triclinic वाक्य
उदाहरण वाक्य
मोबाइल
- Its chemical formula is triclinic crystals.
- Chabazite crystallizes in the triclinic crystal system with typically rhombohedral shaped crystals that are pseudo-cubic.
- The related mineral parahopeite, which has the same composition but different crystal structure, is triclinic.
- Triclinic, monoclinic and orthorhombic crystals have two optic axes, and are said to be biaxial.
- It is generally considered to be monoclinic, though optical studies have suggested it might be triclinic.
- Its crystal symmetry was first assigned as orthorhombic, then as monoclinic, and finally as triclinic.
- Kyanite is triclinic, while andalusite and sillimanite are both orthorhombic and belong to the dipyramidal point group.
- Also the whole parallelepiped has point symmetry " C i " ( see also triclinic ).
- It forms triclinic pinacoidal crystals which often occur as tubes or cylinders which are in fact rolled sheets.
- In total there are six crystal families : triclinic, monoclinic, orthorhombic, tetragonal, hexagonal and cubic.
- For triclinic, orthorhombic, and cubic crystal systems the axis designation is arbitrary and there is no principal axis.
- In the triclinic system, the crystal is described by vectors of unequal length, as in the orthorhombic system.
- It rarely occurs as single crystals, is in the triclinic crystal system, and is pale to bright yellow.
- Triclinic Na 2 FeP 2 O 7 was examined as rechargeable sodium ion batteries by a glass-ceramics method.
- Akatoreite, like hubeite, is triclinic with space group P1 * ( Burns et al ., 1993 ).
- In total there are seven crystal systems : triclinic, monoclinic, orthorhombic, tetragonal, trigonal, hexagonal and cubic.
- So, it can be either monoclinic or triclinic . Keenan Pepper 02 : 00, 8 December 2005 ( UTC)
- It belongs to the triclinic-pinacoidal crystal system ( or triclinic-normal ), It s space group is P.
- It belongs to the triclinic-pinacoidal crystal system ( or triclinic-normal ), It s space group is P.
- Magnetite also has a phase transition at which the crystal symmetry changes from cubic ( above ) to monoclinic or possibly triclinic below.
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