Blue texture

At higher threshold fields, the banana leaf and most other B7 textures observed for MHOBOW also convert irreversibly to bistable blue, though the picture is still complex, with unusual textures still seen in the cell. Our interpretation of this behavior, however, is simple. The bistable blue texture observed for MHOBOW is obtained from an SmCsPF conglomerate the target of the molecular design and synthesis effort. 

Hubbard B, Kuang W, Moser A, Facey GA, DeteUier C (2003) Structural study of maya blue textural, thermal and solid-state multinuclear magnetic resonance characterization of the palygroskite-indigo and sepioUte-indigo adducts. Clays Clay Miner 51 318-326. 

Iron blues have good lightfastness in mass tone or deep shades. Iron blues ate coarse in texture, difficult to grind, and withstand only a few minutes at 175°C. 

Figure 8.34 Left Gold focal conics of MHOBOW coexisting with accordion domains in 4-p.m SSFLC cell. Cell has not seen electric field. Right Same area after brief application of field above threshold for causing textural change of focal conics from gold SmA-like to bistable blue SmC -like. Transition from gold to bistable blue is still incomplete in this photomicrograph clear domain walls between two textures are easily seen.

The bicubic patches are characterized with different colors, intensities and line textures to show attributes such as hydrophobicity and steric properties. Only one attribute may be displayed at a time, with color and intensity representing the value of the attribute, and line texture representing karma s confidence level in the information. For example, when displaying hydrophobicity, red patches are hydrophobic space while blue patches are polar space. Patches drawn with solid lines represent areas which are well explored while patches with short dashes contain little information. Displaying information using multiple cues a ows the user to examine various aspects of the surface model without having to deal with large amounts of numerical data. 

Cathodoluminescence images from the GB deposit show primary quartz of Type II veins (blue CL), with visible growth zoning in CL. These are crosscut by later hydrothermal Type III vein quartz that exhibits growth textures in short-lived blue and red CL colors. Both Type-ll and -III veins are weakly to moderately brecciated and are overprinted by later fluids that modified the primary quartz to red and/or yellow hydrothermal quartz characteristic of higher temperature and likely reflects... 

Hydrothermal euhedral quartz (blue-green/red CL colors), of Type II veins exhibit growth textures and are related to sulfide mineralization during early Salinic Orogeny. 

Separate the precipitate from the solution by filtration through a smooth filter (fine-texture filter paper—Whatman No. 2 or Schleicher and Schnell No. 489 Blue Ribbon). Transfer the filtrate into a... 

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