orthorhombic การใช้

• Cerussite crystallizes in the orthorhombic system and is isomorphous with aragonite.
• Olivine has an orthorhombic structure with a space group of Pbnm.
• This mineral is orthorhombic and sphenoidal, exhibiting symmetry on 222.
• At 75 GPa it changes to a face-centered orthorhombic structure.
• At 100 GPa it changes to a body centered orthorhombic monatomic form.
• This soft grey material crystallizes in an orthorhombic space group.
• It occurs as prismatic to acicular transparent yellow to white orthorhombic crystals.
• It forms opaque silvery white orthorhombic prismatic crystals often exhibiting crystal twinning.
• It is a yellow mineral crystallizing in the orthorhombic system.
• The crystals often show pseudo orthorhombic forms due to twinning.
• The crystal system is orthorhombic and is flat and tabular in appearance.
• At higher temperatures the crystals take on triclinic to orthorhombic.
• It crystallizes in the orthorhombic system with a space group of Pcab.
• Columbite has the same composition and crystal symmetry ( orthorhombic ) as tantalite.
• The mineral is said to be pseudo-orthorhombic.
• Autunite crystallizes in the orthorhombic system and often occurs as tabular square crystals.
• It crystallizes in the orthorhombic dipyramidal system and is typically massive in habit.
• It has a conchoidal, uneven fracture, and an orthorhombic crystal system.
• Two phases exist the hexagonal SnSe 2 phase and the orthorhombic SnSe phase.
• It belongs in the biaxial group, because it is an orthorhombic mineral.