, whereas granulitite consists mainly of quartz, plagioclase and biotite. In schist intercalations within the marbles mineral assemblages include chlorite, calcite, albite, phengite and quartz. The soils are well drained and derived from schist. The magnetization in the veins, schist and sandstones is interpreted to have been acquired when the haematite was precipitated. These zones show the effects of intense alteration: the granite is transformed into a quartz-sericite-andalusite schist. The contact between granite and schist is intrusive, generally cross-cutting a pre-existing schistosity. The schists are dark bluish grey, fine-grained with a high quartz content (> 60 vol. %) and possess a continuous schistosity. In some places it is possible to confuse schist boulders with schist basement. These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors. |
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