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Über die Orientierung des durch Erhitzen aus Manganit entstehenden Pyrolusits
Published/Copyright:
July 28, 2010
Abstract
Manganite crystals heated to 300°C developed countless submicroscopic pyrolusite crystals on their surfaces which grew with their (010) planes parallel to those of the manganite. A contraction occurs in the Y-direction of the manganite crystals.
Published Online: 2010-07-28
Published in Print: 1963-12
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Articles in the same Issue
- Structure defects in kaolinite
- Dehydration of goethite and diaspore*
- Contributions to the crystal chemistry of normal and defect tetrahedral structures*
- The crystal and molecular structure of a synthetic imidazo-purine
- The crystal structure of the anhydrous cadmium and mercuric sulfates
- The crystal structure of dimethyl sulfone
- Hydrogen bonding and conformations in echitamine salts
- Ein einfacher Heizaufsatz für die Präzessionskamera
- Röntgenaufnahmen mit der Buergerschen Präzessionskamera bei Temperaturen zwischen 1000°C und 2000°C
- Die Kristallstruktur des Phenols
- Crystal structure of bis-(hydrazine)manganese(II) chloride
- On the crystal structure of biotites
- A three-dimensional refinement of crystalline structure of trioxane*
- Über die Orientierung des durch Erhitzen aus Manganit entstehenden Pyrolusits
