Ministry of Higher education, Science and Innovation of the Republic of Uzbekistan. Self study work on Practical English of the 2 ne year student of Matniyazov Mukhammed of the department Civil Engineering on speciality
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Bog'liqMarble
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- On the theme : Marble Done by : Karimbaeva Qirmizi Supervisior by : Djumashev Murat Nukus 2023 Plan
Ministry of Higher education , Science and Innovation of the Republic of Uzbekistan. Self study work on Practical English of the 2 ne year student of Matniyazov Mukhammed of the department Civil Engineering on speciality : Building materials of Karakalpak State University named after Berdakh . On the theme : Marble Done by : Karimbaeva Qirmizi Supervisior by : Djumashev Murat Nukus 2023 Plan:
Etymology The word "marble" derives from the Greek marmaros, meaning "shining stone." This stem is also the basis for the English adjective "marmoreal," which refers to something that is like marble, or someone who is aloof like a marble statue. In addtion, the word marble is colloquially used to refer to many other stones that are capable of taking a high polish.
Marble is a metamorphic rock, resulting from the metamorphism (transformation) of sedimentary carbonate rocks—either limestone (composed mainly of the [[mineral calcite) or dolomite rock (composed mainly of the mineral dolomite). The metamorphic process, which takes place at high temperatures and pressures, causes a complete recrystallization of the original rock into an interlocking mosaic of calcite or dolomite crystals. Calcite consists of calcium carbonate (CaCO3), and dolomite, of calcium magnesium carbonate (CaMg(CO3)2). The temperatures and pressures necessary to form marble usually destroy any fossils and sedimentary textures present in the original rock.
Later physical deformation and chemical decomposition of the metamorphic marbles often produces attractive coloured and variegated varieties. Decomposition yields hematite, brown limonite, pale-green talc, and, in particular, the green or yellow serpentine derived from forsterite and diopside, which is characteristic of the ophicalcites or verd antiques. Earth movements may shatter the rocks, producing fissures that are afterward filled with veins of calcite; in this way the beautiful brecciated, or veined, marbles are produced. Sometimes the broken fragments are rolled and rounded by the flow of marble under pressure. Download 6.01 Mb. Do'stlaringiz bilan baham: |
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